Citation
Geology of Jefferson County, Florida ( FGS: Bulletin 48)

Material Information

Title:
Geology of Jefferson County, Florida ( FGS: Bulletin 48)
Series Title:
Florida Geological Survey: Bulletin
Creator:
Yon, J. William
Donor:
unknown ( endowment )
Place of Publication:
Tallahassee, Fla.
Publisher:
Florida Geological Survey
Publication Date:
Copyright Date:
1966
Language:
English
Physical Description:
xi, 119 p. : illus. (1 in pocket), maps (1 in pocket) ; 23 cm.

Subjects

Subjects / Keywords:
Geology -- Florida -- Jefferson County ( lcsh )
Jefferson County ( local )
Wacissa River ( local )
Limestones ( jstor )
Quartz ( jstor )
Colors ( jstor )
Genre:
bibliography ( marcgt )
non-fiction ( marcgt )

Notes

Bibliography:
Bibliography: p. 113-116.
General Note:
Series statement: Geological bulletin - Florida Geological Survey ; 48
Statement of Responsibility:
by J. William Yon, Jr.

Record Information

Source Institution:
University of Florida
Holding Location:
University of Florida
Rights Management:
The author dedicated the work to the public domain by waiving all of his or her rights to the work worldwide under copyright law and all related or neighboring legal rights he or she had in the work, to the extent allowable by law.
Resource Identifier:
AAA1846 ( LTQF )
AKH8174 ( LTUF )
020047973 ( AlephBibNum )
01281203 ( OCLC )
a 67007516 ( LCCN )

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Full Text



STATE OF FLORIDA
STATE BOARD OF CONSERVATION
DIVISION OF GEOLOGY



FLORIDA GEOLOGICAL SURVEY

Robert O. Vernon, Director







GEOLOGICAL BULLETIN NO. 48







GEOLOGY OF JEFFERSON COUNTY, FLORIDA

by
J. William Yon, Jr.


TALLAHASSEE
1966









FLORIDA STATE BOARD

OF

CONSERVATION







HAYDON BURNS
Governor


TOM ADAMS
Secretary of State




BROWARD WILLIAMS
Treasurer




FLOYD T. CHRISTIAN
Superintendent of Public Instruction


EARL FAIRCLOTH
Attorney General




FRED O. DICKINSON, JR.
Comptroller




DOYLE CONNER
Commissioner of Agriculture


W. RANDOLPH HODGES
Director


7 '57 (






LETTER OF TRANSMITTAL


jlorida geological Survey

Callakassee

October 1, 1966

Honorable Haydon Burns, Chairman
Florida State Board of Conservation
Tallahassee, Florida

Dear Governor Burns:

The Division of Geology, of the State Board of Conservation, is
pleased to publish, as Florida Geological Survey Bulletin 48, a
study of the geology and hydrology of Jefferson County, Florida.
This report continues the series of coverage by county of the geo-
logic and economic resources of the State.
It is hoped that a complete coverage of the State will lead to
more comprehensive development of our mineral resources, par-
ticularly where these resources require large volumes and realize
a low sales price. Only if a large reserve can be shown to be present
in an area can such minerals be developed economically.

Respectfully yours,
Robert O. Vernon'
Director and State Geologist























































Completed manuscript received
May 19, 1966
Published for the Florida Geological Survey
By The E. O. Painter Printing Company
DeLand, Florida

iv









CONTENTS

Acknowledgments ---.. .--.. ... -...-..---.-....--.. -- ----.-. --- ---------- xi
Introduction --... ---.... ...........- .....-- -------.. .....-- 1
Purpose and scope of study ---.----...-----------------...- ---.. 1
Location of area .. ....-........- .. ............--------......- ..------.- --. 1
Previous investigations ....- ---------------.. 1
Maps -.... ~~-..-..... .. .-- ..-.- ..... ------.. ........ ....---- 2
Transportation .....---..--. .--.-------...------....- --..-. 4
Climate ......... ...--...------....---..- ....- ---------.--------. 4
Population and industry --------...-----.--...--- ----..-----.- 4
Well and outcrop numbering system -- ----.--. -----..-......--...- ....-- 5
Geology ..... -- ......- ..- ..--.- ... - 5
Physiography .... --- ......... ... .... .. 5
Introduction .....-- -----.. .... -- -------.. .. ....-... -....5..---------. ..
Northern Highlands --..... ..---- ................----------... .... 9
Tallahassee Hills ---....-..--... -------..----- 9
Gulf Coastal Lowlands .....----------......... ~.- -..-.......-... 9
Introduction ... ..........-.._....-------------..--- --.- -.. --..........-- 9
Modern submarine plain and coastline ...---- -. ..................... 11
Silver Bluff surface and shoreline ...........................- 12
Pamlico surface and shoreline _....... ...---. -- ...... 12
Wicomico surface and shoreline ---....-.......-...... ....... 14
W oodville karst plain -.. ---- -.......... --.--.--. ........ .. ------ -- 15
River Valley Lowlands -........-------------------...... 15
Introduction . -...... ..--.........-----------.- 15
Aucilla River Valley Lowlands ..--.. ..........-------..-.... 16
Wacissa River Valley Lowlands -.----...---------..----------........ 18
St. Marks River Valley Lowlands .--........... ... ..... --- 18
Lakes .. .......-- -............ ......-.....- ~... ------- ... 19
Springs ........ -..... ...-........... --------- ..... 20
Wacissa Springs at Wacissa .............. -- ...-- .... ....... 20
Big Spring ...--- .. -...- -----.---_.. --------- ....... 20
Garner Springs .-..--... ------ --....--...... ---------. 22
Blue Spring -.....-----.------..- ..-......... ...---.----.. 22
Buzzard Log Springs -..--.---.. .....-.......------- 22
Minnow Spring ...-----..........-..-..---... --- -..-.---- ---- 22
Cassidy Spring --....--------...........---..----2..- 22
Spring No. 1 ..-..-----. ------------.....--....-....---- --- 23
Spring No. 2 ........... ----.. -----------... ---- -...-.. 23
Thomas Spring .-....-.......-.--. -----.. --.--.--.--. -------. 23
Log Springs ---------------- ----------------..- --.-------.. ...-. 23
Discharge ........------------------------------------23
Big Spring .....-------. -----------.- ---. .. --...--. 23
Garner Spring -......-...---.-.- ------..--....... ---....... --.-------...- 24
Blue Spring .......... .......------- .--......- ... ...- ...... --- 24
Minnow Spring ......----.------- -----.----------------...---- . 24
Utilization ... ......... -----..-.-.. ----- --- ---- 24
Other Springs .... ------..--...... -.--.-----.----.------.. 24







Linear trends ------.--
Stratigraphy --- -- ---------
Introduction --.-----------
Paleozoic Era ----------
Ordovician (?) System .--------------------------
Mesozoic Era -----------
Triassic System ---------
Newark (?) Group
Cretaceous System --------
Comanche Series
Gulf Series --
Atkinson Formation --------------.. -----------
Beds of Austin Age -------
Beds of Taylor Age -------
Cenozoic Era ---
Tertiary System -- ---- -----------
Paleocene Series
Beds of Midway Age --. ------
Eocene Series .--.--... ------------.. .---------------
Wilcox undifferentiated ------
Claiborne Stage ----
Lake City Limestone ---.- -- ------
Avon Park Limestone ------
Ocala Group
Inglis Formation -------
Williston Formation
Crystal River Formation ----- -
Oligocene Series -. --------
Vicksburg Group
Suwannee Limestone ------
History
Distribution --------
General lithology
Thickness ----
Stratigraphic relationships ---
Fauna --
Geologic exposures ----------
Miocene Series -----------------
Tampa Stage
St. Marks Formation ---. ---
History
Distribution -
General lithology ------
Thickness --- ....--- ----
Stratigraphic relationships ------....-
Fauna .... ---------
Geologic exposures ----....----------------
Alum Bluff Stage- ------
Hawthorn Formation ------- ....------------
History -..--.... -----
Distribution -.---------------------------.--
General lithology --------------------------


..------ 24
..------ 25
.------ 25
-..-- 33
-...--- 33
------- 33
33
33
----- 33
--33
34
------ 34
..- 35
--35
-------- 36
--------- 36
36

---.---- 36
------- 36
------36
36
36
37
-------------------- 37
37
38
38
38
38
38
38

38
40
------- 42
42
---43
----43
46
46
--- 46
46
-.- 47
--47
---- 47
--- -... 48
S-------48
-----.... 48
.50
. ----... 50
-..----- 50
------- 50
...-- .. 51








Thickness ---------
Stratigraphic relationships -...........------
Fauna ... ..- .. .....-- ... .... --- .
Geologic exposures -...- -....-------------...
Choctawhatchee Stage -...-..............--------
Miccosukee Formation -....-.--- --...... --
History ...... ....... .....- -----
Definition and distribution --- .. -..-..-----
General lithology ..-............... .........
Thickness .......--........ .-----------.
Stratigraphic relationships ....... -
Fauna ------...... ..... ... ....- ---
Geologic exposures --...--............-----.
Quaternary System ..---......----..--.-----.------.--
Pleistocene and Recent deposits ..- .. ..--.---..
Distribution ------------- ---
General lithology .--...-.-.----.-.--..------.
Thickness ........- ..-- ...- . -----
Stratigraphic relationships --...-......... .-


- .- ..- ...- ..-.......- 51
.--. --.-.- ...-..- -- 51
-.-. ..... ... .---. 51
..-.. .. ..---------..---- 53
--- ...- ...... ..... ---- 53
---....-.-------.---... -. 53
- .----...~ ---. 54
-.--- -........ 54
-....-..--.-.....-------- 55
-. .......--- ..-. .--.--. 55
-..- ..-- .--....----..---. 55
-.--.. ..-.-- ...------ ...--. 57
..- ..-.....-... ....- 61
-.--- ..-- ----.....--......- 61


---..----- 61
.......- -- 61
.....----.. 62
--- -- 62


Fauna -----.. -------------.-- ---------------- .
Structure ----
Geologic history -..... -......-...------. -----. ---..--
The myth of the Wakulla Volcano
Economic geology ........-----------
Limestone ..- .--- ... ..-----------
Dolomite rock ----.. ....--------....... .... .....-.
Clay deposits ---------------.... -
Introduction .-----------...........
Tests .------..-. ------..-...-.. ----------------------
Sand ----- ----------------
Petroleum possibilities --. -----... ..... .... .. ....
Phosphate ...................-------- -.--------. ---
Ground water .-----..........-.....--..------------..
Artesian water ------. ..------- --....-.
Floridan aquifer ---.-----------------
Fluctuations of water levels ----......~.....
Piezometric surface ----
Quality of water .....- ---. .....-..-....-.....--
Dissolved solids ----- ...-------- .......
Hardness .............-.. .....- -----------------
Temperature -........ ------- -....---- ......-.......--
Specific conductance -- --------------
Hydrogen-Ion concentration (pH) ---. ...... ---- ---..-............ ..
Silica (SiO,) .----------------
Iron (Fe) -.------------------
Calcium (Ca) and magnesium (Mg) -----..... ..-......- ........
Sodium (Na) and potassium (K) --...... .....----
Bicarbonate (HCO,) ---- ...--------... ...
Sulfate (SO4) ----------------
Chloride (Cl) .......... ---- --------. -------
Fluoride (F) ------------------
Nitrate (NO ) ---- -----------------------


--------------------
-------------------
-------------------







Appendix -- ~......------------------------- 92
Bibliography ...-- ------------------------------ 112
Index 116
I n d e x ... ... ......-- ------------------- - - --- - - --... . . . . . . . . . . ..-- - -- 1 1 6


ILLUSTRATIONS


Figure Page
1 Map showing location of Jefferson County, Florida --.....-......------- 2
2 Index to Topographic maps of Jefferson County, Florida .-..- ----...- 3
3 Well and outcrop numbering system ........--. -----.-------- --- 6
4 Physiographic map of Jefferson County, Florida ---.......-..--...----..--. 8
5 View looking north towards the Cody Scarp in Jefferson
County, Florida -....---......-..--------------------------- ----.--.-- 10
6 Surface profiles showing Pleistocene shorelines in Jefferson
County, Florida ----....-----..--------..----------------------------- -. 13
7 Aucilla River at low water stage in Jefferson County, Florida ....--. 17
8 Contours showing approximate altitude of the top of the
first limestone in Jefferson County, Florida --....... .- ---.... 21
9 Linear trends in Jefferson County, Florida ------------. ----- 26
10 Contours showing approximate altitude of the top of the
Suwannee Limestone Jefferson County, Florida --...... -- -....... 27
11 Well locations and lines of sections in Jefferson County,
Florida ....--- -.....-......----- ----------- ---.-- ---------- 29
12 Dolomitized Suwannee Limestone cropping out on the bank
of the Aucilla River, Jefferson County, Florida ---........... .....- 39
13 Rapids on the Aucilla River caused by dolomitized Suwannee
Limestone, Jefferson County, Florida ........ ..~.............. .... 40
14 Geologic cross sections in Jefferson County, Florida ----...--..----.. 41
15 Dolomitized Suwannee Limestone exposed in the Gulf of
Mexico off the coast of Jefferson County, Florida .-- ........ 42
16 Silicified boulders of Suwannee Limestone exposed in road-
cuts in the southern part of Jefferson County, Florida -........ -...... 43
17 Quarry of Suwannee Limestone, Jefferson County, Florida --..-....-. 44
18 Roadcut showing clay laminae associated with very fine to
medium grain size quartz sands ---.--. -------------- .....56
19 Roadcut showing clay laminae associated with very fine to
coarse sands and also verticle joints filled with sandy clay --.... ... 57
20 Distribution of the economic deposits of Jefferson County,
Florida ------...--....... ....... --................ ........... ..- ... -- 70
21 Route of Florida's interstate highway system, waterways,
and natural gas pipeline (after Reves) --......-...............-- ------.. 71
22 Cumulative departure curve of average precipitation at
Monticello, Jefferson County from 1948 to December, 1962 ..--.....- 80
23 Graph showing hydrographs of selected wells WJf-3N-4E-22
cb, WJf-3N-7E-27 bb, WJf-1S-3E-15 dc, WJf-1S-4E-28 ac
and total monthly precipitation in Jefferson County, Florida .....--- 82
24 Jefferson County, Florida, showing the piezometric surface
of the Floridan aquifer in May, 1960 --.--.. ...---------...-...... --------------83
25 Jefferson County, Florida, showing the piezometric surface
of the Floridan aquifer in December, 1962 -----...--.............. ...-----.. 84








26 Hydrograph of well WJf-1N-4E-26 bb and a total monthly
precipitation graph of rainfall in Jefferson County, Florida .------- 86
27 Bar graphs showing chemical composition of artesian water
in Jefferson County, Florida -._-- -----._________--------. ---- 87
28 Hardness and total dissolved solids curve of artesian water
in Jefferson County, Florida -..-..._--... -...... ------------ 89

Plate
1 Geologic map of Jefferson County, Florida.

Table
1 Population of Jefferson County in 1950, 1956, and 1960 -- 4
2 Pleistocene terraces in Jefferson County, Florida -- 11
3 Geologic Formations in Jefferson County, Florida ---- 28
4 Geologic data from selected wells in the Jefferson County
area .. ___ _._- .30
5 Chemical analyses of Suwannee Limestone samples from
Jefferson County, Florida ------ -- 68
6 Soil test results of samples of Suwannee Limestone from
Jefferson County, Florida ------ 71
7 Chemical analyses of Suwannee dolomite samples from
Jefferson County, Florida _-_--- _----------- 73
8 Tests of selected clay samples from Jefferson County, Florida -----. 76
9 Analyses of water from selected wells in Jefferson and
Taylor counties, Florida ----...- -------_ In Pocket










ACKNOWLEDGMENTS


Gratitude is expressed to Dr. Robert O. Vernon for many
helpful suggestions and his efforts as State Geologist in making
this study possible. Appreciation is expressed to C. W. Hendry,
Jr., Assistant State Geologist, who gave freely of his time to
the writer both in discussion and field visits. The writer is
grateful to the staff of the Florida Geological Survey, who gave
immeasurable help in the various phases of the project. S. J.
Olsen, vertebrate paleontologist of the Florida Geological Survey,
generously wrote sections on vertebrate faunas for which the
writer is most appreciative.
Appreciation is expressed to Rowe Brothers Well Drilling Com-
pany and Terra-Rosa Hardware Company, Tallahassee, Florida,
and to Carr Well Drilling Company, Thomasville, Georgia, for fur-
nishing rock cuttings and other information on well drilling in
Jefferson County.
Special thanks are due L. H. Crampton, of the Tungsten
Plantation, Inc., for the many courtesies extended the writer.
The writer would like to express his appreciation to R. C.
Crooks, director of the Fertilizer Laboratory of the Chemical Divi-
sion, Florida Department of Agriculture, for providing chemical
data on the limestone samples submitted to his department for
analyses and to T. C. Bransford, Florida State Road Depart-
ment Testing and Materials Laboratory, for determining some
physical properties on limestone samples submitted to his depart-
ment.
The writer is grateful to the citizens of Jefferson County for
their many courtesies and aid during the course of the field work
for this report.
Mr. and Mrs. Paul Appin gave freely of their information con-
cerning the two deep oil tests in Jefferson County, and the writer
is grateful to them.
Sincere appreciation is expressed to William Clark and Nevin
Hoy of the United States Geological Survey for reading the manu-
script and making very useful comments.









GEOLOGY OF JEFFERSON COUNTY, FLORIDA

By
J. William Yon, Jr.

INTRODUCTION

PURPOSE AND SCOPE OF STUDY

The purpose of this report was to make a detailed study of the
geology of Jefferson County and to provide information needed
for development of the mineral resources of the area.
The field work was begun in the summer of 1961 and was
completed in the latter part of 1962. Where accessible, most of the
surface geology was mapped and cuttings from numerous wells
were examined for data on the subsurface geology. In conjunction
with the geological studies, a survey was made of the mineral
resources.

LOCATION OF AREA

Jefferson County is located in what is referred to as the Pan-
handle of Florida, as shown in figure 1. It bounds the State of
Georgia on the north; Leon and Wakulla counties on the west;
Taylor and Madison counties on the east; and the Gulf of Mexico
on the south. Jefferson County is wedge-shaped being approxi-
mately 25 miles wide along its northern boundary and 6 miles
wide along the southern boundary. The length of the county is 39
miles and it comprises an area of 598 square miles.

PREVIOUS INVESTIGATIONS

In many of the reports on the geology of Florida, reference is
made to Jefferson County. However, only those reports which are
countywide in aspect are mentioned below. Reports involving spe-
cifics of the county geology are indexed in the text where they have
direct bearing on some specific phase of the geology.
A report by Sellards (1917, p. 85-139) is a reconnaissance study
of the geology, mineral resources and springs of Jefferson County.
The general geology of Jefferson County is discussed by Mossom
(1926), Cooke and Mossom (1929), and Cooke (1945). The regional








2 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


i-r


!Monticello


Cox




5 R-
i 0


SE iE 7En


hw

Figure 1. Map showing location of Jefferson County, Florida.



work of Applin and Applin (1944, 1947, 1951, 1955) is a major
contribution to the understanding of the subsurface geology of
not only Jefferson County but all of Florida.

MAPS


The maps used for plotting the field data were United States
Geological Survey topographic maps, figure 2, and the Florida
State Road Department general highway map for Jefferson Coun-
ty. The base map used in this report was compiled from the topo-
graphic maps.










GEOLOGY OF JEFFERSON COUNTY, FLORIDA


SCALE


COUNTY
LOCATION


STATE OF FLORIDA
STATE BOARD OF CONSERVATION
JEFFERSON COUNTY
prepared by
DIVISION OF GEOLOGY /


Figure 2. Index to Topographic maps of Jefferson County, Florida.






4 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

TRANSPORTATION

Jefferson County is served by two railroads, the Seaboard Air
Line, and a branch line of the Atlantic Coast Line.
Three major highways traverse the county from west to east,
U. S. 27, 90, and 98. The two major north-south highways are
U. S. 19 and 221. Except for the southernmost part of the county
there are many secondary paved roads that make the county
accessible by car.

CLIMATE

Jefferson County is in an area of southeast wet continental and
north Florida transitional climate. It has an average January tem-
perature of about 57F, an average July temperature of about 82F
and 9 to 10 months frost free. The average annual precipitation
is 55 inches. Most of the rainfall occurs during the months of
June through September.

POPULATION AND INDUSTRY

The population in Jefferson County for 1950, 1956, and 1960
is shown on table 1. The population figures in 1950 and 1960 are
from the records of the U. S. Census Bureau, and the 1956 figure
is from estimates by the Bureau of Economics and Business Re-
search, University of Florida.



TABLE 1. Population of Jefferson County,
1950, 1956, and 1960

Percent change
1950 1956 1960 1950-60

10,413 9,200 9,543 -8.4

Agriculture is the principal industry of Jefferson County; it
has 190,000 acres in farms, and the farms average 342 acres.
The county is a large producer of pecans and watermelons. Cattle
raising, tung oil, and the dairy industry play an important role
in the economy of the county. The percent of total land in forest
is 73 percent or 248,000 acres.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


WELL AND OUTCROP NUMBERING SYSTEM

The well and outcrop numbering system used in this report is
based on the location of the well or outcrop and uses the rectangu-
lar system of section, township and range for identification. The
well or outcrop number consists of six parts: W for well or L for
outcrop, county abbreviation, the quarter/quarter location within
the section, the section, township, and range.
The basic rectangle is the township which is 6 miles square.
It is consecutively numbered by tiers both north and south of the
Florida base line and is also consecutively numbered east and
west of the principal meridian. In the present numbering system
the T will be left off the township number and the R off the range
number. Each township is divided equally into 36 square miles
called sections, and are numbered 1 through 36 as shown on figure
3. The sections are divided into quarters with the quarters being
labeled "a" through "d" as shown on figure 3. In turn, each of
these quarters are divided into quarters with these quarter/quarter
squares labeled "a" through "d."
An exception to the above system will be used for locations
occurring above the Watson Line near the Georgia-Florida State
line where irregular consecutively numbered sections are used and
will be listed only by the irregular section number.
When there is more than one well or outcrop in a quarter
quarter section they are identified by a sixth number at the end
of the fifth unit. The abbreviation used for counties in this report
are Jf for Jefferson, Ln for Leon, Md for Madison, Ty for Taylor
and Wk for Wakulla.

GEOLOGY

PHYSIOGRAPHY

INTRODUCTION

Cooke (1939, p. 14) divided Florida into the following five nat-
ural topographic regions: Coastal Lowlands, for all that area up
to 100 feet in elevation; Western Highlands; Marianna Lowlands;
Tallahassee Hills; and Central Highlands, for the generally higher,
hilly, interior regions.
Vernon (1951, p. 16) proposed a genetic classification in which
he recognized four of the following major physiographic divisions:








6 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT









zu


S+ R3 E + R4 E R5 E R6E + R7E











I BASE LINE
/ WJF 1S-4E-2 bi





S I c- z
++ +a b









i + R3E +"Jr R4E R5E + R6E R 7 E







o 7 8 9 10 11 12
S 18 17 16 15 14 13
19 20 21 22 23 24

30 29 28 27 26 25

31 32 33 34 35 36


Figure 3. Well and Outcrop numbering system.






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


Delta Plain Highlands, Tertiary Highlands, Terraced Coastal Low-
lands, and River Valley Lowlands. He (Vernon, 1951, p. 16) also
stated that these major subdivisions could be further subdivided
into smaller units and local names applied to them.
Based on his idea of origin for the physiographic units of
Florida, Vernon (1951, p. 14, 16) made the following changes in
Cooke's (1939, p 14) terminology: Vernon replaced Cooke's Talla-
hassee Hills with Tertiary Highlands; included the Western High-
lands and Central Highlands in the Delta Plain Highlands; sub-
stituted Terraced Coastal Lowlands for Coastal Lowlands; and
River Valley Lowlands for Marianna Lowlands.
The Tertiary Highlands of Vernon (1951, p. 14, 16) include
sediments formed either as a part of a high-level, widespread,
aggradational delta plain, or of Tertiary sediments rising above
this plain. The lowlands were formed by marine erosion and depo-
sition along coastlines, stream erosion, and alluviation along stream
valleys.
In the latest work on the physiography of Florida, White, Ver-
non and Puri (Puri and Vernon, 1964, p. 7-15) divide Florida into
the following major groups: Coastal Lowlands, Intermediate
Coastal Lowlands, Gulf Coastal Lowlands, Central Highlands,
Northern Highlands, and the Marianna Lowlands. These primary
divisions are subdivided into secondary and tertiary physiographic
units.
The Northern Highlands extend across the northern part of
Florida from Trail Ridge on the east side of the State and then
westward to the Alabama state line (Puri and Vernon, 1964, p. 10).
They are continuous except where interrupted by the Marianna
Lowlands. The Northern Highlands are subdivided into the fol-
lowing secondary units: Trail Ridge, Florahome Valley, Tallahassee
Hills, Grand Ridge, New Hope Ridge, Washington County Out-
liers, and the Western Highlands.
White, Puri and Vernon (Vernon and Puri, 1964, p. 13, 14) pro-
posed three primary divisions to replace Vernon's Terraced Coastal
Lowlands, and they are: Coastal Lowlands, the Intermediate
Coastal Lowlands, and the Gulf Coastal Lowlands.
The deposits studied in this investigation lie within the East
Gulf Coastal Plain, a subdivision of the Coastal Plain Province
(Fenneman, 1938, p. 1-83). In Jefferson County the major phy-
siographic divisions of Vernon (1951, p. 16), White, Vernon,
and Puri are recognized, and include the following major
divisions, figure 4: (1) Tallahassee Hills, (2) Gulf Coastal Low-










8 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


G E O R G I A


1 0 1 2 3 4 5MILES
SCALE


Ai Pa
OF MEX,


NORTHERN HIGHLANDS
TALLAHASSEE HILLS
GULF COASTAL LOWLANDS & WOODVILLE KARST PLAIN
WICOMICO TERRACE
LIMESTONE SHELF
DUNE BELT
PAMLICO TERRACE
LIMESTONE SHELF
DUNE BELT
SILVER BLUFF TERRACE
LIMESTONE AND DOLOMITE SHELF
SAND BAR
COASTAL MARSH BELT
RIVER VALLEY LOWLANDS
AUCILLA RIVER VALLEY
WACISSA RIVER VALLEY
ST. MARKS RIVER VALLEY LOWLANDS


STATE BOARD OF CONSERVATION


Figure 4. Physiographic map of Jefferson County, Florida.


- I I I I - - -1. prepared by DIV151ON OF GEOLOGY


..... ..A uii, )IVli/let-






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


lands, and (3) St. Marks, Wacissa and Aucilla River Valley Low-
lands. A Tertiary unit, the Woodville Karst Plain (Hendry and
Sproul, 1966) can be traced through Jefferson County.

NORTHERN HIGHLANDS

TALLAHASSEE HILLS

The term Tallahassee Hills includes the area lying between
the Florida-Georgia State line on the north, the Gulf Coastal Low-
lands on the south, the Withlacoochee River on the east, and the
Apalachicola River on the west. In Jefferson County the Talla-
hassee Hills includes the area extending southward from the
Florida-Georgia State line to the Gulf Coastal Lowlands.
The Tallahassee Hills are erosional-remnant hills and ridges
with elevations up to 260 feet. Along the eastern side of the county
there is a relatively large topographically low area associated with
a number of isolated hills. Although the Tallahassee Hills in this
area have been highly dissected by stream erosion and subsurface
solution, they probably once represented a nearly flat Miocene
delta plain that covered all of northern Jefferson County. The
Tallahassee Hills are composed of a heterogeneous mass of plastics
that comprise the Upper Miocene Miccosukee Formation and are
underlain by the Middle Miocene Hawthorn Formation, and the
Lower Miocene St. Marks Formation. 'Lake Miccosukee occurs
within the Tallahassee Hills in western Jefferson County, and in
many other places the Hills are interspersed with smaller lakes,
streams, and narrow valleys.
The Tallahassee Hills end in the southern part of Jefferson
County at a well defined southward-facing escarpment, figure 5,
named the Cody Scarp (Puri and Vernon, 1964, p. 11). In the
northeastern portion of Jefferson County the Aucilla River cuts
through the Tallahassee Hills. Where the Aucilla River forms
the county line boundary between Madison and Jefferson counties,
the Tallahassee Hills have been separated by erosion from their
counterpart to the east.

GULF COASTAL LOWLANDS

INTRODUCTION

The Pleistocene Epoch, or "Great Ice Age," is characterized by
worldwide fluctuations in sea level. The periods of time when sea
level was lowered are referred to as glacial stages. This was






10 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


**^ ^ ... . .






.3
1P': .....










Figure 5. View looking north towards the Cody Scarp in Jefferson County,
Florida.

accomplished by the storing of large quantities of ocean's water
as land-glaciers. The interglacial stages were those times when
the glaciers receded, thus returning the water to the seas and
causing a rise in sea level. During each of the interglacial stages,
when sea level rose and remained stationary at one elevation, a
terrace and shoreline was formed. According to Vernon (1951,
p. 36) the older and higher shorelines and terraces are preserved
because each succeeding rise in sea level during the interglacial
stages never reached the height of the preceding older stand of
the sea. Consequently, the record of the different sea levels during
the interglacial stages show a progressive decrease in elevations.
Cooke (1954, p. 248) recognized eight marine terraces and
shorelines in Florida. MacNeil (1950, p. 99) recognized only four
terraces and shorelines. Vernon (1951, p. 36-41) considered that
only four marine surfaces and shorelines exist in Florida. How-
ever, in a later report, Puri and Vernon (1959, p. 239-240), recog-
nized another shoreline for a total of five marine terraces and
shorelines.
Three marine terraces and shorelines are recognized in Jeffer-
son County, as shown in figure 6. The approximate altitude of the
shorelines and, tentative age are shown in table 2.
shorelines and~tentative age are shown in table 2.








GEOLOGY OF JEFFERSON COUNTY, FLORIDA


TABLE 2. Pleistocene terraces in Jefferson County, Florida.

Approximate altitude
Terrace of shoreline (feet) Tentative age assignment

Wicomico 40-45 Sangamon
Pamlico 26-30 Interglacial recession in
Wisconsin glacial
Silver Bluff 10 Interglacial recession in
Wisconsin glacial or Recent

The Gulf Coastal Lowlands in Jefferson County extend from
the Cody Scarp to the coastline and consists of the three Pleisto-
cene terraces and shorelines. The modern coast and submarine
plain is included under the Gulf Coastal Lowlands.

Modern Submarine Plain and Coastline

The present coastline of Jefferson County is a low or zero
energy shoreline (Price, 1953; Tanner, 1960). It is marshy, very
irregular, and is dissected by several streams that originate at
the inner edge of the coastal marshes. The absence of sand beaches
and barriers along the coastline is attributed to the lack of wave
activity and inadequate sand supply (Price, 1953; Tanner, 1960).
The modern submarine plain off the coast of Jefferson County
has a gentle seaward slope and the waters covering it are shallow.
In an attempt to determine the nature of the sediments on
the sea floor, the following methods were used to collect data:
sampled pinnacles which protrude above the surface of the water;
through the use of self-contained underwater breathing apparatus;
and evaluation of data obtained from the Corps of Engineers.
The data obtained from the first two methods indicated that the
submarine plain is a rock surface of silicified and dolomitized
Suwannee Limestone. Two of the features shown on the U.S.
Coast and Geodetic hydrograph 1261, the Grey Mare Rock and
Cobb Rocks, can readily be seen from a boat. The Grey Mare
Rock is a large pinnacle of silicified Suwannee Limestone, and
the Cobb Rocks are dolomitized Suwannee. The Corps of Engineers
prepared a bottom profile with logs of core borings along a proposed
intracoastal waterway from St. Marks to Tampa Bay, Florida.
(Survey Report of 1940, 1952, and 1956). Along the coast border-
ing Jefferson County the logs show that the rock surface is covered
by a thin veneer of clastics. Oyster bars are very prevalent along
the coast of Jefferson County, especially at the mouths of the
creeks and the Aucilla River.






12 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

Silver Bluff Surface and Shoreline

The Silver Bluff shoreline is the term applied to a wave-cut
notch occurring at an elevation of 5 feet at Silver Bluff near
Miami (Parker and Cooke, 1944, p. 24).
The Silver Bluff shoreline was extended by MacNeil (1950, p.
104) to other parts of Florida and northern Georgia, and he con-
siders the toe of the Silver Bluff scarp to occur at an elevation
of 10 feet. As shown on the land-surface profiles (fig. 6), the small
escarpment whose toe occurs at an elevation of 8 to 10 feet is
considered to be the Silver Bluff strandline.
The Silver Bluff marine plain, the youngest and lowest of the
coastal terraces, extends from the edge of the present coastline
inward, four to six miles, to the 10-foot contour line, which marks
the base of a small escarpment.
The coastal marshlands forming the outer part of the Silver
Bluff marine plain consist of mud and silts that support grasses.
Inland from the coastal marsh belt is a fairly flat, poorly drained
sand area, with a prolific stand of cedar, palm, and pine trees.
Beneath the clastics is a shelf composed of Suwannee Limestone
which in places has been silicified or dolomitized. The formation
crops out through the sand cover in many places and in ditches
along logging roads.
The absence of barrier islands, the gentle slope of the Silver
Bluff marine plain, and the poorly developed escarpment seem to
indicate the coastline during Silver Bluff time was generally one
of low or zero energy, with a sparse supply of sand. However, the
feature shown on the physiographic map (fig. 4) along southwes-
tern Jefferson County may have formed as on offshore bar or shoal.

Pamlico Surface and Shoreline

The Pamlico shoreline and terrace is one of the best developed
Pleistocene features in Florida and can be recognized in most
areas of the State.
The Pamlico shoreline and escarpment can be seen in western
Jefferson County in the vicinity of Fanlew. The escarpment has
approximately 8 to 10 feet of relief, and its toe occurs at an
elevation of 26-30 feet. The Pamlico terrace covers the county
from the shoreline of the Silver Bluff terrace inland for a distance
of approximately 8 miles. The Pamlico terrace has formed a lime-
stone plain that is covered by varying thicknesses of sands and
clays. The Wacissa River flows across the terrace and gives rise









GEOLOGY OF JEFFERSON COUNTY, FLORIDA


140-

120-

100-

80-

60-

40-

20

0

140r

120-

100-

80-

60-

40-

20-
0-

20C-

180

160

W 140
w
U-
120-


p 80-

60-
w
-J
S40

20

0-

160-

140-

120-

100-

80-

60-

40-

20-

0

140-

120-

100-

80-

60-

40-

20-
0-


Gulf of Mexico


JEFFERSON COUNTY
o 5 10
5 0 .MILES


RIVER


BASE LINE


CROSS SECTION
0 2_3
I o 0 MLES'


SHORELINE


> AUCILLA RIVER


PAMLICO SHORELINE


BLUFF SHORELINE


ILICO SHORELINE


SILVER BLUFF SHORELINE


Figure 6. Surface profiles showing Pleistocene shorelines in Jefferson County,
Florida.


13


RIVER


I I ,. I ~ L -~






14 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

to a broad swamp area along its course. In eastern Jefferson County
the Pamlico terrace is fairly well drained, but to the west the
drainage is poor and swamps are more prevalent. Palmetto, scrub
oak, hardwood, and pine trees are very common on this surface.
Calico Hill, a sand ridge with about 12 feet of relief and lying
parallel to the Wacissa River, is probably a Pamlico dune (fig. 4).
Inland from the Pamlico shoreline, in eastern Jefferson County,
are found a series of crescent-shaped features which are believed
to be sand dunes that have relief up to 20 feet. Outcrops of the
St. Marks Formation and the Suwannee Limestone occur on the
lower part of the terrace near the Silver Bluff shoreline. Mont-
morillonitic clays, containing weathered mollusk shells, were
found at localities LJf-2S-3E-14-ac and LJf-2S-3E-15-center and
are believed to have been deposited during Pamlico time.
A portion of the Pamlico shoreline, as shown in figure 6, was
drawn by using recognizable escarpments. However, for the most
part, the 30-foot contour was used to show the approximate posi-
tion of the Pamlico shoreline.

Wicomico Surface and Shoreline

Cooke (1945, p. 281-286) places the shoreline for the Wicomico
from 100-105 feet.
The Wicomico shoreline is believed to coincide with the Cody
Scarp, whose base occurs at 40-45 feet, cutting across the southern
part of Jefferson County. However, when the escarpment is traced
westward into Leon County it rises to 100 feet and higher (C. W.
Hendry, Jr. Personal Communication). This anomaly in elevation
of an apparently similarly related feature is not uncommon in
Florida where limestone lies near the ground surface and is readily
susceptible to solution (White, 1958, p. 9-44). Yon and Puri (1962,
p. 679-680) point out that the Wicomico shoreline in Gilchrist
County, Florida, occurred at 70 feet because it had been lowered
by solution of the underlying limestones. The Wicomico terrace
in Jefferson County includes all of the area lying between the
Pamlico shoreline and the Cody Scarp. The Wicomico marine plain
extends across the width of the county and is approximately 4 to
5 miles wide, except on the western edge of Jefferson County where
it becomes about 7 miles wide.
The Wicomico terrace deposits consist essentially of sands and
clayey sands that have been deposited on top of a limestone shelf.
The surface is generally poorly drained and swampy, especially on
the flood plains of the Wacissa and St. Marks rivers. The western







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


side of the terrace contains a belt of sand dunes formed during
the stand of the Pamlico seas.
An area of sandhills, covered with vegetation, with elevations
160 feet and higher, occurs inland from the Wicomico shoreline
in Western Jefferson County and are interspersed with sinkhole
lakes. It is believed these sand hills are Wicomico age deposits.

WOODVILLE KARST PLAIN

C. W. Hendry, Jr. (Personal Communication) proposes the term
Woodville Karst Plain for a low, gently sloping plain beginning in
the southern part of Leon County and extending southward
through Wakulla County to the Gulf. He describes the plain as
being characterized by sand dunes lying upon a limestone surface.
The porous nature of the sands has readily permitted ground
water to percolate downward, thereby causing dissolution of the
limestone. The result of this solution has lead to a continuous and
rapid lowering of the original surface. The area is characterized
by the formation of shallow sand-bottom sinkholes. The Woodville
Karst Plain extends into Jefferson County, and includes all the
area mapped as the Gulf Coastal Lowlands (fig. 4).
The Woodville Karst Plain is not generally as well developed
in Jefferson County as it is in Leon and Wakulla counties. The
dune belt in northwestern Jefferson County best exhibits the
characteristics of the Woodville Karst Plain as described by
Hendry. The dunes appear to be barchan type with up to 20 feet
of relief and are underlain by Miocene and Oligocene limestones
that are soluble in percolating acidized water. Because of the
collapse of the limestone, shallow sinkhole development is fairly
prevalent.

RIVER VALLEY LOWLANDS

INTRODUCTION

The River Valley Lowlands consist of all the valleys in Jefferson
County. A number of creeks originate within the Tallahassee
Hills and flow into the St. Marks and Aucilla rivers. Most of them
are laden with humic acids, are high in color, and carry very little
sediment.
The Aucilla River forms part of the eastern boundary of
Jefferson County and is the largest stream in the county. The St.






16 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

Marks River has its headwaters in Leon County, and only flows
a few miles through Jefferson County.
The Wacissa River originates from a group of springs just
below the town of Wacissa and flows southward into the Aucilla
River.
The Penhook River heads up in the swamps occurring on the
Pamlico surface and flows southward across the Coastal Marsh
Belt into the Gulf.
A number of creeks originate at the head of the Coastal Marsh
Belt in the lower part of Jefferson County and flow southward into
the Gulf.

AUCILLA RIVER VALLEY LOWLANDS

The Aucilla River has its headwaters in Brooks County,
Georgia, and flows southward along the eastern edge of Jefferson
County to the Gulf of Mexico. From the Georgia-Florida State line
southward to where U. S. Highway 90 crosses the Aucilla, the
river flows in a valley approximately 1-mile wide that has been
cut into Miccosukee and Hawthorn clastics. At times the Aucilla
is almost dry, as shown in figure 7. However, during periods of high
rainfall, the river overflows the small channel and broadens out to
cover the entire valley, giving it the appearance of a lake. During
periods of high water the main channel is not distinguishable, and
swamp conditions are prevalent along the upper course. Why the
valley of the Aucilla is considerably wider in the upper reaches
than in the lower reaches presents an interesting problem. The
configuration of the bedrock, figure 8, the reasonable closeness of
the underlying rock to the land surface, and the narrow channel
of the present stream occupying the broad valley, may point
toward solution of the underlying limestone and subsequent col-
lapse of the overlying sediments as an origin for the valley.
However, it is possible that during higher stands of the Pleistocene
seas, the valley was formed by progressive downward cutting of
the stream as sea level fell.
To ascertain if river terraces occurred along the Aucilla River
in the Tallahassee Hills area, a number of land-surface profiles
compiled from topographic maps were drawn normal to the river's
axis. Two stream-cut terraces above the flood plain of the Aucilla
River show up in the profiles at approximately 10 and 40 feet.
Higher fluvial surfaces may be present but erosion has altered
the land surface to a degree that they are no longer apparent.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


Figure 7. Aucilla River at low water stage in Jefferson County, Florida.


From where the Tallahassee Hills join the Gulf Coastal Low-
lands the Aucilla River flows in a steep-walled valley cut into the
Suwannee Limestone. Rapids flowing over silicified limestone are
common. Terraces do not appear to have been formed along this
section of the river. The flood plain is narrow, and during flood
stage the river flows out over the surrounding area. From the
point where State Highway 257 crosses the river to the point
where the Aucilla disappears underground, outcrops of dolomitized
Suwannee Limestone are almost continuous. From a point in
section 21, T3S, R4E to Nutall Rise the river flows underground.
The Aucilla River is joined by the Wacissa River in the vicinity
of Nutall Rise, and flows on a southerly course to the Gulf. Springs
are present along the Aucilla River southward from Nutall Rise
to the Gulf of Mexico.
According to the Surface Water Branch, United States Geologi-
cal Survey, the Aucilla River has an approximate drainage area
of 740 square miles in Florida, which would include most of Jeffer-
son County, almost half of Madison County, and a small portion
of Taylor County.
Gum Creek, Wolf Creek, Beasleys Creek, and Jones Mill Creek
and many others are tributary to the Aucilla River.


17






18 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

WACISSA RIVER VALLEY LOWLANDS

The Wacissa River's origin is a series of springs near the town
of Wacissa in Jefferson County. The river is fairly shallow with
rapids along its course, and flows across the Gulf Coastal Lowlands
in a channel cut into Suwannee Limestone and the St. Marks
Formation. The flood plain of the river is 1 to 3 miles wide and
although ill-defined in some areas, it is distinguishable as swamps
on aerial photographs. Stream terraces are not visible along the
river's valley.
Near the confluence of the Wacissa and Aucilla rivers, the
Wacissa becomes a multichanneled stream. Observation of aerial
photographs shows that the bends in the river seem to indicate
that some of these channels are oriented with northwest-southeast,
and northeast-southwest linear trends. It is also possible that the
bedrock is dolomitized or silicified and offering considerable resis-
tance to erosion; consequently, the stream, in seeking zones of less
resistance has formed multichannels. The water is clear in the
upper reaches of the Wacissa because the source is springs, but
in the lower reaches it becomes charged with humic acid waters
from the swamps, and is high in color.
Welaunee and Cow creeks are tributary to the Wacissa River.



ST. MARKS RIVER VALLEY LOWLANDS

The St. Marks River has its headwaters in Leon County and
only flows a few miles through Jefferson County. The river is
sluggish and flows in a valley approximately a mile wide. Along
most of its course swampy conditions prevail, and the river water
is charged with humic acids giving it a high color. The course of
the river in Jefferson County seems to be somewhat controlled
by the dunes. The Cody Quadrangle map shows that the river
has a meandering course that is oriented with dune development.
In the area where the St. Marks leaves Jefferson County the flood
plain of the river is very swampy and difficult to delineate.
Tributary to the St. Marks are Burnt Mill Creek (enters the
St. Marks in Leon County), Sweetwater and Moore branches.
Sellards (1910, p. 61) believed that a stream flowed through
what is now Lake Miccosukee basin into the St. Marks River.
He also stated that Lloyd Creek during periods of excessive runoff
emptied into the St. Marks River.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


LAKES

Sellards (1910, p. 47-76) published significant information on
lakes in Florida. He discussed lakes in the State that were peculiar
in character and manner of development. He concluded that most
of the shallow lakes in Florida, which included Lake Miccosukee in
Jefferson County, were originally stream channels that have been
lowered by solution, and greatly enlarged laterally by the formation
of sinkholes. He noted that as each new sink formed, the older
sinks became clogged and partially filled with sediments washed
into them from the lake basins in which they occur.
White (1958, p. 66-73) believes that most of Florida's shallow
lakes are the result of solution along the surface of the underlying
limestone caused by lateral movement of the ground water over
the soluble limestone. The depth that solution takes place is
controlled by the depth at which the lateral movement of the
ground-water table occurs. White (1958, p. 66-73) further states
that basin excavation by sinks might be the reason why the water
in the lake basins has disappeared, rather than why the lakes
have formed.
Lake Miccosukee, located in the Tallahassee Hills province, is
irregular in shape with an area of about 5,000 acres. Located near
the north end of the lake is a sinkhole, which has been ringed
by an earthen dam to prevent the sinkhole from draining water
from the lake. Wards Creek which enters the southeast end of
the lake is an intermittent stream that only supplies water to the
lake basin during periods of high runoff. The main source of water'
for the lake is from rainfall in the immediate area. The growth
of aquatic vegetation is so prolific in parts of the lake that boat
travel is restricted to channels cut through the vegetation.
When the water level of the lake is normal or above its normal
stage, surface flow occurs through an outlet in the southern part
of the lake. Northeast of Lloyd a series of sinkholes lie along the
course of the drain and captures much of the water. According
to Sellards (1910, p. 61):

"Lake Miccosukee probably represents a basin developed by
solution near the headwaters of streams originally tributary
to St. Marks River. Previous to the formation of Miccosukee
Basin the drainage of this part of the county doubtless
passed through small streams, to the south past the present
village of Lloyds, then to the Gulf through the St. Marks
River."






20 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

The bedrock map, figure 8, indicates that Lake Miccosukee
overlies a basin in the limestone. It appears from the available
data that the Miocene St. Marks Formation is missing, and the
basin is formed in the Oligocene Suwannee Limestone.
The piezometric surface in the area around Lake Miccosukee
is 40 to 60 feet above mean sea level, and 20 to 40 feet below the
lake surface. Consequently, ground-water recharge is taking
place through the sinkholes in the lake region.

SPRINGS

The springs that form the headwaters of the Wacissa River
are discussed by Ferguson and others (1947, p. 88-91), and except
for the measurements made on Big Spring and Blue Spring on
December 7, 1960, they state:

WACISSA SPRINGS AT WACISSA

"Location-The group of springs known as Wacissa Springs
are located 1 mile south of the town of Wacissa.
Description-These springs comprise the headwaters of Wacis-
sa River and are located within 0.8 mile of the head of the
Wacissa River.
Wacissa Springs are composed of the following springs: Big
Spring, Garner Springs, Blue Spring, Buzzard Log Springs, Min-
now Spring, Cassidy Spring, two apparently unnamed springs
herein designated as No. 1 and No. 2, Thomas Spring, and Log
Springs.

BIG SPRING

Big Spring, sometimes known as Big Blue Spring, consists of
a circular pool approximately 90 feet in diameter. Having a cavity
about 70 feet in diameter whose side walls drop almost vertically
to a depth of about 40 feet. The cavity is in limestone which appears
to be cavernous on both the east and west sides. Soundings indicate
a maximum depth of 45 feet. The bottom of the pool is covered
with a layer of silt approximately one foot in depth. The average
depth of the pool away from the cavity varies from 2 to 5 feet.
The spring flow discharges into two runs, one flowing southwest
and the other flowing northwest, both entering the Wacissa River
within 0.2 mile of each other. The runs are full of eel grass and
measurements of the discharge are made very difficult. The run







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


G E O R G I


-- 1 0 1 2 3 4 5 MILES
SCALE


o
/


*\~ 4
C'
3


of ~IEX.
c6te


EXPLANATION


STATE BOARD of CONSERVATION


prepared by DIVISION of GEOLOGY


Figure 8. Contours showing approximate altitude of the top of the first
limestone in Jefferson County, Florida.


A


A OUTCROP
o WELL OR CORE HOLE
io ALTITUDE IN FEET, OF TOP
OF FIRST LIMESTONE
REFERRED TO MEAN SEA LEVEL
L10- LINE, IN FEET, REFERRED TO
MEAN SEA LEVEL
CONTOUR INTERVAL 20 FEET
AREA WHERE ST MARKS IS
FIRST LIMESTONE PENETRATED
IIIIII AREAWHERE SUWANNEE IS
FIRST LIMESTONE PENETRATED


21






22 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

flowing northwest is approximately 0.2 mile in length and 80 feet
in width, the dimensions of the other were not determined.

GARNER SPRINGS

Garner Springs consists of two headpools. In the smaller a
limestone cavity, 8 feet in diameter, has a maximum depth of
6.3 feet. It was impracticable to get to the larger of the spring-
heads because its outlet channel was obstructed by fallen trees.
This spring run is approximately 800 feet long and 50 feet in
width and is full of eel grass and other aquatic growth.

BLUE SPRING

Blue Spring consists of a circular pool with a limestone cavity
about 40 feet in diameter, which has a maximum depth of 19.0
feet. The spring run is about 900 feet long and approximately
50 feet in width. The run is full of eel grass and aquatic vegeta-
tion and the surface has a scum of "duck seed."

BUZZARD LOG SPRINGS

Buzzard Log Springs consists of four springheads, two being
at the confluence of the run with the Wacissa River and the other
two at the head of the run which is approximately 0.2 mile in
length. The maximum depth of the two spring cavities at the
mouth of the run was 8.1 feet and the flow emerges from limestone
in one and apparently from a sand boil in the other. It was imprac-
ticable to get to the head of the run due to the stream being
obstructed by logs. The run is covered with "duck seed" and is
full of aquatic growth.

MINNOW SPRING

Minnow Spring consists of a circular pool with a limestone cavi-
ty about 15 feet in diameter in the bottom at a maximum depth of
8.1 feet. The water in the boil of the spring is filled with sand
particles flushed out of the cave. The run is approximately 100
feet in length and flows in an easternly direction.

CASSIDY SPRING

Cassidy Spring consists of a pool with a limestone cavity at the
bottom 8 feet in diameter and in a maximum of 28.0 feet of water.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


The run is approximately 70 feet long and discharges into the
Wacissa River.

SPRING NO. 1

Spring No. 1 consists of a cavity in a limestone outcrop within
the Wacissa River. The maximum depth of the pool cavity was
24.7 feet.

SPRING NO. 2

Spring No. 2 discharges from a circular cavity in a limestone
outcrop beneath a maximum of 18.9 feet of water in the Wacissa
River.

THOMAS SPRING

Thomas Spring discharges from a limestone cavity approxi-
mately 8 feet in diameter under the Wacissa River at a maximum
depth of 28.2 feet.

LOG SPRINGS

Log Springs discharges from two cavitiies within a limestone
pool 40. feet in length by 15 feet in width. The maximum depths
to the floors of the cavities are 28.2 feet and 24.0 feet, respectively.
Sand Spring boils are visible at many points along the stretch
of the river from Teate's fish camp to the head of the Wacissa
River. There are believed to be additional springs upstream from
Thomas Spring, downstream from the mouth of Big Spring Run
and also in Little River. These were not investigated.

DISCHARGE

The following measurements of discharges were made on July
16, 1942:

BIG SPRING

Big Spring-The total discharge was found to be 69.4 (64.5
second-feet total, Dec. 7, 1960) second-feet which was comprised
of a discharge of 22.7 cfs (15 mgd) in the southwest run, and
46.7 cfs (30 mgd) in the northwest run or a total of 41.7 mgd
on December 7, 1960.






24 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

GARNER SPRING

Garner Spring-17 cfs (11 mgd) measured 200 feet below the
head of the smaller spring.

BLUE SPRING

Blue Spring-9.43 cfs (6 mgd) measured 300 feet below the
head of the spring (2.6 cfs, Dec. 7, 1960).

MINNOW SPRING

Minnow Spring-5 cfs (3 mgd), estimated.
Big Spring, Garner Springs, Blue Spring, Buzzard Log Springs,
Minnow Spring, Cassidy Spring and Log Springs discharge into
the Wacissa River. Thomas Spring, Spring No. 1 and Spring No. 2
are within the Wacissa River channel and therefore their flow
would be difficult to measure.

UTILIZATION

The springs are intact in their natural surroundings. A group
of men at one time were said to have been interested in developing
the springs as an attraction for tourists but the plan never mater-
ialized. The river in the vicinity of Springs No. 1 and No. 2 is used
for swimming. The runs of the various springs are frequented
by fishermen, owing to the abundance of fish.

OTHER SPRINGS

Walker Spring, also in Jefferson County, is 8 miles southeast
of Lamont."

LINEAR TRENDS

Vernon (1951, p. 47) recognized faulting and extensive frac-
ture patterns in Florida. The fracture patterns were mapped on
the basis of their physiographic expression, as shown on mosaics
of aerial photographs.
In Citrus and Levy counties (Vernon, 1951, p. 47) the axis
of the Ocala uplift is paralleled by regional fractures trending
northwest-southeast, exactly marking the crest of the anticline.
A secondary system crosses the primary system at large angles and






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


trends northeast-southwest. According to Vernon (1951, p. 48)
the northwest plunge of the Ocala uplift extends through Madison
County into Jefferson County.
Examination of a mosaic of aerial photographs of Jefferson
County shows that northeast-southwest and northwest-southeast
linear trends exist in the county, as shown in figure 9. The multi-
channels of the Wacissa River in its lower reaches may be the
result of the stream following fractures in the Suwannee limestone.
Certain portions of the Aucilla River also seem to be following
linear trends. The lack of subsurface control and surface ex-
posures makes it difficult to determine whether or not all the map
lineations represent fractures. However, fractures do exist in the
county because the writer observed a large one in the limestone at a
spring near the headwaters of the Wacissa River. The trend of the
fracture was northeast-southwest. This particular fracture was not
seen as a distinct lineation on the aerial mosaic but as figure 9
shows, a northeast-southwest linear zone passes just north of the
headwaters of the Wicassa River, to which it may be related. The
structure map showing the configuration of the top of the Suwan-
nee Limestone, as shown in figure 10, indicates that a northwest
slope of a Suwannee high almost parallels the northeast-southwest
linear trend mentioned above. Observation of the bedrock map (fig.
8) shows that the St. Marks does not reflect the slope that occurs
within the underlying Suwannee positive area thus, apparently,
ruling out a surface fault. It may mean, however, that the linea-
tion is a fracture that extends through the Miocene clastics over-
lying the limestones of the St. Marks Formation and the Suwannee
Limestone.


STRATIGRAPHY

INTRODUCTION

The sediments that occur in Jefferson County range in age from
Paleozoic to Recent. The Suwannee Limestone (Oligocene) is
the oldest rock exposed in the area, and the deposits laid down
during the Recent are the youngest. Table 3 is a list of the
geologic formations that occur in Jefferson County.
Most of the subsurface data discussed in this report was ob-
tained from studying well cuttings, and core samples, figure 11.
Data on the age of rock older than late Eocene was from two oil
exploratory wells. The discussion of the older sediments encoun-








26 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

V----


G


E 0 R G I A


1 0 1 2 3 4 5MILES
SCALE


PP. 3I e ; say
Sp MEC 0


Figure 9. Linear trends in Jefferson County, Florida.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


E O R G I A


1 0 1 2 3 45 MILES
SCALE


OUTCROP
o WELL OR CORE HOLE
10 ALTITUDE IN FEET, OF TOP
OF SUWANNEE LIMESTONE
REFERRED TO MEAN SEA LEVEL
,-10-,LINE, IN FEET, REFERRED TO MEAN
SEA LEVEL
CONTOUR INTERVAL 20 FEET


STATE BOARD of CONSERVATION


prepared by DIVISION of GEOLOGY


Figure 10. Contours showing approximate altitude of the top of the
Suwannee Limestone Jefferson County, Florida.


G


1e




OF M EXICO


27







28 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

TABLE 3. Geologic Formations in Jefferson County, Florida.

Era System Series Group Formation

Recent Stream alluvium
Quaternary
Pleistocene Terrace sands

Miccosukee Formation
Miocene Hawthorn Formation
St. Marks

Cenozoic Oligocene Suwannee Limestone

Crystal River Formation
Tertiary Ocala Williston Formation
Inglis Formation

Avon Park Limestone
Eocene
Lake City Limestone

Paleocene Beds of Midway Age

Beds of Taylor Age
Cretaceous Gulf Beds of Austin Age
Atkinson Formation

Undifferentiated
Comanche Shales and sands

Varicolored shales and
Upper Newark sand associated with
Mesozoic Triassic (?) diabase sills or dikes

Lower
Paleozoic Ordovician Quartzitic sandstone
(?)



tered in these two wells will be generalized, and, for the most
part is taken from other sources.
Table 4 lists wells in Jefferson County from which geologic
data was obtained.
Jefferson County lies within or near a zone of facies change
and, so that a better understanding of how the county fits in with
the general stratigraphy of Florida, the following statement of
Applin and Applin is cited (1944, p. 1679-80):

"Beds from the top of the Oligocene to the base of the
late middle Eocene are a continuous limestone sequence
throughout the area, whereas two sedimentary or deposi-
tional faces are recognized in Florida and Southern Georgia,
in each stratigraphic unit between the top of the early









GEOLOGY OF JEFFERSON COUNTY, FLORIDA


R3E + R4E + R5E E R6E




G E O R G


R3 E 4- R4E -- R5E


STATE OF FLORIDA
STATE BOARD OF CONSERVATION
JEFFERSON COUNTY
prpdred by
DIVISION OF GEOLOGY

R6E R7E


Figure 11. Well locations and lines of sections in Jefferson County, Florida.


29


R7E




A


_ ~~














TABLE 4. Geologic data from selected wells in the Jefferson County area.
Source of data: s-samples; d-driller's log; el-electrical log;
gr-gamma ray log.


Elevation
This report land
well number surface


WJf-3N-3E-36 ca
WJf-3N-4E-18 bc
WJf-3N-4E-34 da
WJf-3N-4E-24 bd
WJf- 150

WJf- 155
WJf-3N-5E-25 dd
WJf-3N-6E-23 cc
WJf- 181
WJf-3N-7E-27 bb
WLn-2N-3-E-35 cc
WJf-2N-4E-16 ca
WJf-2N-4E-12 ab
WJf-2N-4E-25 center
WJf-2N-5E-5 center
WJf-2N-5E-7 cc

WJf-2N-5E-17 ba
WJf-2N-5E- 5 ca
WJf-2N-5E-17 cc
WJf-2N-5E-25 da
WJf-2N-5E-30 aa

WJf-2N-5E-30 bb
WJf-2N-5E-30 da
WJf-2N-6E- 1 dd
WJf-2N-6E- 6 da
WJf-1N-3E-15 cc


213.74
108.82
110.30
153.21
193.00

124.66
188.00
154.14
117.80
98.32

93.12
149.00
190.00
203.00
146.00

209.56
74.51
217.94
156.49
237.01

209.84
210.34
184.09
189.65
95.82


Altitude in feet referred to mean sea level


Recent and Upper
Pleistocene Miocene


213.74
108.82
110.30
153.21
193.00

124.66
188.00
154.14
118.00
98.00

93.12
149.00
190.00
203.00
146.00

209.56
74.51
217.94
156.49
237.01

209.84
210.34
184.09
189.65
95.82


Middle Lower
Miocene Miocene


165.0
39.0
61.0
133.0
158.0


110.0
19.0

88.0
93.0


? 47.0
? ?
113.0
43.0
54.0 26.0


63.0
79.0
140.0
147.0
86.0

170.00

146.0

187.0

?155.0
121.0
148.0
157.0
74.0


40.0

120.0
73.0
66.0

106.0

114.0
45.0
127.0

130.0
91.0
103.0
131.0
56.0


Upper Sour(
Oligocene Eocene da


-10.0
6.0
55.0
63.0
28.0

25.0
48.0
67.0
28.0
- 6.0

26.0
59.0
40.0
51.0
46.0

82.0
35.0
53.0

37.0


8.0

96.0
-28.0


-100.0


S
el.,
el.,



S
S
el.,

S
S
S, e
S
S

S, e
S
S
S
S

S
S
S
S
S, e


-283


ce of
tta




gr. -
gr.





gr.

ti
Sgr.


I., gr.


O





*1., gr. Z

H


Division
of
Geology
W-No.


W-6933
W-6186
W-6029
W-5719
W-5703

W-5702
W-5701
W- 319
W- 97

W-3320
W-6185
W-4733
W-6607
W-6927
W-3871

W-5302
W-4813
W- 19
W-5432
W-3204

W-6043
W- 14
W-6561
W-6911
W-5504









TABLE 4. CONTINUED.


Altitude in feet referred to mean sea level
Elevation
This report land Recent and Upper Middle Lower Upper
well number surface Pleistocene Miocene Miocene Miocene Oligocene Eocene


Division
of
Geology
W-No.


W-5434
W-6061
W-6932
W-6517
W-6559

W-6560
W-6558
W-6906

W- 905

W- 906
W-6402
W-6930
W-6931

W-5455
W-6925
W-5325
W-6174
W-1854

W-6518
W-6527
W-6526
W-6525


196.68
121.59
214.00
87.89
80.00

82.00
115.59
165.44
40.00
187.45

169.36
205.00
127.98
200.00
178.83

73.90
134.00
86.63
68.05
37.00

29.00
14.09
13.00
6.00


WJf-1N-4E- 1 bb
WJf-1N-4E-30 da
WJf-1N-4E-35 ca
WJf-1N-5E-16 bc
WJf-1N-5E-25 ca

WJf-1N-6E- 8 dd
WMd-1N-6E- 9 cor. d
WJf-1S-3E-13 aa
WJf-1S-3E-30 ca
WJf-1S-3E-25 db

WJf-1S-3E-25 db
WJf-1S-4E- 1 bc
WJf-1S-4E-14 ab
WJf-1S-4E-29 cb
WJf-1S-4E-28 ac

WJf-1S-5E- 6 cd
WJf-1S-5E-32 ac
WJf-1S-5E- 1 ad
WJf-1S-5E-22 bc
WJf-2S-3E- 1 ad

WWk-2S-2E-36 db
WJf-3S-3E-30 ac
WJf-3S-3E-28 dc
WTy-4S-3E-24 dd


196.68
121.59
214.00
88.89
80.00

82.00
115.59
165.44

187.45

169.36
205.00
127.98
200.00
178.83

74.90
134.00
86.63
68.05


142.0
97.0
139.0
43.0
10.0

36.0
100.0

112.0

154.0
- 2.0
140.0
151.0

50.0
99.0

40.0


102.0 2.0
38.0 54.0
17.0 18.0
23.0 5.0
00.0 5.0


25.0

43.0

- 4.0
106.0
00.0
110.0
100.0


-109.0
- 64.0
3.0

- 22.0

- 22.0
23.0
73.0


? 5.0
89.0 84.0
10.0
7.0
8.0 3.0


9.0
7.0
10.0


17.0


- 7.0
- 24.0
- 12.0
0.0


0
Source of O
data l


S
S, el., gr. O
S, el., gr.
S
S


S I
S 0
S
S 0
s 3



S
S


el., gr.

S
S
s r
S
S
S, el.

S
S
s


37.00

29.00
14.09
13.00
6.00






32 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

middle Eocene and the base of beds of Austin age (Upper
Cretaceous). On the one hand, west Florida and southern
Georgia are occupied by a elastic facies which is similar in
its broader aspects to the sediments of the western Gulf
Coastal Plain and is composed largely of sand and shale with
some limestone and chalky marl. On the other hand, over
most of the peninsula, the sedimentary section is almost
continuous limestone from the top of the Oligocene into the
Lower Cretaceous, giving a known thickness for this facies
of more than 10,000 feet in southern Florida. Anhydrite and
gypsum are present in this facies from late middle Eocene
to Paleocene and also in the limestone of the Lower Cretace-
ous, but little has been noted in the Upper Cretaceous units.
Thin streaks of carbonaceous shale and lignite are found in
the central part of the peninsula in the limestone facies of
the middle Eocene. In northern Florida and in the north
quarter or north third of the peninsula, the limestone and
plastic facies grade laterally into each other. In general,
with the passage of time, the limestone of the peninsula
encroaches upon the elastic facies, spreading northward in
successive stages, so that by the end of early middle Eocene
the limestone facies occupies all of the peninsula, northern
Florida, and southern Georgia. In general also, the fora-
miniferal microfaunas of the elastic facies resemble those
present in formations in the western Gulf Coast, whereas
the microfaunas of the limestone facies in the peninsula
from the top of the early middle Eocene to the top of the
beds of Taylor age resemble those of Cuba, the West Indies,
Mexico, and Europe, with only a few species present that are
known in other places in the United States. Species of
ostracods and bryozoans show a like dissimilarity with those
found in western faunas. Beginning with the top of the
beds of Taylor age in the peninsula, the more familiar Gulf
Coast microfaunas again appear. Some mingling of faunas
of the two facies has been noted in a few wells in north
Florida in the early middle and lower Eocene, but none in
Paleocene or late Upper Cretaceous. The fauna of the Lower
Cretaceous limestones of southern Florida again resembles
that found in certain derived deposits in Cuba and also that
of the El Abra limestone of southern Mexico (Cenomanian-
Albian) there designated as Middle Cretaceous."






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


PALEOZOIC ERA

ORDOVICIAN (?) SYSTEM

According to Applin (1951, p. 23), Coastal Petroleum Company,
E. P. Larsh No. 1, penetrated Paleozoic quartzitic sandstone at a
depth of 7,909 feet. He assigned it to the Lower Ordovician (?)
undifferentiated, but stated that only 4 feet of these sediments
were penetrated and could be a boulder in the lower part of the
Mesozic (personal communication, August, 1963).


MESOZOIC ERA

TRIASSIC SYSTEM

Newark (?) Group

Varicolored shales and sands of Triassic Age were reported
by Applin (1951, p. 10-26) in the Coastal Petroleum Company,
E. P. Larsh No. 1 test well at a depth of 6,800 feet. Near the base
of the well, from 7,850 to 7,890 feet, volcanic diabase sills or dikes
are associated with these plastic rocks of Triassic (?) Age, (Applin,
1957, p. 1489). Applin (personal communication August 1, 1963)
now refers the above sediments to the Upper Triassic (?) Newark
(?) Group, and also lowered the top of the Triassic beds to 7,030
(?) feet.


CRETACEOUS SYSTEM

Comanche Series

The two deep oil tests drilled in Jefferson County penetrated
beds of the Comanche Series. These beds consist of varicolored
shales interbedded with quartz sands and limestone.
The Comanche Series was penetrated in the Coastal Petroleum
Company, E. P. Larsh No. 1 test well, located in the NW1/4SE1/4
sec. 1, T2S, R3E, at the depth of 3,875 feet (Applin, personal
communication Aug 1, 1963), and the Southern States Oil Corpora-
tion test well, located in the SW4SW1/, Sec. 17, T2N, R5E, at
3,800 (?) feet. The thickness of the Comanche Series in the
Coastal-Larsh well is 3,155 feet.






34 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

Gulf Series

Studies made by Applin and Applin (1944, 1947) and the
Southeastern Geological Society Mesozoic Committee (1949)
placed the Upper Cretaceous sediments occurring in Jefferson
County in the Gulf Series. According to these reports, Jefferson
County lies within or near the zone where the carbonate facies
of peninsular Florida meet the Clastic facies of western Florida.
The Gulf Series in Jefferson County, from oldest to youngest
beds, consists of the Atkinson Formation, beds of Austin Age. and
beds of Taylor Age.

ATKINSON FORMATION

The Applins (1947) introduced the name Atkinson Formation
for those subsurface sediments occurring in Alabama, Georgia,
and north Florida that lie between the top of the Lower Cretaceous
and the base of the beds of Austin Age. On the basis of differences
in lithology, they divided the Atkinson into three unnamed mem-
bers (upper, middle, and lower) and also recognized two
microfaunal groups within the Atkinson Formation. The upper
member carries a fauna closely related to that of the Eagleford
shale in Texas and the middle and lower members contain a fauna
similar to that of the Woodbine Sand in Texas. On the basis of
this faunal difference The Southeastern Geological Society Mesozoic
Committee (September, 1949) divided the Atkinson Formation
into an "A" zone, which contains the Eagleford fauna, and a "B"
zone, which contains the Woodbine fauna. To facilitate the
correlation of the Atkinson Formation of the southeastern gulf
region with the Eagleford and Woodbine Formations of Texas,
Esther R. Applin (1955, p. 1511) redefined the Atkinson to consist
of two members; an upper member, of Eagleford Age, and a lower
member of Woodbine Age. The lower member includes the middle
and lower members as originally defined by Applin (1947).
According to Paul L. Applin (personal communication August 1,
1963) in the Southern States Oil Corporation, Millard and Gossard
No. 1, ". . the sandy beds in the lower part of the lower Atkinson
are absent, and the 'marine shale' (formerly called middle
Atkinson) rests unconformably on the Comanche Series." The top
of the upper member of the Atkinson occurs from 3,410 (?) to
3,655 (?) feet, and the lower member is encountered from 3,665
(?) to 3,800 (?) feet in the Southern States well, thus giving the
formation a total thickness of 390 feet. Lithologically the upper







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


member is brownish to greenish gray shale, interbedded with some
fine grained glauconitic sandstone containing microfossils and
molluscan shell fragments. The lower member is primarily a dark
gray microfossiliferous shale.
The upper and lower members of the Atkinson Formation are
present in the Coastal Petroleum, E. P. Larsh No. 1 oil test well.
The upper member occurs from 3,400 to 3,700 feet, and is a
greenish gray and gray calcareous sandy shale; and a greenish gray
to gray, fine to medium glauconitic quartz sand. The upper member
is characterized for the foraminifers Planulina eaglefordensis,
Valvulineria infreqeuns, Gumbelina moremai, Gumbelina reussi,
Globigerina cretacea, and Trochammina wickendeni. The lower
member of the Atkinson is encountered from 3,700 to 3,875 feet
(Applin, personal communication, August 1, 1963) and is a gray
to gray-green glauconitic, fine to medium, quartz sand; and a gray
to dark gray sandy shale. The foraminifers Ammobaculities braun-
steini, Ammobaculites comprimatus, Ammobaculites advenus, Am-
mobaculites plummerae, and Trochammina rainwater characterize
the lower member.


BEDS OF AUSTIN AGE

Beds of Austin age occur from the depth of 3,268 to 3,410 (?)
feet in the Southern States Oil Corporation oil test well, and the
formation consists of gray, chalky, microfossiliferous limestone,
gray calcareous shale, brown-speckled shale, and hard gray marl
(Applin and Applin, 1944, p.1472-73). The lithology of the Austin
beds occurring in the Coastal-Larsh oil test are similar to those
described above in the Southern States Oil Corporation well, and
range in depth from 2,890 to 3,400 feet.


BEDS OF TAYLOR AGE

The upper beds of Taylor Age are missing in the Southern
States Oil Corporation oil test well, and the first penetration is
in beds of lower Taylor Age at 3,056 feet, (Applin and Applin, 1944,
p. 1711). In the southern part of Jefferson County, in the Coastal-
Larsh No. 1 oil test, beds of Taylor Age occur in the interval-
2,890 to 3,400 feet. Lithologically the Taylor is composed of gray
chalk, and a gray calcareous microfossiliferous shale containing
Inoceramus fragments.







36 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

CENOZOIC ERA

TERTIARY SYSTEM

Paleocene Series

BEDS OF MIDWAY AGE

The Applins (1944, p. 1703) recognized beds in the Tallahassee
area containing a microfauna similar to the foraminifers found
in the Tamesi (Velasco) of Mexico. They consider this faunal
unit a part of the Midway Group. In the Southern States Oil
Corporation oil test well, located in Jefferson County, this fauna
occurs from 2,490 feet to approximately 3,056 feet (Applin and
Applin, 1944, p. 1706). In the southern part of Jefferson County,
the writer also found the Tamesi fauna in the Coastal Petroleum
Co., Larsh No. 1 oil test well in the intervals-2,510 to 2,560 feet.
The lithology of this unit is a dark gray, very calcareous, slightly
glauconitic, clay containing abundant microfossils.

Eocene Series

WILCOX UNDIFFERENTIATED

In the Southern States Oil Corporation, oil test well, Applin and
Applin (1944, p. 1701) designated a plastic interval of fine to very
fine grained, glauconitic and microfossiliferous quartz sand
occurring between 2,223 and 2,490? feet as Wilcox Stage. This
determination was on the basis of several species of Globigerina
and Globorotalia, and Globototalia wilcoxensis Cushman.

CLAIBORNE STAGE

LAKE CITY LIMESTONE

The Lake City Limestone was proposed by Applin and Applin
(1944, p. 1693) for a limestone faces of early middle Eocene
occurring in north Florida and peninsular Florida.
The Lake City Limestone in Jefferson County consists of
cream to light brown, slightly peat flecked, medium hard,
limestone (calcarenite). It is gypsiferous, glauconitic, cherty,
microfossiliferous and has moderate to good porosity. In the
Southern States Oil Corporation oil test well, the Lake City
Limestone was encountered from 1,740 to 2,223 feet, a thickness







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


of 483 feet (Applin and Applin, 1944, p. 1695). In the Coastal-
Larsh well the Lake City is from 970 to 1,820 feet, a thickness of
850 feet. The foraminifer Dictyoconus americanus is a principal
fossil guide to the Lake City Limestone, and occurs in abundance
in the Larsh well.

AVON PARK LIMESTONE
The Avon Park Limestone was proposed by Applin and Applin
(1944, p. 1686) for the upper part of late middle Eocene deposits
found in a well at the Avon Park Bombing Range, Polk County,
Florida. Florida Geological Survey well No. W-668 was designated
as the type well.
The Avon Park Limestone in Jefferson County is a very pale
orange, medium hard, moderately porous, gypsiferous, microfos-
siliferous, cherty, partially recrystallized to crystalline limestone
(calcarenite). Near the bottom of the Avon Park, the sediments
became peat flecked and dolomitized. In the Southern States Oil
Corporation well the Avon Park Limestone occurs from 880 to
1,740 feet, a thickness of 860 feet. The complete Avon Park
Limestone interval in the Coastal-E. P. Larsh No. 1 test well is
unknown because of a sample gap from 160 to 925 feet.

OCALA GROUP

For historical review of the term Ocala prior to 1957, Florida
Geological Survey Bulletin 38 is cited as a reference. Puri (1957,
p. 22-24) redefined the Ocala Limestone and raised it to the rank
of group and subdivided it into three formations which are in
ascending order: The Inglis Formation, the Williston Formation,
and the Crystal River Formation.

INGLIS FORMATION
The Moodys Branch Formation, consisting of two members,
the Inglis and Williston, was proposed by Vernon (1951, p. 115-
116) for basal sediments of late Eocene age in Florida. Puri (1957,
p. 24) later raised the Inglis Member to the rank of formation.
The Inglis Formation in Jefferson County is a tan, soft to
medium hard, moderately porous, gypsiferous, microfossiliferous,
partially dolomitized, crystalline limestone (calcarenite). In the
vicinity of Monticello the top of the formation occurs at 780 feet
and the base at 880 feet, a thickness of 100 feet.






38 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

WILLISTON FORMATION
The Williston member was proposed by Vernon (1951, p. 141)
for about 30 feet of foraminiferal limestone overlying the Inglis
member of the Moodys Branch Formation. The Williston member
was raised to the rank of formation by Puri (1957, p. 28-29).
The Williston Formation occurs from 705-780 feet, a thickness
of 75 feet in a well near Monticello. Lithologically, the Williston
Formation is a pale orange, moderately porous, microfossiliferous,
crystalline to partially recrystallized limestone (calcarenite).

CRYSTAL RIVER FORMATION
Puri (1953, p. 130) proposed the Crystal River Formation to
replace Vernon's Ocala limestone (restricted). The type locality
of the Crystal River Formation is in the Crystal River Rock
Company quarry, Citrus County, Florida, where 108 feet of lime-
stone is exposed.
The Crystal River Formation primarily consists of a pale
orange, soft to medium hard, good to moderately porous, microfos-
siliferous, partially recrystallized limestone (calcarenite). In some
instances it is a calcirudite because of the large number of
Lepidocyclina specimens. In the vicinity of Monticello the Crystal
River Formation is 205 feet thick and occurs from 500 to 705 feet.


Oligocene Series

VICKSBURG GROUP

SUWANNEE LIMESTONE

History.-Cooke and Mansfield (1936) applied the name Suwannee
Limestone to the fossiliferous limestones cropping out along the
Suwannee River from White Springs to Ellaville. The history of
the stratigraphic nomenclature of the Suwannee Limestone has
been adequately discussed in Florida Geological Survey Bulletins
21 and 29, and are cited as very good references for historical
information.
Distribution.-The Suwannee Limestone is the oldest rock crop-
ping out in Jefferson County and the area of outcrop is shown on
the geologic map (Plate 1). It extends from the Wakulla-Jefferson
County lines eastward along the edge of secs. 31 and 32, T3S, R3E,
for about 2 miles before turning northward and intersecting U. S.






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


Figure 12. Dolomitized Suwannee Limestone cropping out on the bank of
the Aucilla River, Jefferson County, Florida.


Highway 98 on the east side of Gum Creek. From U. S. Highway
98 the outcrop pattern continues northward, almost parallels State
Highway 59, and finally merges with the Cody Scarp (fig. 5) north
of the town of Wacissa. The Suwannee Limestone, in many areas,
is covered by a thin veneer of Pleistocene sand. However, from
just below Lamont to just north of Nutall Rise, it is almost
continually exposed along the banks of the Aucilla River either
as silicified boulders, or as massive dolomite beds, figure 12. Both
the dolomite beds and the silicified boulders often form rapids
along the river, figure 13.
The Suwannee Limestone is exposed in the bed of the Wacissa
River from just below its headwaters near the town of Wacissa
to the confluence with the Aucilla River, just above Nutall Rise.
North of Cody Scarp the formation is covered by younger deposits.
However, a few outcrops have been observed, such as the outcrop
of silicified Suwannee Limestone occurring on the rim of a sinkhole
lake on sec. 32, T3N, R6E, and at a locality LJf-1S-5E-12-bb
located north of Lamont. As shown in the geologic cross sections,
figure 14, the Suwannee is continuous over all of Jefferson County
and in many places is the first bedrock encountered. Silicified or


39






40 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


Figure 13. Rapids on the Aucilla River caused by dolomitized Suwannee
Limestone, Jefferson County, Florida.


dolomitized Suwannee Limestone forms the bottom of the Gulf
of Mexico off Jefferson County, shown in figure 15.
General Lithology.-The Suwannee Limestone is a marine lime-
stone consisting of a partially recrystallized limestone (calcare-
nite). It is very pale orange, finely crystalline, weakly cemented
with CaCO3, with moderate to good porosity, and very fossiliferous.
Chemically, it will approach 97 percent CaCO,.
Silicified limestones are very common in the outcrop area in
the form of boulders, shown in figure 16. In some cases the top of
the formation is silicified in the subsurface. Examination of well
cuttings indicates dolomitization of the limestone has also occurred
in the subsurface at different depths and in the outcrop area,
especially along the Aucilla River.
A lithology different from that at the type locality of the
Suwannee Limestone was noted from cuttings and cores for several
wells in the county. It is a limestone (calcirudite) characterized
by Lepidocyclina specimens. Generally, most of the microfauna is
so poorly preserved, they are difficult to identify. In core hole
WJf-1N-5E-25-ca, near Aucilla, a Lepidocyclina horizon was





NORTH


Correction to Vertical Scale on Section A-t,.
Elevation should be moved down one Interval. SOUTH
Sea Level is at the -40 interval.


40-T .... LJf-3S-3E-21bd -I 40

40 -40
.80 -80 0
2o SECTION A-A' -lr-120 .
EXPLANATION SETO o

PLEISTOCENE TERRACE DEPOSITS WEST EAST
WEST---36caWJf-2N-5E-5 center WJf2N6E6d24 A
E MICCOSUKEE FORMATION 240- WJ3N-3E-36ca WJf-3N-4E-34daWf-N-6E-6da Jf-2N-6E-Idd -240
200- -200 B B
I HAWTHORN FORMATION 160- -160
ST.MARKS FORMATION 12 1
SUWANNEE LIMESTONE 40- 40
-0 LOCATION
-40 SECTION B-B -40 of 0
2 1 0 1 2 3 4 5MILES -0- 80f0 D CROSS
___ _, SECTIONS
AH
WESTEAST WEST EAST
240 T WMd-IN-GE-gcorner d -240
240 WLn-IS-2E-3ad WJf-IN-4E-30ca W df-IN -6E-9corner 240 LJf-3S-3E-28dd LJf-3S-4E-28db
20 WJf-IN-5E-b 5-3F- LJf-3S-4E-28da
LEON CO.! JEFFERSON CO. WJf-IN-6E-8dd 160 WJf330-3- LJf-3S-3E-27dd
0 120 30 Wacissa River30
S120- -120 30 t
o80- -80
40- 40 0 0
0- -0
-40- 0 -30 -30
-80 -- 80 O
-10 SECTION C-C --120 SECTION D-D'I

Figure 14. Geologic cross sections in Jefferson County, Florida.


---- .--~- __ _____ __ ~_ _~__ __ C __~ __.__ .__ ~ ______I_ ______ ___ _ _~ __ _,_,----rllL~_, ~_ __ __r. ~_ _, .___ _






42 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


Figure 15. Dolomitized Suwannee Limestone exposed in the Gulf of Mexico
off the coast of Jefferson County, Florida.


encountered and according to Cole (personal communication, April,
1964), the Lepidocyclinas are Lepidocyclina (Lepidocyclina)
mantelli and Lepidocyclina (Eulepidina) undosa and this section
could be correlated in time with the Oligocene Marianna Limestone.

Thickness.-The exact thickness of the Suwannee has not been de-
termined in Jefferson County because most of the information
available is from wells that terminate in the Suwannee. However,
in the previously mentioned Southern States Oil Corporation'oil
test, 336 feet of the Suwannee Limestone was penetrated and quite
likely represents the formation's maximum thickness.

Stratigraphic Relationships.-The Suwannee Limestone lies un-
conformably upon the Crystal River Formation and unconform-
ably underlies the St. Marks or Hawthorn Formations. Where the
St. Marks and Hawthorn Formations are absent, it underlies the
younger Miccosukee Formation. Below the Cody Scarp the Suwan-






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


Figure 16. Silicified boulders of Suwannee Limestone exposed in roadcuts
in southern part of Jefferson County, Florida.



nee is covered unconformably by Pleistocene deposits and scattered
outliers of the Hawthorn Formation.
Fauna.-The echinoids Cassidulus gouldii (Bouve) and Clypeaster
rogersi (Morton) were identified from the Suwannee Limestone
in the outcrop area. The foraminifers Coskinolina floridana Cole,
Discorinopsis gunteri Cole, and Rotalia mexicana Nutall were
identified from outcrops as well as well cuttings.
Geologic Exposures.-The Suwannee Limestone is at or near the
surface in most of the southern half of Jefferson County.
The best exposure of the Suwannee Limestone in Jefferson
County is present at locality LJf-3S-4E-28-da on the south face
of an active quarry. The following section was measured at this
locality, figure 17:


43






44 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


Figure 17. Quarry of Suwannee Limestone, Jefferson County, Florida.


Bed Description Thickness
(feet)
Pleistocene Series
3 Quartz sand, very fine to medium grained --_ 2.0
Unconformity
Oligocene Series
Vicksburg Group
Suwannee Limestone

2 Partially recrystallized limestone (calcarenite)
pale orange, finely crystalline, cemented weakly
with CaCO3, moderate porosity, weathering irreg-
ular, very microfossiliferous, Coskinolina floridana,
Discorinopsis gunteri ------- -___ ______ 6.0






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


1 Partially recrystallized limestone (calcarenite),
very pale orange, finely crystalline, cemented
weakly to firmly with CaCOs, moderate porosity.
Cross sections of dissected solution pipes filled with
plastic material are present. Some of the pipes
appear to have a diameter of 2 feet _____________ 2.5
Total thickness ----______________10.5

On the north face of the quarry there are hard
ledges formed, and in the base of the quarry a hard
dark brown dolomite is exposed. Adjacent to the
north side of the quarry there are a series of caves,
sinks, and natural bridges.

The following are localities where the formation can be seen
exposed in the bed of the Wacissa River or in the banks of the
Aucilla River:

1. LJf-2S-5E-29 dc: Six-tenths of a mile north of the bridge
on State Highway 257 on the east bank of the Aucilla
River. Just above rapids formed by silicified Suwannee
about 4 feet of partially recrystallized limestone (calcare-
nite), very pale orange, finely crystalline, becoming deeply
weathered with blue-green clay and streaks of chert forming
in the rock.
2. LJf-2S-5E-22 aa: On the west bank of the Aucilla River,
2 feet of partially recrystallized limestone (calcarenite),
containing molds of microfossils.
3. LJf-2S-3E-2 bd: 10 feet below water level on Wacissa River,
is a crystalline limestone (calcarenite), containing molds of
microfossils.
4. LJf-2S-3E-13 da: Exposed in the bed of the Wacissa River
is a partially recrystallized microfossiliferous limestone
(calcarenite).
Approximately 3 miles northeast of Lamont at locality LJf-
1S-5E-12 bb, 4 feet of Suwannee Limestone is exposed in an
inactive quarry that was dug around the year 1909.
A number of exposures of Suwannee sediments are present
in the southern part of the outcrop area just north and to the
south of U. S. Highway 98. The following localities are represen-
tative:


45






46 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

1. LJf-4S-3E-16 ab: In a ditch beside a timber road.
2. LJf-4S-3E-17 bb: In a ditch beside a timber road.
3. LJf-3S-3E-27 dd: In a ditch beside a timber road.
4. LJf-4S-3E-22 ba: On the bank of the Penhook River.
5. LJf-4S-3E-15 cb: On the bank of the Penhook River.
As shown on the geologic map (Plate 1), numerous localities
of silicified Suwannee Limestone are present throughout the
county. Perhaps the most impressive evidence of silicification of
the limestone is at the Big Blue Spring on the Wacissa River,
where about 45 feet of silicified Suwannee Limestone is exposed
in a vertical section. Because of the silicification of the Suwannee
Limestone many rapids are present on the Aucilla River.
Dolomitization of the Suwannee can be observed at many
localities in the outcrop area, and many dolomite boulders, exposed
by construction, are present along U. S. Highway 98 beginning
in sec. 2, T4S, R3E, and continuing to the Aucilla River. Dolomitiz-
ation is also very prevalent along the Aucilla River and the
following localities are cited:

1. LJf-3S-4E-2 cb: Four feet exposed on east bank of Aucilla
River.
2. LJf-3S-4E-10 cc: Eight feet exposed on west bank of Aucilla
River.
3. LJf-3S-4E-28 db: Ten feet exposed in one of a series of sinks
about three-quarters of a mile from where the Aucilla River
goes underground.



Miocene Series

TAMPA STAGE

ST. MARKS FORMATION

History.-The sediments assigned to the Lower Miocene have been
sub-divided and redefined many times since the name Tampa was
first applied to those deposits by L. C. Johnson (1888, p. 235). The
latest revision was made by Puri (1953, p. 17). He places all
sediments previously called the Tampa Formation in the Tampa
Stage. He divided the Tampa Stage into the St. Marks and
Chattahoochee Formations. In the present report, the writer will
adhere to the nomenclature presented by Puri.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


Distribution.-As shown in Plate 1, the St. Marks sediments do not
occur all over Jefferson County, but are confined to two separate
areas. The largest area is irregularly shaped and occurs in over half
of the northwestern and central parts of the county. A smaller
area of St. Marks sediments occur in an oblong shaped region
in southwestern Jefferson County. Outcrops of St. Marks are
rare as the greater part of the deposits are covered by younger
sediments. The exposures of the St. Marks that were observed
occur in sinkholes, ditches and stream valleys. As shown by cross
sections A-A' and C-C' (fig. 14), the St. Marks Formation is
absent in part of the county.

General Lithology.-The St. Marks Formation is a white to very
pale orange, finely crystalline, sandy, silty, clayey, limestone (cal-
cilutite). It has poor to moderate porosity, contains molluscan
casts, and few species of foraminifers. The calcilutite has been
partially dolomitized and silicified in the outcrop area and in the
subsurface. In the outcrop area, located in the lower southwestern
part of the county, and in core holes WJf-1S-3E-13-aa and WJf-1S-
4E-29-db the St. Marks is a partially recrystallized limestone
(calcilutite). It is very pale orange, very sandy, finely crystalline,
with poor porosity. This lithology is incorporated with a pale
yellowish brown, sandy, cryptocrystalline, microfossiliferous,
partially dolomitized limestone (calcilutite), with poor to moderate
porosity. These two calcilutites are similar to the intraformational
conglomerates reported by Hendry and Yon (1958, p. 28) in the
Jim Woodruff Dam area.


Thickness.-As shown by the geologic cross sections in figure 14,
the thickness of the St. Marks is variable. Geologic cross section
A-A' indicates that the accumulation of the St. Marks sediments in
the large basin on the western side of Jefferson County approaches
a thickness of 90 feet. Section B-B' (fig. 14), in the northern part
of the county, shows the thickness is variable. However, in core
hole WJf-3N-3E-36-ca the St. Marks is 120 feet thick and this
is the greatest noted accumulation of St. Marks sediments in the
county. Section C-C' (fig. 14) shows that the St. Marks sediments
become very thin or absent on the outer edges of the Suwannee
basin in the central portion of the county. Section D-D' shows
that 20 to 35 feet of St. Marks accumulated in a Suwannee
Limestone basin, but to the east the formation is missing.






48 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

Stratigraphic Relationships.-The St. Marks unconformably
overlies the Suwannee Limestone and is overlain unconformably
by the Hawthorn Formation. In the southwestern part of the
county, St. Marks deposits are covered unconformably by the
Miccosukee Formation. It appears from the elevation of the St.
Marks sediments in the Monticello area that at one time these
sediments covered most of Jefferson County. However, during or
prior to Hawthorn deposition, the sediments were extensively
eroded and removed from a large expanse of the area.

Fauna.-The microfossils in the St. Marks Formation have not
been fully described, but Sorites sp. and Archaias floridanus are
two common species that are readily identifiable in St. Marks
deposits.
The Mollusca in the Tampa Stage sediments have been
described by Dall (1890, 1915) and Mansfield (1937).

Geologic Exposures.-As shown on the geologic map (Plate 1), the
St. Marks Formation can be seen cropping out in the ditches along
U.S. Highway 98 from the Wakulla County line eastward for 21/2
miles to Gum Creek. It is also exposed for about 2 miles in the
ditches beside a north-south road that almost parallels the Wakulla-
Jefferson County lines in secs. 19 and 30, T3S, R3E.
The thickest exposure of St. Marks beds is at locality LJf-154
located in the southeast corner of Land Lot 154, Monticello NE
quadrangle. The following section was measured on the north
side of a sinkhole:


Bed Description Thickness (feet)
Miocene Series
Choctawhatchee Stage
Miccosukee Formation

4 Badly weathered red clayey quartz sands --- 18.0

Miocene Series
Tampa Stage
St. Marks Formation

3 Yellowish gray, chalky to finely crystalline, finely
sandy, massive, fairly soft, poorly porous limestone






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


(calcilutite), weathered surface is knobby, no fos-
sils observed -- ..--------.--..... .. ... ------- 1.0
Covered ---- ....--------..--------. ....... _... 5.7

2 Pale yellowish brown, very finely crystalline, mas-
sive, finely sandy, hard to fairly soft, dolomitic
limestone (calcilutite), weathered surface is
knobby due to soft and hard nature of limestone,
no fossils observed ---------------_--.-. -----...__.___. 5.3
Covered -___ ____--- _...._---- ..... .........._. __...... __. 9.4

1 Pale yellowish brown, very finely crystalline, mas-
sive, finely sandy, hard, dense, dolomitic limestone
(calcilutite) weathered surface fairly smooth, no
fossils observed; contains inclusions of very pale
orange, cryptocrystalline, hard, sandy limestone.
This bed is exposed about 1 foot above sinkhole
floor ---... --- .____ ___ --___... --- --- ....... 1.0
Total Thickness .. ... ......------------.--.....-.... _...___-__.. .... 40.4

Many exposures of St. Marks Formation were observed on
Lloyd Creek north of the town of Lloyd. The following description
is of samples taken on the west face of Lake Drain sink (locality
LJf-1N-3E-11-dd) located on Lloyd Creek:


Sample Description Approximate
no. elevation (feet)

4 Very pale orange, very finely sandy, finely
crystalline, poor porous dolomitized lime-
stone (calcilutite) ; no fossils noted ------- 50
3 Silicified sandy limestone (calcilutite); fos-
sil ghosts still apparent .--..-----.. __--------.___ ___ 41
2 Very pale orange, finely crystalline and
chalky, finely sandy, porous dolomitized
limestone (calcilutite) ; Archaias sp. -_____ 37
1 Very pale orange, finely crystalline, finely
sandy, poorly porous dolomitized limestone
(calcilutite) ; no fossils noted ------------____ 33





50 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

Approximately 26 feet of St. Marks Formation was observed
at Horseshoe Spring, one of the several springs at the headwaters
of the Wacissa River.



ALUM BLUFF STAGE

HAWTHORN FORMATION

History.-The term Hawthorn Formation was proposed by Dall and
Harris (1892, p. 107) for deposits exposed at Hawthorne, Florida.
(For a good historical review of the term Hawthorn, the reader
is referred to Florida Geological Survey Bulletin 29). Puri (1953,
p. 38, 39) described the formation as a lithofacies of the Middle
Miocene Alum Bluff Stage. Puri and Vernon (1959, p. 120) later
cited Brooks Sink, Bradford County, as a cotype locality of the
Hawthorn Formation. Vernon (1951, p. 187) used the term
Hawthorn Formation to include all Middle Miocene marine beds
in peninsular Florida.
In the past, the Hawthorn Formation in Jefferson County
included all Miocene beds younger than the St. Marks Formation.
However, during the course of working well samples and observing
the surface outcrops, it became apparent that the sediments
contained phosphate and the "mineral" phosphorite. As these
phosphatic beds covered most of the county and seemed to correlate
with the sediments Vernon defined as Hawthorn in the peninsula,
this horizon will be separated from the overyling section of
heterogeneous non phosphatic clastics and only the lower section
containing phosphate will be considered as the Middle Miocene
Hawthorn Formation.

Distribution.-The Hawthorn Formation is present in the
subsurface over most of Jefferson County north of the Cody Scarp.
Much of the Hawthorn outcrop pattern shown on the geologic
map was not observed in the field. A contour map was drawn on
top of the Hawthorn Formation, and where the Hawthorn surface
was higher or equal to the ground surface the formation was
considered to be at or close to the ground surface. In theory the
Hawthorn should be visible in these areas which are generally
confined to stream valleys and low areas. However, in most
instances the formation is covered by slump and is not visible.
Outcrops were observed on Lloyd Creek and the Cascades near the




GEOLOGY OF JEFFERSON COUNTY, FLORIDA


town of Lloyd. Except for two outcrops observed on the Aucilla
River the formation appears to be missing in the southern part
of the county.

General Lithology.-The Hawthorn Formation consists of pale
olive, light greenish gray, yellowish gray, light gray, and moderate
yellow, sandy, waxy, phosphatic clay. The clay contains
phosphorite grains and is interbedded with very fine to medium,
some coarse, clayey quartz sands that also contain phosphorite.
In some instances, the clays and sands are cherty, and are also
associated with thin sandy calcilutite stringers.

Thickness.-The geologic section B-B' (fig. 14) indicates that in
the northern part of the county the top of the Hawthorn Formation
is irregular, and the thickness has been reduced by erosion. Section
A-A' (fig. 14) shows that the Hawthorn Formation in central and
southern Jefferson County reaches a thickness of 50 to 70 feet.
On the eastern side of Jefferson County as shown in cross section
C-C' (fig. 14) the Hawthorn appears to have been deposited in
a basin and attains a thickness of about 240 feet.
At a sinkhole called the Cascades, 51 feet of Hawthorn sedi-
ments are exposed and this is the thickest outcrop of the Hawthorn
observed in Jefferson County.

Stratigraphic Relationships.-The Hawthorn Formation lies
unconformably upon the St. Marks Formation or the Oligocene
Suwannee Limestone.
The type of contact between the Miccosukee Formation and
the Hawthorn is not known. However, available data indicates
the two units may be conformable. Where the Miccosukee For-
mation is absent, the Hawthorn deposits are overlain unconform-
ably by Pleistocene sands.

Fauna.-The fauna in the Hawthorn deposits consists of rare
sharks teeth and very rare species of the foraminifers Streblus
beccarii, Globigerina bulloides and Elphidium species. Oyster
shells were observed eroded from the bank of Lloyd Creek just
south of the bridge on State Highway 158.

Geologic Exposures.-The thickest exposure of Hawthorn deposits
is at the Cascades (locality LJf-1N13E-22-bd). The following
section was measured on the northwest wall of the sink:






52 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

Bed Description Thickness
(feet)
Miocene Series
Alum Bluff Stage
Hawthorn Formation
4 Pale olive green to moderate yellow, very fine to
fine, some medium grains, angular, very clayey to
silty, phosphoritic, quartz sand, more clayey toward
the top of bed, contains phosphorite nodules up to
2 mm. firmly cemented by clay and silt, massive
on sloped face of sinkhole _- ---- ---- 11
Covered ---_____ ---- ------- 18

3 Predominantly pale olive with light brown,
sandy (very fine to fine, some medium grains),
clay; seems to contain sand pockets, micaceous,
contains nodules of white, sandy calcilutite, mas-
sive, verticle side of sinkhole ----____ -- 4

2 Predominantly pale olive with moderate yellow,
very fine to fine, some medium grains, angular,
micaceous quartz sand; very slightly phosphoritic,
contains nodules of white sandy, limestone (calcilu-
tite). The sand is cemented firmly by clay and
contains heavies, forms verticle side of sinkhole .----- 5

1 Pale greenish yellow, moderate greenish yellow and
moderate yellow, very fine to fine, angular, micace-
ous, clayey, silty, phosphoritic quartz sand;
contains very pale olive clay blebs, cemented
firmly by clay, massive, vertical side of sinkhole ----- 5
Total thickness ---_---_ --- 43.0

Exposures of Hawthorn were observed along the Aucilla River
at the following localities:
1. LJf-1S-5E-27 bb: On east bank of Aucilla River, 4 feet of
light gray, very sandy, phosphoritic clay.
2. LJf-2S-5E-29 dc: On east bank of Aucilla River, 2 feet of
light gray, fine to medium, angular to subangular, clayey,
phosphoritic, quartz sand.





GEOLOGY OF JEFFERSON COUNTY, FLORIDA


Exposures of nonphosphoritic sediments observed along Lloyd
Creek are assigned to the Hawthorn Formation because of their
stratigraphic position and because lithologically they are similar
to the Hawthorn beds exposed at the Cascades.

CHOCTAWHATCHEE STAGE

MICCOSUKEE FORMATION

History.-The Miccosukee Formation is composed of a heterogene-
ous complex of sediments that was referred to the Lafayette
Formation (Pliocene) by Matson and Clapp (1909).
Sellards (1917, p. 96-110) referred the sediments of the
Lafayette Formation to the lower Miocene Alum Bluff Formation.
Later Gardner (1926, p. 1-2) raised the Alum Bluff Formation to
the rank of group. Mossom (1926, p. 184) placed the Alum Bluff
Formation as mapped by Sellards in the Chipola Formation of the
Alum Bluff Group (Middle Miocene).
Cooke and Mossom (1929, p. 77-125) included these sediments
in the Hawthorn Formation (Middle Miocene) and considered the
Hawthorn Formation an equivalent of the Alum Bluff Group as
mapped by Gardner.
Vernon (1951) recognized the complex of deltaic sediments as
a delta of "Hawthorn age."
Doering (1960, p. 182-189) assigned these sediments to the
Plio-Pleistocene Citronelle Formation.
Puri and Vernon (1964) reported all pro-deltaic Upper Miocene
sediments as the "Miccosukee formation." The name "Miccosukee
formation"was taken from preliminary copies of the manuscripts
of Yon's Jefferson County and Hendry's Leon County geological
reports.
Puri and Vernon (1959) pointed up the need for a detailed
survey of the surficial sediments in north Florida that would
determine the source of the deposits, the nature of their deposition,
and their geologic age.
In the independent investigations of the geology of Jefferson
County, Florida, by J. W. Yon, Jr. and of Leon County, Florida,
by C. W. Hendry, Jr., cuttings from approximately 200 water wells
and 15 core holes and outcrops were examined. The surface
deposits in the Tallahassee Hills area of Jefferson and Leon
counties represent an upper elastic unit that is deltaic in origin,
as pointed out by previous investigators, and unconformably
overlie a lower marine plastic unit. The deltaic unit caps the hills





54 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

and high level flats, whereas the marine plastics occupy the lower
inter-hill areas, though these lower areas are in part rolling
topography as well. The gross lithologies of each unit are distinctly
different; however, this difference is frequently not readily
apparent in single exposures. The upper unit can be mapped
across Jefferson and Leon counties, Florida, and in adjacent
counties. This unit is herein formally named the Miccosukee
Formation by Hendry and Yon (1967, In press).

Definition and Distribution.-In Jefferson County the Miccosukee
Formation includes all deposits in the Tallahassee Hills area that
lie above the Middle Miocene Hawthorn Formation.
The Miccosukee covers all of Jefferson County from the Cody
Scarp (Plate 1) northward to the Georgia State line. The absence
of these plastics south of the escarpment, indicates that the
Miccosukee was never deposited or was thin and subsequently
removed by Pleistocene marine erosion.
The geographic limits of Miccosukee Formation are not yet
adequately known. However, in addition to Jefferson County it is
present to the west in Leon and Gadsden counties and extends
eastward into Madison County. The Miccosukee is a heterogeneous
unit with physical features that are characteristic of deltaic
deposits, such as channel cut and fill, irregular and variable bedding
in the vertical sections, lenticular deposits of sand and clay,
crossbedded sands, interbedding of montmorillonitic and kaolinitic
clays and alluvial sands, and the presence of land vertebrates.
These above features substantiate Vernon's theory (1951) that
the deposits from Tallahassee eastward are part of a large deltaic
mass. Vernon also postulates that this deltaic mass wedges out
to the east.

General Lithology.-The Miccosukee, in outcrops and in subsur-
face samples is an assemblage of lenticular clayey sands and clay
beds which individually can be traced laterally for only short
distances. In general, the formation consists of moderately sorted
to poorly sorted, coarse to fine grained, varicolored, clayey, quartz
sand; and montmorillonitic, kaolinitic, varicolored, sandy clays.
Quite frequently the sands are crossbedded, and also contain
crossbedded thin laminae of white to light gray clay. The clay
laminae are associated with sands of two different grain sizes;
that is, very fine to medium size, figure 18, and very fine to very
coarse size, figure 19. Vernon Taylor (written communication,
1963) stated the X-ray diffraction patterns indicate that the





GEOLOGY OF JEFFERSON COUNTY, FLORIDA


laminae associated with both quartz sands is kaolinite. The sands
containing the clay laminae are the most widespread and generally
the most persistent characteristics of these deposits and always
occur at the top of the unit. In general the Miccosukee is
heterogeneous in nature and, as already mentioned, no two
outcrops exhibit the same pattern of deposition. However, this
in itself makes these deposits very distinctive. The sediments in
many places are deeply weathered laterites, and the weathered
profile is often 10 to 15 feet deep, which gives the outcrops a
massive appearance. However, bedding undoubtedly was once
present, but has been obliterated by the intense weathering.

Thickness.-As shown on the geologic cross section C-C', (fig. 14)
the Miccosukee has a thickness up to 160 feet. The cross sections
show the surface of the plastics to be very irregular and probably
represents an eroded surface. However, the cross sections indicate
that the top of some of the highest hills approach the same
elevations and probably nearly represent the original depositional
surface.

Stratigraphic Relationships.-In northeastern Jefferson County,
the Miccosukee Formation lies unconformably upon the St. Marks
Formation. The contact between the Miccosukee Formation and
the underlying Hawthorn Formation in Jefferson County may be
conformable because of a transition from marine to deltaic
sediments with no loss in the record. Regional correlations will
be necessary to determine the stratigraphic relationships of this
unit with the known upper and middle Miocene beds to the east
of Jefferson County.
In southwestern Jefferson County, Pleistocene sands overlie
the Miccosukee unconformably.

Fauna-At locality LJf-2N-6E-l-dd teeth were found that have
been described by Olsen (1963, p. 308-314) as molars from the horse
Merychippus sp. and rhinoceros Diceratherium sp. Olsen (1963)
compared the Jefferson County horse teeth with a larger series
of Tertiary horses from the western United States They agreed
most closely with Merychippus from pre-Valantine (Early
Pliocene) and post-lower Snake Creek (Upper Miocene) beds.
However, the material was too fragmentary for more than a
generic determination.
According to Olsen (1963) the single molar of the rhinoceros
Diceratherium sp. is not the same as those of the genus from the







56 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


Figure 18. Roadcut showing clay laminae associated with very fine to
medium grain size quartz sands.






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


S57
04g


Figure 19. Roadcut showing clay laminae associated with very fine to coarse
sands and also verticle joints filled with sandy clay.

Middle Miocene of western United States. He (Olsen, 1933)
concludes this is expected from an animal that occurs in a slightly
higher stratigraphic horizon.
Olsen (1963) further states:
"A new species, Merychippus gunteri was described by
Simpson (1930) from a fullers earth pit of lower Middle
Miocene age at Midway, Florida, some 50 miles to the west
of the Jefferson County locality: In the same paper, Simpson
also recorded another species, M. westoni from the Middle
Miocene of Newberry, Florida, 85 miles to the south of the
locality under discussion. The Merychippus teeth from
Jefferson County do not belong to either of these two
species."

Geologic Exposures.-The Miccosukee Formation can be observed
in roadcuts throughout the area. The sediments are so variable






58 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

that at any given outcrop you might observe individual features
or sequence of beds that are different from any other outcrop.
However, as already stated, the fact that the sediments are variable
on a local scale makes them mappable on a gross scale. The
following outcrops are cited to give some idea of the nature of the
sediments:

Locality LJf-3N-5E-31 aa: Roadcut on the east side of U. S.
Highway 19, about 3.1 miles south of the Georgia-Florida
State line. The sediments in this section illustrate the rapid
sedimentation changes and channel cut and fill of a deltaic
environment. This section is the type locality of the
Miccosukee Formation.


Unit Description Variable
thickness (feet)

C Mottled yellow brown, red brown, and
greenish gray, very fine to medium, some
coarse, angular to subangular, clayey, quartz
sand, cemented firmly with clay and iron
oxide, contains thin laminae of white clay
that apparently dip northward under unit
B, these crossbedded laminae are most
noticeable near the contact of Unit C with B,
top of Unit C becomes a deeply weathered
red color (rust).
Near the contact of Unit C and B the
sand at the base of Unit C becomes fine to
coarse and angular to subrounded, predomi-
nately coarse grained; there is no sharp
contact between Unit C and B except that
they weather differently, also near the
contact of the units the color in Unit C
becomes a mottled purple red and greenish
gray, with large gray spots up to 6 inches in
diameter. Northward along the roadcut
Unit C occurs again. However, here the color
is more a light yellow brown, with some
mottled red and greenish gray color; this
part of the unit contains crossbedded







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


laminae that apparently dip southward
under Unit B. The sand is coarse grained
in this part of the unit near the contact of
Unit C and A (clay bed), and has 2-inch
joints filled with greenish gray clay. These
joints have good relief because limonite
cemented sands border their outside edges
and hold them up. The sediments on the
extreme northern end of this roadcut are
believed to belong to Unit C, but are a deeply
weathered red color and all bedding
characteristics are destroyed -_-----
B Mottled purplish red, red brown, yellow
brown, and greenish gray, very fine to
medium, some coarse, angular to subangular,
quartz sand more clayey than Unit C, firmly
cemented by clay and iron oxide, massive; no
sharp contact with Unit C. On weathered
surface the color is much lighter than fresh
cut. Joints filled with greenish gray clay
A Yellow brown and greenish gray, slightly
sandy, silty, massive clay, that weathers
blocky, sharp contact with Unit C that lies
above __._ ....

Locality LJf-2N-7E-6 dc: On the east side of
Highway 146.


Unit


Description


th


D Weathered Zone
Fine to very coarse, angular to subrounded
quartz sand, most of clay has been leached out,
some limonite forming along contact with Unit C
C Fine to very coarse, angular to subrounded,
quartz sand, some pea-size gravel scattered
throughout unit, mottled light and dark red
brown, yellow-brown, greenish gray on east end
of unit, cemented with iron oxide and clay,
contains thin crossbedded laminae, sharp contact
with Unit B, resistant to weathering ---


Up to 13.0








Up to 14.0



Up to 5.5

Florida State


Variable
sickness (feet)


3.0-9-3






60 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

B Mottled light yellow-brown and greenish
gray, slightly sandy, waxy, blocky, massive, clay,
sharp contact with Units A and C ---- 1.5
A Light yellow-brown, fine to very coarse,
angular to subrounded, quartz sand, cemented
with iron oxide and clay, contains laminae of
white clay (0.5-2mm) that are crossbedded, sharp
contact with Unit B. Pea gravel scattered
throughout unit. At top of unit is a thin bed
that is resistant to weathering ------3.4


Locality LJf-2N-6E-1 dd: On north side of State Highway 146.
Upper Miocene vertebrate remains were found at this locality;


Unit Description Variable
thickness (feet)

F Very fine to coarse, predominantly light
yellow and red brown, very silty and clayey,
quartz sand, massive bedding, gradational contact
with Unit E, but more clayey. Roadcut slopes
back and near the top of unit the sediments
become a highly weathered yellow tan with much
of the clay leached away ___------- __ 7.5
E Very fine to medium, some coarse mottled
light brown and grayish green, angular to sub-
angular, quartz sand cemented with iron oxide
and clay, thin green laminae of clay, ?cross-
bedded, gradational contact with Unit F, but
fairly sharp contact with Unit D, weathers
irregular, forms a slight bluff _------ 2.0
D Dark yellow-brown, silty, sandy, waxy,
massive clay, fairly sharp contact with bed
below; most of unit covered but to the east it
thickens and becomes a dark gray, pale olive
color, similar to Unit B _--------- -- 1.5

C Mottled yellow-brown, and light gray-green,
fine to very coarse, angular to subrounded, quartz
sand, contains some pea-size and larger quartz







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


pebbles, clayey, contains blebs of yellow brown
clay and light gray clay granules; contact with
the underlying clay Unit B fairly sharp. Unit C
upon exposure to weathering becomes sufficiently
lithified to form a small wall along the side of the
roadcut. On the west end of the outcrop, the
unit thickens and remains resistant to weather-
ing. This unit contains vertebrate remains ------__ 2.0
B Pale olive, waxy, blocky, sandy, clay, fairly
sharp contact with Unit A, unit slopes back along
roadcut, a rubble of light gray, very fine grained
sandstone on the surface of this unit occurs,
which forms a cellular-like structure ---_______ 4.0
A Pale olive to white and yellow-brown, very
fine to medium, some coarse, angular to sub-
angular, quartz sand cemented with silica and
clay, very clayey, massive, the outer surface of
this unit is case-hardened and forms a thin
sandstone layer just on the surface that is very
resistant to weathering ___--___ ---_._.....__--------..... 3.0


QUATERNARY SYSTEM

Pleistocene and Recent Deposits

Distribution.-Surficial sediments of Jefferson County from the
Cody Scarp near Wacissa to the Gulf of Mexico form the Gulf
Coastal Lowlands and are Pleistocene in age. The Recent
sediments are confined mostly to the present stream valleys.
Northwest of Wacissa, Pleistocene deposits make up a series of
sand hills.
General Lithology.-The Pleistocene deposits forming the Gulf
Coastal Lowlands south of the Cody Scarp are very fine to medium
quartz sands with blue-green to light olive montmorillonitic clay
lenses. The clay lenses contain occasional very badly weathered
macrofossils. In the sandhill area the sediments are yellow-brown,
very fine to very course, predominantly fine to medium, angular
to subrounded, clayey, quartz sands.
The Recent deposits occurring along the stream valleys are
reworked Pleistocene quartz sands and quartz sands derived
from the Miccosukee Formation.






62 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

Thickness.-Geologic cross section A-A' (fig. 14) shows that the
Pleistocene deposits range in thickness from 2 to 3 feet at the
coastline up to 20 feet at the toe of the Cody Scarp. Cross section
D-D' (fig. 14) shows that at the Jefferson-Wakulla County line the
Pleistocene is about 7 feet thick. Eastward it thins to only a
veneer but at the eastern edge of the county the Pleistocene sands
thicken to approximately 10 feet.
In WJf-2S-3E-31-ca and WJf-1S-3E-3-ca located on the western
edge of the county, 20 and 37 feet of Pleistocene quartz sand,
respectively, overlie the St. Marks Formation.

Stratigraphic Relationships.-The Pleistocene deposits uncon-
formably overlie the St. Marks Formation and the Suwannee
Limestone in the southern part of the county. In the sandhill area
northwest of Wacissa, Pleistocene sands unconformably overlie
the Miccosukee Formation.

Fauna.-Vertebrate remains have been found in the Aucilla River
and S. J. Olsen (personal communication, January 8, 1964),
remarked that "the general clear waters of the Aucilla River have
been particularly rewarding for the skindiving bone collector.
From the eroded holes in the bottom of the river bed, along its
entire course, countless bones of late Pleistocene and sub-Recent
mammals have been collected. These remains appear to be
redeposited, and, in some cases, entombed in a reworked clay."
Some of the forms represent animals still found in the area
(deer, bear) however, the bulk of the mammals are of genera that
become extinct before the close of the Pleistocene."
"Perhaps the most important find is one of associated Bison
bison (the modern plains "Buffalo") with the remains of the
extinct long-horned bison, Bison cf. latifrons. Most mammalogists,
in past reports, do not map the distribution of the plains bison
as extending into Florida, although the Spaniards reported the
animals in the vicinity of Lake Jackson in Leon County."
"Credit for collecting representative bones of the animals listed
below goes to Mr. Richard Ohmes and his son Donald, of Chaires,
Florida. The bones were recovered by scuba diving and are in
the Ohmes' collection in Chaires."

Edentata:
Megatheriidae:
Megatherium sp. (Ground sloth).






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


Carnivora:
Ursidae:
Ursus americanus (Black bear).
Proboscidae:
Mammutidae:
Mammut americanum (American Mastodon).
Elephantidae:
Mammuthus sp. (Mammoth).
Perissodactyla:
Equidae:
Equus sp. (Pleistocene horse).
Tapiridae:
Tapirus veroensis (Florida tapir).
Artiodactyla:
Camelidae:
Cervidae:
Odocoileus virginianus (White-tailed deer).
Bovidae:
Bison bison (American "Buffalo" bison).
Bison cf. latifrons (Extinct bison).


Geologic Exposures:
1. Locality LJf-2S-3E-14 ac: About 2 feet of yellow-brown and
mottled gray, plastic, montmorillonitic, slightly sandy clay, con-
taining very badly weathered macrofossils.
2. Locality LJf-2S-3E-15 center: About 1 to 2 feet of montmoril-
lonitic macrofossiliferous clay similar to locality LJf-2S-3E-14-ac.


STRUCTURE

The configuration and altitude of the Suwannee Limestone is
shown by a contour map (fig. 10). The geologic cross-sections in
figure 14 further exemplify the altitude of the beds. The contour
map was constructed from information gathered by studying
well cuttings and gamma ray logs.
As indicated on the contour map, the top of the Suwannee
Limestone is very irregular as a result of erosion. The contour
lines are generalized and can not possibly show all the irregularities
of the limestone surface. The map shows that two positive and






64 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

several negative areas are present. The positive areas may be
related to the northwest trend of the Ocala Uplift (Vernon, 1951,
p. 48). The two negative areas on the western side of the county
could be related to the deep basin known as the Apalachicola
Embayment of the north Gulf Coast sedimentary province
(Pressler, 1947, p. 1853). The geologic cross sections (fig. 14)
indicate the basins were active after Suwannee times. The basin
developed on the east side of the county is deeper and appears
to be smaller than the one mentioned above. The western side
of the high located in the central and eastern side of Jefferson
County could be interpreted as faulting based on the linear
alignment of the contour lines. However, the writer chose not to
draw in a fault along this trend, as subsurface data is lacking.
Also the contour map may be drawn on an eroded surface and
therefore, not a true representative of the structural conditions.
The high area located north of Lamont was drawn on the basis
of one outcrop and may represent an area that was once connected
to the positive area in the central part of the county, but has been
separated by erosion.
Establishing true dip and strike of the Suwannee Limestone
would be difficult and would depend largely in what section of the
county you were working.

GEOLOGIC HISTORY

The relative age of the deposits in Jefferson County range in
age from Recent to Paleozoic. The rocks are either exposed or have
been penetrated in the subsurface by wells.
From the beginning of late Cretaceous, until early middle
Eocene, Jefferson County was in an area of plastic deposition.
At the beginning of early middle Eocene the depositional environ-
ment changed and carbonates became the predominant sediment
deposited.
During this period of time the middle Eocene, Lake City
Limestone, the Eocene Ocala Group, and the Oligocene Suwannee
Limestone was deposited. The above formations represent a
depositional change from clastics to carbonates that were deposited
in a shallow, warm open sea. At the end of the deposition of the
Lake City, the early middle Eocene seas regressed and according
to Vernon (1951, p. 92), the Avon Park Limestone was deposited
by a transgressing sea on the eroded surface of the Lake City
Limestone. The end of Avon Park deposition again marked the






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


regression of the seas and its surface emerged and was eroded.
The seas once again returned and the Ocala Group was deposited
unconformably upon the Avon Park Limestone. During the time
the upper Eocene Ocala Group was deposited the seas did not re-
gress, as there does not appear to be any break in deposition be-
tween the formations of the Ocala Group. The Eocene Epoch was
brought to a close with the deposition of the Crystal River, the
youngest formation in the Ocala Group.
The lithology and fauna of the Oligocene Suwannee Limestone
seems to indicate that it was deposited in seas that were warm,
shallow and open. At the close of the Oligocene Epoch a period
of predominantly plastic sedimentation took place. The two
positive areas shown on the contour map (fig. 10) may be related
to the Ocala Uplift, a post-Oligocene structural movement, (Vernon
1951( p. 61-62). These areas were not, however, high enough
to prevent encroachment by the early Miocene seas that deposited
the St. Marks Formation. As the cross-sections in figure 14 show,
the St. Marks Formation was deposited on top of the high areas.
The basin on the western side of Jefferson County appears to have
been formed prior to the encroachment of the early Miocene seas.
However, the thick deposits of St. Marks in the basin seems to
indicate that subsidence was still taking place up to the close of
early Miocene. As shown by the sediments forming the St. Marks
Formation, the same influence of carbon deposition was occurring
during early Miocene, even though sands and clays were being
deposited with the carbonates.
At the end of early Miocene time extensive erosion took place
in Jefferson County, especially in the eastern part, where the St.
Marks is either missing or very thin and the Hawthorn Formation
lies directly upon the Suwannee Limestone.
During Middle Miocene time, the depositional environment
changed and a great mass of clastics generally masked out all
carbonate deposition. The shallow marine or brackish water
deposits composing the Middle Miocene Hawthorn Formation
consists of sands and clays that contain phosphorite. As the
deposition of the Hawthorn deposits ceased, a predominantly
marine depositional environment gave way to a deltaic environ-
ment. The deposits forming the delta complex are widespread
as they encompass many square miles both to the east and west
of Jefferson County. The age of these deposits, at least in part,
has been established as late Miocene on the basis of land
mammals found in eastern Jefferson County. The sequence of






66 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

deposition from Middle Miocene Hawthorn Formation to the
overlying Upper Miocene Miccosukee Formation gives the appear-
ance of being only a gradual change in the mode and environment
of deposition and the contact is probably a conformable one.
With the inception of the Pleistocene Epoch, the seas once
again stood over Jefferson County at various levels and formed
the Gulf Coastal Lowlands in the southern part of the county.
The Aucilla\River and most of the creeks probably had their
beginning during the Pleistocene Epoch and the St. Marks
Formation was almost entirely removed by erosion in the Gulf
Coastal Lowlands.
Since the beginning of the Recent Epoch, sea level has been
fairly stationary and the deposition of sediments in Jefferson
County is restricted to alluvium along the many streams, peat and
muck in the lakes and Coastal Marshes.

THE MYTH OF THE WAKULLA VOLCANO

Articles by Wilfred T. Neill (1963) and Hallie Boyles (1964)
have been recently published on a volcano in the southern part
of Jefferson County. The following general information was taken
from these two articles.
Superstition, folklore and imagination produced strange tales
about a thin column of smoke and sometimes fire that rose above
the swamps near the Wacissa River, in southern Jefferson County.
According to Indian legend the column of smoke had always
been there.
Supposedly, the Spaniards were the next people after the
Indians to see the smoke.
Undoubtedly, as they and other people in later years watched
the smoke curling up out of the swamp week after week and year
after year, they begun to speculate about its origin.
As the story goes the Spaniards thought perhaps the smoke
was coming from a pirates den.
When St. Marks began to develop as a seaport, sailors used
the smoke column to get their bearings as they approached the
coast. They are said to have remarked that the old man of the
swamp was smoking his pipe again.
Prior to civil war days the local folks thought perhaps the
smoke was coming from a camp of run away slaves.
Finally someone advanced the theory that the smoke was from
a volcano. As the story of the volcano began to spread, historians,
newspapermen, writers, and just plain folks came from far and






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


wide to investigate the strange phenomena. In fact, a New York
newspaper man lost his life trying to solve the mystery.
The smoke coming from the Wacissa Swamp seemed to be
located near the small settlement of Wakulla and was named the
"Wakulla Volcano" by Barton Jones in an article published in the
Lippincott's magazine in 1882.
Maurice Thompson, in his novel "The Tallahassee Girl," wrote
about the great smoke column. He remarked that the smoke column
was no hoax and would be a permanent and persistent mystery.
On August 31, 1886, an intense earthquake rocked the city of
Charleston, South Carolina. The earthquake was intense enough
that shock waves were felt in Tallahassee. The interesting thing
about this is that on this day the smoke disappeared, never to be
seen again.
Consequently, many of the local residents attribute the
disappearance of the volcano to the Charleston earthquake.
In recent years several eye witnesses claim they have seen the
crater. According to their reports, huge black boulders charred
by fire surround the crater.
However, evidence gathered by the Division of Geology
indicates that the surface rocks in Jefferson County are far
different from those that come from volcanoes. Volcanic rocks
are present in the county, but lie below 7000 feet of sands, clays
and limestones. These volcanic rocks form what geologists call
volcanic diabase sills or dikes and are believed to be millions of
years old. Since the time the sills or dikes were formed the rocks
show no evidence of volcanic activity in the area.
The reported smoke coming from the Wacissa Swamp presents
a problem, although not an uncommon one. In an article in Florida
Wildlife about the volcano Wilfred Neill presents the theory that
the smoke was a result of peat fires that varied in intensity. He
further states that the earthquake of 1886 caused sinkhole
development in the area and subsequently the burning peat slumped
into these collapse features and was extinguished. Whether or
not Mr. Neill is correct in his assumptions, his explanation is a
reasonable one.
The large boulders supposedly of volcanic origin are nothing
more than silicified limestone residue of the Suwannee Limestone.
They represent the remains of a highly eroded limestone surface
where the original composition of the rock has been replaced
chemically by quartz. These boulders in no way are related to
volcanic activity.








68 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


The volcano story makes for interesting popular reading, but
cannot be substantiated by any fact, and therefore, is nothing
more than a legend or a myth.


ECONOMIC GEOLOGY


LIMESTONE


The term limestone applies to a sedimentary rock composed
essentially of calcium carbonate (CaCOj). It may have varying
amounts of impurities such as clay, silica, iron oxide, carbonaceous
material and magnesium carbonate.
The quantity of limestone in Jefferson County is sufficient to
sustain large quarry operations. The Suwannee Limestone is the
most important source of limestone because of its accessibility,
softness, and as shown in table 5, it is essentially a pure "high
calcium" rock in that it contains more than 95 percent calcium
carbonate. The distribution of the Suwannee Limestone is shown



TABLE 5. Chemical analyses of Suwannee Limestone samples from
Jefferson County, Florida


F.G.S.
sample No.

LJf-2S-3E-1 ac
LJf-1S-5E-12 bb
LJf-1S-5E-12 bb
LJf-3S-4E-28 ca
LJf-3S-4E-28 db
LJf-4S-3E-16 cb
LJf-3S-3E-27 dd


O


















101.2
U



0a





0

99.2
99.5






101.2
100.0
99.2


0
o










Trace




Trace


Trace
Ia

so
a




Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace


0

o






0.09
.07
Trace
.12
.13
.11
.16


Trace
Trace
trace
Trace
Trace
Trace
Trace


a








0.55
.38
.31
.44
.22
.88
.24


Total
percent1

98.89
99.55
99.01
100.06
101.55
100.99
99.60


1The percentage total is the sum of all the percentages of the individual chemical components
and do not always add up to 100 percent. To convert the sum of all the components to 100
percent use the following formula:
Chemical component x 100
percent total







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


on figure 20. In 1964, the only active mining of limestone was
by the Jefferson County Road Department and Buckeye Cellulose
Company for use as road metal in the southern part of the county.
In adjacent Taylor County, limestone has been quarried for
use as a road base. In both cases, the method of mining has been
with draglines and front end loaders on tractors.
The abundance of Suwannee Limestone could make it a very
valuable commodity for use in road building as a base course
material and stabilized base rock. A number of samples were
submitted to the State Road Department to see if they would
meet their specifications for use as stabilized base rock and base
course material and, as noted on table 6, all categories were
satisfactory.
The high calcium content of the Suwannee Limestone would
make it very suitable for use in any chemical process such as
agricultural limestone and the manufacture of cement, and quick
and hydrated lime.
Reves (1961) presented a discussion of the various uses and
technical data pertaining to uses of limestone.
Some of the main factors involving the future exploitation
of the limestone resources in Jefferson County are transportation
and fuel. At present no railroads traverse the area where the
greatest reserves of limestone occur. However, two major railroads
run through the county and spur lines could be extended into this
region. Two principal highways, U. S. Highway 90 and U. S.
Highway 27, and several Florida secondary highways run
sufficiently near the limestone deposits to be useful for transporting
the commodity to local consumers or to rail lines for shipping.
Upon the completion of Interstate Highway 10, figure 21, across
Jefferson County another important transportation route will
become available.
Upon the construction and completion of the intercoastal
waterway (fig. 21) off the coast of Jefferson County, another
means of transportation would become available and open the way
to markets all over the State.
A natural gas pipeline traverses the county (fig. 21) and could
be an important source of fuel in potential chemical processing
of limestone.

DOLOMITE ROCK

Secondary dolomite generally is considered a variety of
limestone that theoretically contains 54.6 percent calcium








70 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


G E 0


1 0 1 2 3 45 MILES
SCALE


L-- c lie e B1
of A r IE.1-1c


STATE BOARD of CONSERVATION


EXPLANATION

LIMESTONE
high calcium, soft, friable

DOLOMITE

Primary Area of
SClayey Quartz Sand

_ Secondary Areas of
Clayey Quartz Sands


prepared by DIVISION of GEOLOGY


Figure 20. Distribution of the economic deposits of Jefferson County, Florida.


G








GEOLOGY OF JEFFERSON COUNTY, FLORIDA 71


TABLE 6. Soil test results of samples of Suwannee Limestone from
Jefferson County, Florida

Florida State Road
Department
specifications2
Sample Liquid Plastic Organic Base course
no. limit1 index' matter materials

LJf-1S-5E-12 bb NP NP 0.3 Passes
LJf-4S-3E-16 da NP NP .1 Passes
LJf-3S-3E-34 bb NP NP .1 Passes
LJf-3S-4E-28 ca NP NP .1 Passes
LJf-3S-4E-28 da NP NP .1 Passes
LJf-3S-4E-10 dc NP NP .2 Passes

'For a technical discussion of these categories see Florida Geological Survey Bulletin 42, p.
99-102.
2See Florida State Road Department Standard Specifications 1959, p. 423.
NP-Nonplastic


carbonate (CaCO3) and 45.4 percent magnesium carbonate
(MgCO3). This is not to say that all dolomites will approach the
theoretical proportions mentioned above for there is generally
gradations from dolomitic limestones, (4.4 to 22.7% MaCOs)
calcitic dolomites, (22.7 to 41.0% MaCO,) to true dolomites (41.0
to 45.4% MaCOS). Dolomites can, in a general way, be
distinguished from limestones by their slower effervescence in






A L A B A M A











Interstate Highwy(Completed) -
S. Inter.tateHighwayUnderconstruction or Proposed)
Cro Flo e Marida n a













..... Opn Bay Water Route(Propod)
Figure 21. Route of Florida interstate highway system, waterways, and





natural gas pipeline (after Reves)
4/ ~






72 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

cold, dilute, hydrochloric acid. This test does not, however, tell
you the amount of magnesium carbonate present.
The dolomites of commercial value in Jefferson County are
Suwannee Limestones that have been replaced in part by MgCO3.
The approximate areal distribution of the dolomites is shown on
the mineral resources map (fig. 20). Field observation seems to
indicate that the dolomites are confined for the most part along
the Aucilla River and the low area east of the Aucilla River and
south of U. S. Highway 98. The thickness of the dolomites in
this area is not known; however, core test WJf-4S-3E-24-bd
bottomed in dolomite at 24 feet. Along the Aucilla River in Taylor
County, dolomite prospecting was conducted by the Florida
Geological Survey in 1942. For results of these test holes, the
location of the wells and the dolomitic areas, the reader is referred
to the Florida Geological Survey Report of Investigations No. 3,
p. 13-25. Observation of table 7 shows that the dolomites tested
are almost pure as they contain 41 toA2 percent magnesium
carbonate. One of the samples, LJf-3S-4E-10-dc was subjected
to the Los Angeles abrasion test and failed as its abrasion loss
was 46 percent and exceeded the 40 percent minimum set by the
Florida State Road Department Standard Specifications.

CLAY DEPOSITS

INTRODUCTION

At the present time there is no clay being mined commercially
in Jefferson County. The clays are montmorillonites and kaolinites
which occur in the Hawthorn, Miccosukee, and the Pleistocene
deposits. Some of the clays in the Miccosukee Formation have
a very small percentage of sand and may be of commercial value.
However, because of their lenticular nature and generally short
lateral extent, an extensive drilling program would be necessary
to determine if it would be feasible to mine them for commerical
use. In the southern part of the county the terrace deposits contain
sandy montmorillonitic clays and detailed exploration may find
deposits suitable for commercial use.

TESTS

Samples of clays from outcrops were collected and submitted
to the Bureau of Mines for determination of the physical and firing
characteristics and recommended uses. Table 8 gives the data on











TABLE 7. Chemical analyses of Suwannee Dolomite samples from
Jefferson County, Florida


F.G.S.
WJf-4S-3E-24 bd
(depth in feet)


8'9" to
14' to
16' to
20' to


F.G.S.
sample no.






LJf-3S-4E-28
LJf-3S-4E-28
LJf-3S-4E-10
LJf-3S-4E- 2
LJf-3S-4E- 2


55.7
55.7
55.3
54.9
db 57.9
ac 56.6
de 56.2
bd 56.6
cb 57.0


1The percentage total is the Sum of all the percentages of the individual chemical components and do not always add up to 100
the sum of all the components to 100 percent use the following formula:
Chemical component x 100

percent total


percent. To convert


Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace
Trace






74 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

these clays. Also included in the table is an analysis of clay
collected from a 111/2 foot test hole, located one and one-half miles
east of Wacissa near milepost 822 on the abandoned Seaboard
Air Line Railway. The data on the clay from the test hole was
taken from the Florida Geological Survey Information Circular
No. 2, (1949, p. 35, 54).
The location and description of the samples collected and tested
as shown in table 8 are as follows:


Sample No.
LJf-2N-5E- 8 ad


LJf-152


LJf-3N-5E-31 ca


LJf-2N-6E-1 dd


LJf-1S-4E-33 ac


LJf-1S-5E-19 bb


Roadcut on Florida Highway 149A. 5 feet of
mottled yellow brown and light greenish gray
sandy clay.
Roadcut on Florida Highway 149, 2 feet of
mottled yellow brown and light greenish gray
sandy clay.
Roadcut on U. S. Highway 19, 5 feet of mottled
yellow brown and light greenish gray sandy
clay.
Roadcut on Florida- Highway 146. 5 feet of
mottled yellow brown and gray green sandy
clay.
Ditch on county road west of Thomas City.
2 feet of mottled yellow brown and light
greenish gray sandy clay.
Roadcut on U. S. Highway 27, approximately
15 feet of mottled dark yellowish brown and
dusky red sandy, silty clay.

SAND


The most extensive areas of sand occur in the Gulf Coastal
Lowlands, along the eastern side of the county, the Dune Belt and
in the sandhill area northwest of Wacissa (fig. 20). In the Gulf
Coastal Lowlands area the sand deposits are generally thin,
slightly clayey, fine to medium grained quartz. The deposits in
the Dune Belt sandhill area are very fine to very coarse grained,
predominantly fine to medium grained, clayey, iron-stained quartz
sand. Coarse sands were encountered in core holes WJf-1S-3E-
13-aa from 35 to 60' and in WJf-1N-6E-8-dd located in the eastern
part of the county, from 16 to 43 feet. The sands in the core
holes, and in the Dune Belt, would require some washing to remove
the clay content.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


PETROLEUM POSSIBILITY

Two oil test wells, the Southern States Oil Corporation No. 1
Millard and Gossard and the Coastal Petroleum Company No. 1
E. P. Larsh, have been drilled in Jefferson County. The two tests
penetrated the Atkinson Formation of Upper Cretaceous age,
which is the same age and is similar lithologically to the oil pro-
ducing zones in the Pollard Field just north of the Florida-Alabama
State line in Escambia County, Alabama. Neither of the tests had
oil shows and were abandoned as dry holes. Although the absence
of oil in these wells has been discouraging, the sands in the lower
member of the Atkinson Formation appear to be adequate as a
reservoir rock and if oil is present in the county these beds are
the best prospect.

PHOSPHATE

Phosphate is common in the Hawthorn Formation in Jefferson
County. The phosphate occurs in two forms, as phosphorite and
as colloidal phosphate embedded in a clay matrix.
A thick section of colloidal phosphate-clay was found in a core
hole located in the center of Sec. 5, T2N, R5E and is the richest
phosphate deposit encountered in the county. Nodular beds of
phosphate and phosphate pebbles up to 2 inches in diameter also
occur within the unit.
The phosphatic unit was analyzed for PsO, and the results of
the analyses are listed below:

Core Hole WJf-2N-5E-5 center
Core Sample (Depth in feet) % P2,O
Dry Basis

70-721/2 2.3
7212-75 0.2
75-771/2 6.2
771/2-80 2.3
80-821/ 1.3
821/2-85 17.1
85-871/2 7.6
871/2-90 19.0
90-921/2 13.5
92/2-95 10.7
95-9712 8.5













TABLE 8. Tests of selected clay samples from Jefferson County, Florida.


Sample Designation



Raw Properties:
Working
characteristics





Water of
plasticity %
Drying
shrinkage %
Dry strength
Drying
characteristics


Slow Firing Test:
% Linear
Shrinkage
1800* F
1900* F
2000* F
21000 F
22000 F
23000 F
2400* F


% Absorption:
1800* F
1900 F
2000* F
21000 F
22000 F
2300" F
2400" F


LJf-2N-5E-8 ad I LJf- 152


Fairly long work-
ing, plastic, fine
grit




39.0

10.0
Good


Fair, slight scum, Fair,
slightly rough ing,
surface


Long working,
smooth, plastic


46.0

16.0
Fair

slight warp-
scumming



19.5
20.0
22.0
25.0
26.0
26.0



16.7
15.2
9.7
4.1
3.(
2.1


LJf-3N-5E-31 ca




Long working,
smooth, plastic





38.0

10.5
Good

Poor, wavey
rough surface



14
V5
14.5
19.5
19.5
19.5



16.7
25.0
20.4
11.4
10.8
7.8


LJf-2N-6E-1 dd




Long working,
smooth, plastic
sticky




59.0

4.5
Fair

Poor, grainy




5.0
5.0
5.0
10.0
10.0
10.0



20.8
20.8
18.5
18.2
14.3
14.1


LJf-1S-4E-33 ac




Short working,
sticky, plastic





25.0

10.0
Fair, slight
scum, rough
surface




5.5
5.5
5.5
5.5
4.0
4.0



16.4
18.9
20.4
20.4
20.0
13.3


LJf-1S-5E-19 bb




Long working,
smooth, plastic





26.0

5.5
Fair, warping






5.0
5.0
5.0
6.0
9.0
9.0



18.5
19.6
17.6
17.0
13.9)
12.9


Sample
Designation


Physical
Properties:
Plasticity
Water of
plasticity %
Linear air
shrinkage %
Modulus of
rupture
Slaking test
Color





Firing Behavior:
% Linear
Shrinkage
9500 C
10500 C
1090 C
11500 C
1190 C
1253o C


Absorption
weight
9500
10500
10900
11500
1190"
1250"


% by

C
C
C
C
C
C


t

0-263(I.C. #2)



0
Good
31.0

8.6

210. C
Fast
Brown
rr







1.0
2.5
2.0
2.5
2.5
2.5








Color:
18000 F
19000 F
20000 F
21000 F
22000 F
23000 F
24000 F

Hardness:
18000 F
19000 F
2000 F
21000 F
22000 F
23000 F

Bloating Test:


Potential Use:


Light Brown
Light Brown
Light Brown
Brown
Brown
Brown


Fair Hard
Fair Hard
Hard
Very Hard
Steel Hard
Steel Hard

Negative


Light Brown
Light Brown
Light Brown
Brown
Brown
Brown


Fair Hard
Hard
Very Hard
Steel Hard
Steel Hard
Steel Hard

Negative


Light Brown
Light Brown
Light Brown
Brown
Chocolate
Buff Brown


Fair Hard
Fair Hard
Hard
Very Hard
Very Hard
Steel Hard

Negative


Flesh
Flesh
Flesh
Tan
Buff
Buff


Fair Hard
Fair Hard
Fair Hard
Hard
Very Hard
Very Hard

Negative


Light Brown
Light Brown
.rown
Chocolate
Chocolate
Chocolate


Fair Hard
Fair Hard
Hard
Hard
Very Hard
Very Hard

Negative


Could be used
in making brick


Tan
Tan
Tan
Tan
Buff Tan
Olive Tan


Fair Hard
Fair Hard
Hard
Hard
Very Hard
Steel Hard

Negative


Light color,
some cracking,
shrinkage a
little high,
addition of
alkali might
make a pottery
or derative tile


Color:
950* C
10500 C
10900 C
11500 C
11900 C
12500 C


Porosity %:
9500 C
10500 C
10900 C
11500 C
1190 C
12500 C

Potential Use:


Reddish Orange
Reddish Orange
Brick Red
Brick Red
Brick Red
Brick Red


34.8
35.0
34.0
34.0
32.5
33.3

Rather porous,
common brick


I







78 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

971/2-100 8.9
100-1021/2 9.2
1021/2-105 13.7
105-1071/ 11.9
10712-110 12.8
110-1121/2 6.9
1121/2-115 6.9
115-1171/2 3.9
11712-120 11.2
120-122/2 7.6
1221/2-125 6.9
125-1271/2 11.2
1271/2-130 8.3
As shown by the analysis, the phosphate content of the core
hole interval is low. However, in future years a lower grade
phosphate may be economically acceptable and could be utilized
as suggested by Vernon (1951, p. 228-30). He (Vernon, 1951,
p. 228-30) indicates that this type phosphate is used as a soil
conditioner and filler in fertilizer.
The Hawthorn Formation in Jefferson County also contains
sand size phosphate particles that are associated with clayey
sands or sandy montmorillonitic clays. These particles are
referred to in this report as phosphorite. The visual estimate of
the phosphorite grains in cuttings from wells, core hole samples
and outcrops indicates the phosphorite does not exceed 10 percent
of the bulk volume of the sediments. Vernon (1951, p. 224) reports
that phosphorite from other areas in Florida is composed of the
mineral fluorapatite.
Knowledge of the occurrence of phosphate in Jefferson County
is limited to the available data and trends cannot be predicted
at this time. However, in the future as more is known of the
genesis and occurrence of phosphate, these data may indicate that
further investigation is warranted.

GROUND WATER

The term "ground water" refers to the water that fills all
the open pores and interstices in the rocks below the surface of
the earth in the zone of saturation.
The source of ground water in Jefferson County is the
precipitation in the county and nearby areas. Some of the
precipitation that falls on Jefferson County leaves the area by







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


surface runoff in streams, by evaporation and by transpiration.
The part that is left soaks into the ground and slowly moves
downward to the zone of saturation. After reaching the zone of
saturation, the water under the influence of gravity begins to move
slowly toward points of discharge such as wells, springs, streams,
or the Gulf of Mexico.
Ground water in Jefferson County can be divided into two
categories: (1) Unconfined water (water table) which occurs in
the shallow formations above the St. Marks Formation and is
under atmospheric conditions; that is, the water surface is free
to rise and fall. The unconfined water will not be discussed in
this report. (2) Water that is confined under pressure between
relatively impermeable formations, and is not free to rise and
fall. This water is said to be under artesian conditions.

ARTESIAN WATER

The artesian water in Jefferson County occurs in the Floridan
aquifer from which most of the water for irrigation, industry,
and public supply is derived.

FLORIDAN AQUIFER

The term Floridan aquifer was introduced by Parker and
others (1955, p. 188) and it includes all or parts of formations
from Middle Eocene to Middle Miocene.
In Jefferson County it is believed that the Floridan aquifer is
recharged by Lake Miccosukee through sinkholes, along the Aucilla
River, and in the northeastern portion of the county in the swamp
areas where leakage occurs through the overlying sediments of
the Hawthorn Formation and Miccosukee Formation.

FLUCTUATIONS OF WATER LEVELS

Twenty-one wells were measured periodically from January,
1960, to December, 1962, to determine trends in water-level
fluctuations. Water-level recorders were installed on two wells in
April, 1960, and were in operation until December, 1962. The
graphs obtained from the water-level recorders showed a daily
as well as seasonal fluctuation.
To determine the relationship of rainfall to water levels, a
cumulative departure curve of average precipitation at Monticello
from 1948 to December, 1962, was plotted, figure 22. Except for















CUMULATIVE DEPARTURE FROM THE AVERAGE PRECIPITATION
20 BASED ON ANNUAL AVERAGE OF 54.82 INCHES

1\0



20
i i


t ,



-20-







0 i I
1948 1949 1950 1951 1952 1953 1954 1955 1956 1957 1958 1959 1960 1961 1962---------





: I I__-

1948 1949 1950 1951 1952 1953 1954 1955 1956 1957 1958 1959 1960 1961 1962 L J

Figure 22. Cumulative departure curve of average precipitation at Monti-
cello, Jefferson County from 1948 to December, 1962.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


1952, the rainfall was below average between 1948 and 1956. In
1957 the rainfall was sufficient to start an upward trend which
peaked in December, 1960, 12 inches above normal. From
December, 1960, through December, 1962, the cumulative
departure curve shows a gradual decline.
The hydrograph of wells WJf-3N-4E-22-cb, WJf-3N-7E-27-bb,
WJf-1S-3E-15-dc, and WJf-1S-4E-28-ac and the average monthly
precipitation graph for the years 1960 through 1962 are shown
on figure 23. As shown in the figure, the hydrographs indicate
that during the months of high precipitation, the water levels
rise and during the months of low precipitation, the water levels
fall. The peaks on the hydrograph of well WJf-1S-4E-28-ac
indicate rapid response of the water level to heavy rainfall near
the well. The overall trend of the water levels from July, 1961,
to December, 1962, has been downward.
In well WJf-3N-4E-22-cb, the water levels declined 8.88 feet
from May, 1960, to December, 1962, and the water level in well
WJf-1S-3E-15-cd declined 3.92 feet during the same period.
The principal cause of fluctuations of water levels in Jefferson
County is believed to be rainfall, as very little water is withdrawn
from the aquifer.

PIEZOMETRIC SURFACE

The height to which water will rise in tightly cased wells that
penetrate an artesian aquifer creates an imaginary surface called
the piezometric surface. It should be pointed out, however, that
in parts of Jefferson County, the piezometric surface lies below
the top of the bedrock forming the Floridan aquifer. This condition
indicates that in these areas the ground water is actually under
water table conditions rather than artesian.
Two maps, figures 24 and 25, were prepared to show the
configuration of the piezometric surface in May, 1960, and in
December, 1962. The primary reason for showing the piezometric
surface at these two different time intervals was to point out how
the artesian pressures had dropped during this period. From
May, 1960, to December, 1962, the amount of decline was about
9 feet in the northern half of the county and 3 feet over most
of the southern half of the county. This lowering is probably the
result of the decline in rainfall after 1960.
The piezometric surface ranges from sea level along the coast
to 80 feet above sea level in northeastern Jefferson County. The









82 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


WJf S-3E-15 d


oo4 4 ^ --, .... ... ....... ^----'
5 62 - . . .... .
z 61



57
,,.


40
W 40|-i---- -----------------------------------
39


I 38 . ; - ; .- .. .
37
341


Figure 23. Graph showing hydrographs of selected wells WJf-3N-4E-22 cb,
WJf-3N-7E-27 bb, WJf-1S-3E-15 dc, WJf-1S-4E-28 ac and total monthly
precipitation in Jefferson County, Florida.


ground water moves in a direction perpendicular to the contours

and as is shown in figures 24 and 25 this is generally to the

southwest. The shape of the contours in the area just below

Lake Miccosukee and southward indicates a recharge area with

the flow of water to the southeast. The springs located just below

the town of Wacissa, both at the headwaters of the Wacissa River

and along the upper part of the river itself doesn't seem to have

a great deal of effect on the piezometric surface. Along the lower

southeast side of Jefferson County the piezometric map shows an

area of recharge and along the lower reaches of the Aucilla River

north of Nutall Rise water can be seen entering the aquifer

through sinkholes. The Auci la River goes underground here but


I
.----~--------c--- -, -~----1----
i
i----------;----
i
---ii --1 -------(
--1-


i











GEOLOGY OF JEFFERSON COUNTY, FLORIDA


R4 E


R5 E


R6 E


G E O R G 731


,3achee Bay
AI PJ
OO ME)UCO
G"L


R3 E


R4E


10 1 4 MILES
APPROX. SCALE







EXPLANATION
037
WELL NUMBER IS ALTITUDE OF THE PIEZOMETRIC
SURFACE IN MAY 1960.

CONTOUR SHOWING THE ALTITUDE OF THE
PIEZOMETRIC SURFACE IN FEET.
CONTOUR INTERVAL IS 10 FEET
DATUM IS SEA LEVEL.


R5 E


R6 E


R7E


Figure 24. Jefferson County, Florida, showing the piezometric surface of
the Floridan aquifer in May, 1960.


R3 E


83


R7E


A

z












z


D









84 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT


R3 E


G


R4 E


R5 E


R6 E


R7E


E 0 R G I A
.64


z









Lake
CN
Miccosukee







z z OY
0: 45


tic




-I -

of MEXICO


R3 E


*24


0
-
v-


R4 E


AUCILLA o










\MON
47 O
\ o








1 1 2 3 4 MILES
APPROX. SCALE








EXPLANATION
036
WELL NUMBER IS ALTITUDE OF THE PIEZOMETRIC
SURFACE IN DECEMBER 1962.

CONTOUR SHOWING THE ALTITUDE OF THE
PIEZOMETRIC SURFACE IN FEET.
CONTOUR INTERVAL IS 10 FEET.

DATUM IS SEA LEVEL.


R5 E


R6 E


R7E


Figure 25. Jefferson County, Florida, showing the piezometric surface of
the Floridan aquifer in December, 1962.







GEOLOGY OF JEFFERSON COUNTY, FLORIDA


comes up again near Nutall Rise. Another area of recharge is
believed to exist in the northeast part of the county by leakage
through the plastics overlying the Suwannee Limestone.
In well WJf-1N-4E-26-bb the water level is approximately
115 feet higher than the water level in a Floridan aquifer well
located two miles to the north. It is on this basis the writer
believes that water from WJf-1N-4E-26-bb is coming from a
secondary aquifer or that it is a water table well.
The recharge to this aquifer is probably from the overlying
Hawthorn Formation and Miccosukee Formation.
By comparing the hydrograph and the average monthly
precipitation graph for the years 1960 through 1962, figure 26,
the water level seems to respond to rainfall; that is, the water
levels rise during wet periods and fall during dry periods.
WJf-1N-4E-26-bb also shows a downward trend of the water
levels after 1960. The low water level in September, 1960, was a
result of extensive pumping of the well, and at the time the
measurement was made the water level in the well had not
recovered from the pumping.
A complete water analysis was run on a water sample from
well WJf-1N-4E-26-bb and is shown in table 9.

QUALITY OF WATER

The rain falling upon the earth's surface is relatively free of
dissolved minerals except for small quantities of atmospheric
gases and dust. However, that part of rainfall that is absorbed
into the soil and percolates downward through the earth's crust
dissolves a part of the rock with which it comes into contact.
Consequently, the chemical character of the water is to a large
degree dependent upon the composition solubility of the material
through which it has passed.
Chemical analyses of water from wells in Jefferson County
and from well WTy-4S-3E-24-bd in Taylor County were made
by the Quality of Water Branch of the U. S. Geological Survey
(table 9). All of the samples were from the Floridan aquifer,
except one water sample from a secondary aquifer or water table
in Jefferson County. The chemical composition of the seven
samples is shown in figure 27 by bar graphs. The mineral
constituents analyzed are discussed below. The mineral constituents
as shown in table 9 are expressed in parts per million (ppm) by
weight. One part per million (ppm) is equivalent to approximately














0
o


0


0
0




0











H
z



0
H

0

H
tr

M-
Co
d
o
H



bd
fC1

i-
H
r-
1-
M


^J
0C
?0
X


Figure 26. Hydrograph of well WJf-1N-4E-26 bb and a total monthly
precipitation graph of rainfall in Jefferson County, Florida.









GEOLOGY OF JEFFERSON COUNTY, FLORIDA


G


E O





WJf 3N-4E-34 da


Lake
- Miccosukee


LLOYD -i



WJf 1N-4E-

CAPPS



WACISSA WJf IS-4E-30 da


G


-l. WJI 2N-5E-19aa
"MONTICELLO



AUCILL,


26 bb


I A




WJf 3N-6E-23 cc






A -



0 b
A

)~ o


O
/ 1
^**'~,
f~


LAMONTJ f
o"


.936 E PM

2 5 50 EPM

WJf 2S-3E-31 bb // 0i
5 50 E PM


z
o 0

GU E I F





Jefferson Count24bd
a a- 'h ir" .e/"--


GLJ OF/

STATE BOARD of CONSERVATION
Figure 27. Bar graphs showing chemical
Jefferson County,


-3




-








C 0


EXPLANATION
MAGNESIUM--------------
SODIUM --
POTASSIUM -:--
CHLORIDE
NITRATE -----------
SULPHATE |
BICARBONATE-----------L-
CALCIUM----------------
WELL SYMBOL and
WELL NUMBER--e WJfIS-4E-30da


prepared by DIVISION of GEOLOGY

composition of artesian water in
Florida.


87


ZI


2


i


Z.


I






88 FLORIDA GEOLOGICAL SURVEY-BULLETIN FORTY-EIGHT

1 pound of dissolved mineral constituents in 120,000 gallons of
water.

DISSOLVED SOLIDS

The concentration of dissolved solids in water is approximately
equal to the amount of mineral matter left after a quantity of
water is evaporated. The U. S. Public Health Service recommends
that for drinking water the maximum amount of dissolved solids
should not exceed 500 ppm. However, water containing 1,000 ppm
is permissible if water of better quality is not available. The
dissolved solid concentrations in the water samples from Jefferson
County ranged from 112 to 206 ppm. Well WTy-4S-3E-24-bd,
located in Taylor County, had a dissolved solid content of 1,790
ppm.

HARDNESS

In waters that are considered hard, soap does not lather easily
and a curd is left on the surface of the water. The cations, calcium
and magnesium generally are the cause of hardness of water.
The calcium and magnesium hardness of the water samples
analyzed from Jefferson County ranges from 100 to 206 ppm. The
water sample from the well in Taylor County had a calcium and
magnesium hardness of 670.

TEMPERATURE

The temperature of the water from all of the wells ranged
from 68' to 710 F.

SPECIFIC CONDUCTANCE

The specific conductance of water is a measure of its ability
to conduct an electrical current. The higher the mineralization the
better the water conducts an electrical current.
The relationship between the measured total dissolved solids,
hardness and specific conductance of water from six wells located
in Jefferson County is shown by the straight line plots in figure
28. Specific conductance of 18 water samples from wells in
Jefferson County, one from Madison County, and two from Taylor
County, are shown in table 9. An approximate value for the
hardness and total dissolved solids was calculated from the specific






GEOLOGY OF JEFFERSON COUNTY, FLORIDA


Figure 28. Hardness and total dissolved solids curve of artesian water in
Jefferson County, Florida.

conductance of these 18 water samples by using the straight line
plots in figure 28.

HYDROGEN-ION CONCENTRATION (pH)

The concentration of hydrogen-ions in water is expressed as
pH. A water having a pH of 7.0 is said to be neutral. A higher
pH value indicates alkaline water and a lower value is said to be
acidic and may be corrosive. All the water samples tested had a
pH value greater than 7.0 and ranged from 7.9 to 8.4.

SILICA (SiO,)

Silica is dissolved from rocks and is present in almost all
ground water samples. Silica is of little importance in water use
except it can contribute to the formation of scale in steam boilers.
Silica in the 6 samples from the Floridan aquifer range from
7.2 to 17 ppm. In the water sample from the secondary artesian
aquifer the silica content was 39.0 ppm.

IRON (Fe)

Iron is one of the most objectionable constituents occurring
in ground water. The quantity may vary geographically as well
as vertically within the same formation. Iron in excessive
quantities will stain laundry, plumbing fixtures and cause water




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REPORT xsi:schemaLocation 'http:www.fcla.edudlsmddaitss http:www.fcla.edudlsmddaitssdaitss2Report.xsd' xmlns:xsi 'http:www.w3.org2001XMLSchema-instance' xmlns 'http:www.fcla.edudlsmddaitss'
DISSEMINATION IEID 'E20100110_AAACDP' PACKAGE 'UF00000234_00001' INGEST_TIME '2010-01-10T17:09:26-05:00'
AGREEMENT_INFO ACCOUNT 'UF' PROJECT 'UFDC'
REQUEST_EVENTS TITLE Disseminate Event
REQUEST_EVENT NAME 'disseminate request placed' TIME '2015-10-09T15:36:56-04:00' NOTE 'request id: 303201; 1' AGENT 'UF64'
finished' '2015-10-09T15:58:38-04:00' '' 'SYSTEM'
FILES
FILE SIZE '519037' DFID 'info:fdaE20100110_AAACDPfileF20100110_AABOPY' ORIGIN 'DEPOSITOR' PATH 'sip-files00001.jp2'
MESSAGE_DIGEST ALGORITHM 'MD5' a49f9328356228837183d04694038238
'SHA-1' a8d2112134062b7f495f21cfccb60b6750a40d0c
EVENT '2012-05-16T12:23:45-04:00' OUTCOME 'success'
PROCEDURE describe
'423983' 'info:fdaE20100110_AAACDPfileF20100110_AABOPZ' 'sip-files00001.jpg'
b2d31362e2ef4d7927bf3c3af3263305
2ba79ca8d6b2954081fbe8af06838b56930b4b10
'2012-05-16T12:25:05-04:00'
describe
'44659' 'info:fdaE20100110_AAACDPfileF20100110_AABOQA' 'sip-files00001.pro'
e73d458c8a708e6f97d0ce8a5e9456a7
6e22f79357c7342647b6f90117f56798b51a66f3
'2012-05-16T12:27:14-04:00'
describe
'133929' 'info:fdaE20100110_AAACDPfileF20100110_AABOQB' 'sip-files00001.QC.jpg'
d6fbb9e3b2645ce42b42dc658d30982e
f63c37c47e68f64adc9ea9c9e69da4fba4a28648
'2012-05-16T12:18:44-04:00'
describe
'4155276' 'info:fdaE20100110_AAACDPfileF20100110_AABOQC' 'sip-files00001.tif'
b50321c918298dd7d5b31e98ebeaf53c
9645dbc95a02bfa2507ff54a3efcb3fc00debf7a
'2012-05-16T12:25:58-04:00'
describe
'1910' 'info:fdaE20100110_AAACDPfileF20100110_AABOQD' 'sip-files00001.txt'
52aa02fb34eb7fc2106e31bda3a25b20
f70ac3637be1e2efef2e6d5ccb324f19d1d55d11
'2012-05-16T12:22:33-04:00'
describe
'41111' 'info:fdaE20100110_AAACDPfileF20100110_AABOQE' 'sip-files00001thm.jpg'
9b55df72e4093b42c43e0fc1e4fc511e
0bb61ceeff049f2d03ad55ba8ba6be5fa34fdec8
'2012-05-16T12:27:33-04:00'
describe
'1532851' 'info:fdaE20100110_AAACDPfileF20100110_AABOQF' 'sip-files00002.jp2'
68014664c6f0655bcc65575f98a09945
032d41418cd1892b906b91eab4bdd82b7c91a99d
'2012-05-16T12:24:13-04:00'
describe
'341284' 'info:fdaE20100110_AAACDPfileF20100110_AABOQG' 'sip-files00002.jpg'
6ffd2298cf6ada27080134fa13e8b97b
eff791af8d0d6849c8fba3533e5e0b02e5ef8799
'2012-05-16T12:25:47-04:00'
describe
'15885' 'info:fdaE20100110_AAACDPfileF20100110_AABOQH' 'sip-files00002.pro'
f47891aedd97296e1520a10df42d0e33
0ff6fd1ca0c6f555c33adbdd5f8957712611f64d
'2012-05-16T12:25:52-04:00'
describe
'105195' 'info:fdaE20100110_AAACDPfileF20100110_AABOQI' 'sip-files00002.QC.jpg'
b81a2b37a4953cd94b9ddafdb9eaebe3
0b62534b67c9530bf5c89008a2540929b4ef2b81
'2012-05-16T12:21:01-04:00'
describe
'15522638' 'info:fdaE20100110_AAACDPfileF20100110_AABOQJ' 'sip-files00002.tif'
28da3a86967ec424fa37b292d5470422
c9e62c30132b939f00593a07e2d15c91b8f8e3ce
'2012-05-16T12:21:41-04:00'
describe
'784' 'info:fdaE20100110_AAACDPfileF20100110_AABOQK' 'sip-files00002.txt'
5a8bf268f000dfc84f2043a4c15c2393
60f5bb1b3a6943416041f4f53f48bf63ac7233a7
'2012-05-16T12:24:06-04:00'
describe
'36846' 'info:fdaE20100110_AAACDPfileF20100110_AABOQL' 'sip-files00002thm.jpg'
f3071814897d3e781c7ad2d102ebaec8
ca1a8b358942b5f64cef4b9c431f811cd448e9ab
'2012-05-16T12:25:38-04:00'
describe
'2059515' 'info:fdaE20100110_AAACDPfileF20100110_AABOQM' 'sip-files00003.jp2'
bbe9f4201609959ba33a93bab8c29879
435b3edbaf545c769e03d94a611b814cdd1d8edb
'2012-05-16T12:23:12-04:00'
describe
'387937' 'info:fdaE20100110_AAACDPfileF20100110_AABOQN' 'sip-files00003.jpg'
59b82fe9080c902a083ead2be4b48374
f9ed9ba5931afec28e82a1372778524765700a3b
'2012-05-16T12:20:24-04:00'
describe
'6395' 'info:fdaE20100110_AAACDPfileF20100110_AABOQO' 'sip-files00003.pro'
872523966b580528327b2a435682d267
07c819b0f4a8347e99f3374433499f9f4af9c05a
'2012-05-16T12:24:12-04:00'
describe
'117878' 'info:fdaE20100110_AAACDPfileF20100110_AABOQP' 'sip-files00003.QC.jpg'
3bfaf4820c00e85c515cd8cde2f87247
757d727a640b3def061bdbb2673d657507cf3478
'2012-05-16T12:20:16-04:00'
describe
'16481418' 'info:fdaE20100110_AAACDPfileF20100110_AABOQQ' 'sip-files00003.tif'
87b8dcebce3b1db390f50095515b82b4
ebcd918a4ce029d1adf592ba4275a21db404179a
'2012-05-16T12:22:02-04:00'
describe
'297' 'info:fdaE20100110_AAACDPfileF20100110_AABOQR' 'sip-files00003.txt'
98bc02fc0eb166262b76ce4e9f4560df
89f190a45cac58bcc9edaa0438e28b9b10cf750c
'2012-05-16T12:26:38-04:00'
describe
'42003' 'info:fdaE20100110_AAACDPfileF20100110_AABOQS' 'sip-files00003thm.jpg'
8dc454329bbcadbe79c6a6a36b9beae3
38aeade106460ca966ca955d74edc44508614439
'2012-05-16T12:20:42-04:00'
describe
'487320' 'info:fdaE20100110_AAACDPfileF20100110_AABOQT' 'sip-files00004.jp2'
c7e038ed6d0ed4c4b0f991f0df966581
ed95d26b3b86ed1a8213f406d355906b0c9494ef
'2012-05-16T12:28:22-04:00'
describe
'366313' 'info:fdaE20100110_AAACDPfileF20100110_AABOQU' 'sip-files00004.jpg'
4fd13e18bf7b0e68a54e714b1097e967
30c85158b422d05bb8d4fca16a6ae15ac2acbc66
'2012-05-16T12:25:29-04:00'
describe
'41930' 'info:fdaE20100110_AAACDPfileF20100110_AABOQV' 'sip-files00004.pro'
e3f2efada68c4b4c3557b7755c415861
af6d6825bf1f149050d839855ddc6bb19af3554c
'2012-05-16T12:24:14-04:00'
describe
'126459' 'info:fdaE20100110_AAACDPfileF20100110_AABOQW' 'sip-files00004.QC.jpg'
42b5c9099302de0fc869189e4352102e
7f2362692096eeed2e50596a65cc54732339568d
'2012-05-16T12:24:27-04:00'
describe
'3901296' 'info:fdaE20100110_AAACDPfileF20100110_AABOQX' 'sip-files00004.tif'
33512e8b8fbcfdaeabc42f63e612fa8f
4687f0845501dda9ccb41a095d06075a3e9d6f70
describe
'1883' 'info:fdaE20100110_AAACDPfileF20100110_AABOQY' 'sip-files00004.txt'
31a3f29c21ebe7b181f57da497aea526
1052c085fbf4b9352d05781c410885bc18ff70fc
'2012-05-16T12:27:50-04:00'
describe
WARNING CODE 'Daitss::Anomaly' Invalid character
'41263' 'info:fdaE20100110_AAACDPfileF20100110_AABOQZ' 'sip-files00004thm.jpg'
c4d87ca52c3e95ba49e12234987c646d
2529d82a79ee686c7a85f8359e281148c512683e
'2012-05-16T12:22:09-04:00'
describe
'503532' 'info:fdaE20100110_AAACDPfileF20100110_AABORA' 'sip-files00005.jp2'
713ab7addfeec21520a885f266e1f2bc
55204285d3b516380283540b3fdf2adc9f3aa7e4
'2012-05-16T12:24:19-04:00'
describe
'439428' 'info:fdaE20100110_AAACDPfileF20100110_AABORB' 'sip-files00005.jpg'
b05f7394c822810597b5a5bd4c65f760
859b367e02f3ec8932a89199fbe9de07ef74efef
'2012-05-16T12:22:18-04:00'
describe
'54535' 'info:fdaE20100110_AAACDPfileF20100110_AABORC' 'sip-files00005.pro'
6ae77cfbbab08bafc2b542b53c7cb861
da6ee8f0902b5e3a38b5d2fddabe6efaf8e7c07f
'2012-05-16T12:26:33-04:00'
describe
'143671' 'info:fdaE20100110_AAACDPfileF20100110_AABORD' 'sip-files00005.QC.jpg'
021e4a36c8fd42487a42706ab59207f5
e17231d36fb184a1ccd3a7a2df34c1690c468e16
'2012-05-16T12:20:34-04:00'
describe
'4031410' 'info:fdaE20100110_AAACDPfileF20100110_AABORE' 'sip-files00005.tif'
77f91bf9315ace462ac59524c9c811cd
569d214066138649315114ca7184940ab9529ed5
'2012-05-16T12:18:36-04:00'
describe
'2254' 'info:fdaE20100110_AAACDPfileF20100110_AABORF' 'sip-files00005.txt'
c13073afdbfddbd00c5e13baf6aea03a
46e790f650ae812e368b1524daa095d8ce1286a0
'2012-05-16T12:21:08-04:00'
describe
'45584' 'info:fdaE20100110_AAACDPfileF20100110_AABORG' 'sip-files00005thm.jpg'
8f6921381ca4d123a7a9d56e9e67ec24
108d002faffb578e0aaf6bfc6b197a3ddcc4b681
'2012-05-16T12:21:02-04:00'
describe
'1959020' 'info:fdaE20100110_AAACDPfileF20100110_AABORH' 'sip-files00006.jp2'
263ee684632ef80344de2ae1454cb357
885ba696e1434ecbc3bb5103177f1d0116520fbe
'2012-05-16T12:25:42-04:00'
describe
'348943' 'info:fdaE20100110_AAACDPfileF20100110_AABORI' 'sip-files00006.jpg'
98695057ce9af01b0551c5e9a7063771
00a230357e831439a504fbf0b520955fe7911fe2
'2012-05-16T12:18:18-04:00'
describe
'10404' 'info:fdaE20100110_AAACDPfileF20100110_AABORJ' 'sip-files00006.pro'
ecd0e5153c9575eeddff4dee8ff85428
fbd89ff3c6fb6ff83005dce514fd7ef900321e56
'2012-05-16T12:21:48-04:00'
describe
'111305' 'info:fdaE20100110_AAACDPfileF20100110_AABORK' 'sip-files00006.QC.jpg'
35e489f76a1a5ffd9869959f9c18a9bb
9da360b3539b454c74daefa1ddf540b1034fd163
'2012-05-16T12:20:17-04:00'
describe
'15677300' 'info:fdaE20100110_AAACDPfileF20100110_AABORL' 'sip-files00006.tif'
9f5a12460a1c26427885c412ce30206d
3c3f82b309b67a3c7dc63e904863bf42710bd4b0
'2012-05-16T12:20:12-04:00'
describe
'839' 'info:fdaE20100110_AAACDPfileF20100110_AABORM' 'sip-files00006.txt'
6e1e3d88a1cb20f5c7c4a744b147b51f
7a111096794a6d9bb79a074660abdb4cce4651e2
'2012-05-16T12:22:53-04:00'
describe
'39497' 'info:fdaE20100110_AAACDPfileF20100110_AABORN' 'sip-files00006thm.jpg'
7300d33a664938f0c6d0cafc1d968698
56b105743f7c43b9216cd120055c21af2901082e
'2012-05-16T12:28:32-04:00'
describe
'502223' 'info:fdaE20100110_AAACDPfileF20100110_AABORO' 'sip-files00007.jp2'
5dccde9863983e523b0fd02937842dc7
8f323d98e2052ebd470bf35b92cfe2faa3fd46fb
'2012-05-16T12:20:22-04:00'
describe
'545703' 'info:fdaE20100110_AAACDPfileF20100110_AABORP' 'sip-files00007.jpg'
5e6e26468314d6f90424975c0ee1f2f4
a0da963245799c2378a7cd58c5aba90fa7c65df8
'2012-05-16T12:28:23-04:00'
describe
'65224' 'info:fdaE20100110_AAACDPfileF20100110_AABORQ' 'sip-files00007.pro'
ab0542f95570d916eec4061e22b908b5
08e913452d227ddb6b5fe75f202919578d8b108d
'2012-05-16T12:21:54-04:00'
describe
'169057' 'info:fdaE20100110_AAACDPfileF20100110_AABORR' 'sip-files00007.QC.jpg'
7eee8239451c7795022a29bdab9b090b
5b0ab46a1930ac8ecb0ec80ffb0eb3163fd9ef36
'2012-05-16T12:19:24-04:00'
describe
'4020354' 'info:fdaE20100110_AAACDPfileF20100110_AABORS' 'sip-files00007.tif'
065897a676e3f47bc3b180cd2edb39a3
35d4d0218faa5dce38a34a8093ab7a99ba84cad6
'2012-05-16T12:24:24-04:00'
describe
'2576' 'info:fdaE20100110_AAACDPfileF20100110_AABORT' 'sip-files00007.txt'
1685ba1d1200b7fed7354c44545bc36a
e1b3c7f3d8c5caa145bc6bb2a3bb26b9e80098d9
'2012-05-16T12:23:17-04:00'
describe
'49754' 'info:fdaE20100110_AAACDPfileF20100110_AABORU' 'sip-files00007thm.jpg'
d7856620f2645c5130258b812e3657c1
12471c1f638a443524a2a28284638b1d1a6cc5b4
'2012-05-16T12:25:08-04:00'
describe
'2050548' 'info:fdaE20100110_AAACDPfileF20100110_AABORV' 'sip-files00008.jp2'
4bbb138cb87abf29fe21a7ec1b709aa6
ff7de7bfea2eb43436c8411192f72edfeb850ef8
'2012-05-16T12:20:59-04:00'
describe
'433683' 'info:fdaE20100110_AAACDPfileF20100110_AABORW' 'sip-files00008.jpg'
c8e7c8420d1d52df8e47ce0182091d84
3a1c13295afcdbc498168db1e222ec25a13087d3
'2012-05-16T12:28:25-04:00'
describe
'18945' 'info:fdaE20100110_AAACDPfileF20100110_AABORX' 'sip-files00008.pro'
65152e276c2dff2f6c6749d47937424e
a77de7df52e46140a3edae8c6542d92413ad723b
'2012-05-16T12:27:52-04:00'
describe
'126497' 'info:fdaE20100110_AAACDPfileF20100110_AABORY' 'sip-files00008.QC.jpg'
e870af42cfa056d60ed5e8def651c7c5
ee3adf408370ee7ffa5d4b0237736cd760eb7edd
'2012-05-16T12:21:13-04:00'
describe
'16409758' 'info:fdaE20100110_AAACDPfileF20100110_AABORZ' 'sip-files00008.tif'
1f7a5d329aee72653fa126410800ca5d
2108ebe4a6acdf73e415ecf96ed4c483d8f8a939
'2012-05-16T12:24:50-04:00'
describe
'896' 'info:fdaE20100110_AAACDPfileF20100110_AABOSA' 'sip-files00008.txt'
57da67768266ee7fdad845ae7037872a
f20904b99bf52d428dd1fe26d8faf5b53b78e40a
'2012-05-16T12:18:52-04:00'
describe
Invalid character
'41546' 'info:fdaE20100110_AAACDPfileF20100110_AABOSB' 'sip-files00008thm.jpg'
1972cadab34ea463926295c3bd2015e0
58a4cd294a2a7f15b34bf92127edc9ba6ae5633b
'2012-05-16T12:20:23-04:00'
describe
'515223' 'info:fdaE20100110_AAACDPfileF20100110_AABOSC' 'sip-files00009.jp2'
c5ef41e02d673cac2df306eeaa6ccb5f
83164a21d6dec4c765f2cbd7c3d687f24a902a26
'2012-05-16T12:27:08-04:00'
describe
'490850' 'info:fdaE20100110_AAACDPfileF20100110_AABOSD' 'sip-files00009.jpg'
8c8fb5e1646da97ece8c870c86547bc0
b207eaa169d2467be1ede7265dd1107581796a44
'2012-05-16T12:27:05-04:00'
describe
'56785' 'info:fdaE20100110_AAACDPfileF20100110_AABOSE' 'sip-files00009.pro'
e4a3521614084bd818df34480c18b710
0b9f066040f69e5d68d45e09d5971e282a3c6fc8
'2012-05-16T12:27:07-04:00'
describe
'153083' 'info:fdaE20100110_AAACDPfileF20100110_AABOSF' 'sip-files00009.QC.jpg'
e53ce246d03378b96a41e8fde7c20c57
376c0ab0d0a66f42e761c6c8468919c773b53af3
describe
'4124636' 'info:fdaE20100110_AAACDPfileF20100110_AABOSG' 'sip-files00009.tif'
7814a64f81d815c6ed57bc4ac338e9e1
cad048d28d5c617bee94c7e5e8518f89cb6bfcb5
'2012-05-16T12:27:51-04:00'
describe
'2336' 'info:fdaE20100110_AAACDPfileF20100110_AABOSH' 'sip-files00009.txt'
92a1633398dd3e8c7bf3bb70f124d2c3
8a85709e38b460e8f1a0c6d8c391b79a673fd103
'2012-05-16T12:23:24-04:00'
describe
'44247' 'info:fdaE20100110_AAACDPfileF20100110_AABOSI' 'sip-files00009thm.jpg'
d604ccd8340c6a60ab78f3ac5e37e759
89d9d13cb3559bfb71f442fd732f1b570688d299
'2012-05-16T12:26:19-04:00'
describe
'1970276' 'info:fdaE20100110_AAACDPfileF20100110_AABOSJ' 'sip-files00010.jp2'
255f5a2f27bb2d83b6afe32e6d7b2ef1
fa4885690c6478768fbc3a51ffe73f3367afdfc8
'2012-05-16T12:26:25-04:00'
describe
'569243' 'info:fdaE20100110_AAACDPfileF20100110_AABOSK' 'sip-files00010.jpg'
8ab22716196d27e5e7f7bbab4469635e
7e23f8275ddf1b82dc95b80224dd21104d4435f8
'2012-05-16T12:20:32-04:00'
describe
'40146' 'info:fdaE20100110_AAACDPfileF20100110_AABOSL' 'sip-files00010.pro'
4abf05d4b6daf8769c84f35a571fb25d
4a333333f103243f6859abccd453fd80de0eeece
'2012-05-16T12:25:12-04:00'
describe
'162089' 'info:fdaE20100110_AAACDPfileF20100110_AABOSM' 'sip-files00010.QC.jpg'
a837db43cf2ef7d78874db53eed380a9
825abe3ee362048768cbc9580bdab3f79bcf5384
'2012-05-16T12:27:01-04:00'
describe
'15767388' 'info:fdaE20100110_AAACDPfileF20100110_AABOSN' 'sip-files00010.tif'
f4eea59a4bee665cb793cfa7376c798b
6b54b368b68f649415d6cd1d9f50879349c4d6ba
'2012-05-16T12:23:40-04:00'
describe
'1739' 'info:fdaE20100110_AAACDPfileF20100110_AABOSO' 'sip-files00010.txt'
00f0ecff210e08b8529600c8eda703d1
46c6daeb25fa15bf755d099e86cb0c491b20fda3
'2012-05-16T12:25:32-04:00'
describe
Invalid character
'50321' 'info:fdaE20100110_AAACDPfileF20100110_AABOSP' 'sip-files00010thm.jpg'
b2ce792c6c49231814a0a22f85123dee
1ff01d0ea468b63ffd53f747ff0c53058a71de38
'2012-05-16T12:21:28-04:00'
describe
'531767' 'info:fdaE20100110_AAACDPfileF20100110_AABOSQ' 'sip-files00011.jp2'
0bdf90ccba3c29e489d21c1e227fbe13
b3be969a74782eb50f16f39748e52601a3a582b7
'2012-05-16T12:28:34-04:00'
describe
'515016' 'info:fdaE20100110_AAACDPfileF20100110_AABOSR' 'sip-files00011.jpg'
7023029f55fcb16b3d11b611464d2299
9c7484cb0d290918c11f0380f57e80a327a28d79
'2012-05-16T12:19:18-04:00'
describe
'60437' 'info:fdaE20100110_AAACDPfileF20100110_AABOSS' 'sip-files00011.pro'
6984f9baebf57fd0d571b2a9c151ae7b
afb1e520c5989a03ed9e90f48337853ea1d457f6
'2012-05-16T12:27:02-04:00'
describe
'156278' 'info:fdaE20100110_AAACDPfileF20100110_AABOST' 'sip-files00011.QC.jpg'
df2d96cd84217bc0483da7ae0b989b64
43a3160f22d1870dc267e88dca780cafd48559e1
'2012-05-16T12:20:46-04:00'
describe
'4256660' 'info:fdaE20100110_AAACDPfileF20100110_AABOSU' 'sip-files00011.tif'
f6475b4edf1b9df35d15f5ef614a387a
31ad03661dd7b3c1fff972498da980e82f526631
'2012-05-16T12:26:55-04:00'
describe
'2606' 'info:fdaE20100110_AAACDPfileF20100110_AABOSV' 'sip-files00011.txt'
f7f1e3bd8788e3b9469262f29b7b0390
7e3541475da3edda60cad8a0b7420d19b25f0b5c
'2012-05-16T12:27:35-04:00'
describe
'44217' 'info:fdaE20100110_AAACDPfileF20100110_AABOSW' 'sip-files00011thm.jpg'
ec88ce24b9555b49094f6977ce7db3d8
fff804c38413a7527d02064a4c08a6f7f7ac0286
'2012-05-16T12:25:28-04:00'
describe
'489652' 'info:fdaE20100110_AAACDPfileF20100110_AABOSX' 'sip-files00012.jp2'
24806eebca13c0533bb07d0778177fde
6b65d9e2442656d878aec9afba1d187a621f679a
'2012-05-16T12:26:47-04:00'
describe
'523756' 'info:fdaE20100110_AAACDPfileF20100110_AABOSY' 'sip-files00012.jpg'
809f0d14f1b7a14ee7fb48c0df286596
dcee701d2ea2d46eada08cdc1d703090305d2609
'2012-05-16T12:24:58-04:00'
describe
'62359' 'info:fdaE20100110_AAACDPfileF20100110_AABOSZ' 'sip-files00012.pro'
df823cf099b07709ab2abd51744d944c
1c5413e15b153b41b05013ffc202ca9a7f233ace
'2012-05-16T12:19:32-04:00'
describe
'163100' 'info:fdaE20100110_AAACDPfileF20100110_AABOTA' 'sip-files00012.QC.jpg'
d16454282f8845770a200dbd16d56b18
d9059c48c75022ea882fca3e0c45efa95c12d02a
'2012-05-16T12:21:50-04:00'
describe
'3919778' 'info:fdaE20100110_AAACDPfileF20100110_AABOTB' 'sip-files00012.tif'
f21f2134a32999dac9682e6fcfc91718
cb69c6a8da4734c8d9218396318e4fffb8dbbdac
'2012-05-16T12:25:14-04:00'
describe
'2515' 'info:fdaE20100110_AAACDPfileF20100110_AABOTC' 'sip-files00012.txt'
47c5d76961be83a713f441ccd0e781d2
ca3a988641ca85c18e19edc0c43ef71b03516a02
'2012-05-16T12:21:31-04:00'
describe
'48082' 'info:fdaE20100110_AAACDPfileF20100110_AABOTD' 'sip-files00012thm.jpg'
f8e4a262483622f1cbcb17fc2703f660
3d1ce41a65bd9ed6380e005b190c26dd54f7e241
'2012-05-16T12:26:07-04:00'
describe
'2042519' 'info:fdaE20100110_AAACDPfileF20100110_AABOTE' 'sip-files00013.jp2'
e4d3a9b30561b92c2ff82c47177b8745
c276be9b5ae5ec25a02766bdd15631bd6981706c
'2012-05-16T12:24:34-04:00'
describe
'392251' 'info:fdaE20100110_AAACDPfileF20100110_AABOTF' 'sip-files00013.jpg'
96597825d7bdbf435b2ddf87a734d354
1f67dd7cc830113a256b0b0af57465096a23e9a2
'2012-05-16T12:27:56-04:00'
describe
'16118' 'info:fdaE20100110_AAACDPfileF20100110_AABOTG' 'sip-files00013.pro'
5243b02081a602097b5e70a0ccfa8ed9
a89b068a658e4d3b322ec7ea4273fa2bf7c19ff7
'2012-05-16T12:18:56-04:00'
describe
'116789' 'info:fdaE20100110_AAACDPfileF20100110_AABOTH' 'sip-files00013.QC.jpg'
edc21ac7ff933b883d02ab8333f01ea2
a24fe5d2f1db9e401db941014f4c8671c0785f60
'2012-05-16T12:21:30-04:00'
describe
'16345444' 'info:fdaE20100110_AAACDPfileF20100110_AABOTI' 'sip-files00013.tif'
1e1d84cb8e3add002c4ef304b155e1ab
1896096f8dd377d580ab507743fe662e32108feb
'2012-05-16T12:24:15-04:00'
describe
'939' 'info:fdaE20100110_AAACDPfileF20100110_AABOTJ' 'sip-files00013.txt'
e9c1fb5c22510bc19dc26551d527bf4e
83c57500bffce1ad85f8398dfbb49bbd69621454
'2012-05-16T12:25:07-04:00'
describe
Invalid character
'39093' 'info:fdaE20100110_AAACDPfileF20100110_AABOTK' 'sip-files00013thm.jpg'
5d8c970a73c20fea941d8ac2fcf2a5b0
d7d08daed1912eb339388834d54c8bfd09f31b1d
'2012-05-16T12:27:00-04:00'
describe
'499525' 'info:fdaE20100110_AAACDPfileF20100110_AABOTL' 'sip-files00014.jp2'
03a9ca9bf87d925fa92ab02074192915
5dabb96a44100f3a40bae7d085df3b576c806414
'2012-05-16T12:28:09-04:00'
describe
'545998' 'info:fdaE20100110_AAACDPfileF20100110_AABOTM' 'sip-files00014.jpg'
27e2e2757cd485963bd904364db2811a
60f058c3802e9b1941391b044883c5cca9a156ef
'2012-05-16T12:24:46-04:00'
describe
'66295' 'info:fdaE20100110_AAACDPfileF20100110_AABOTN' 'sip-files00014.pro'
6bf853704263a5b728a675137776166f
fc20fe9769495fdb8d11e2e12469928fa9295bb1
'2012-05-16T12:23:05-04:00'
describe
'172529' 'info:fdaE20100110_AAACDPfileF20100110_AABOTO' 'sip-files00014.QC.jpg'
2b3a9f4ebf6f594a55f10ff78f3cfbdd
5227dd563ebe6f23452a3b3eb5ea85a2bec5224c
'2012-05-16T12:26:56-04:00'
describe
'3998878' 'info:fdaE20100110_AAACDPfileF20100110_AABOTP' 'sip-files00014.tif'
8852a40c5db6b0fbd3b620e1b22fc059
76bb71da254060f1f18637dd2868de91522f5cd6
'2012-05-16T12:22:25-04:00'
describe
'2634' 'info:fdaE20100110_AAACDPfileF20100110_AABOTQ' 'sip-files00014.txt'
be4385800924599027d51e13718e882e
4e8cd1c40e8a77f2208306838c660b3914bf5d38
'2012-05-16T12:23:44-04:00'
describe
'50866' 'info:fdaE20100110_AAACDPfileF20100110_AABOTR' 'sip-files00014thm.jpg'
58f624db6e7ed04477e571fe0726b600
fac026a7d5904308266c6d26ffc21d9293a71c43
'2012-05-16T12:21:49-04:00'
describe
'523801' 'info:fdaE20100110_AAACDPfileF20100110_AABOTS' 'sip-files00015.jp2'
088aafd236996fa2cb6981166141470c
c262376a5ea5a92fa7deb530c3b02cdb5d57fdb9
'2012-05-16T12:28:13-04:00'
describe
'476133' 'info:fdaE20100110_AAACDPfileF20100110_AABOTT' 'sip-files00015.jpg'
551a656d4bfd3f1a2850221fdfd6575a
46956bd34b50e5bec592f66d03d764ddf7d5a4d9
'2012-05-16T12:23:50-04:00'
describe
'54771' 'info:fdaE20100110_AAACDPfileF20100110_AABOTU' 'sip-files00015.pro'
092e7da0eab8ba174e442f5cf412cdbf
a15955f8f413f86dbccd111571af9d9ca0f94213
'2012-05-16T12:18:37-04:00'
describe
'150416' 'info:fdaE20100110_AAACDPfileF20100110_AABOTV' 'sip-files00015.QC.jpg'
72b64ad5edc815ffcb882da0fe78901c
d6ea8a49b411b4eb59856da858c5e98b93d9414a
'2012-05-16T12:23:35-04:00'
describe
'4193044' 'info:fdaE20100110_AAACDPfileF20100110_AABOTW' 'sip-files00015.tif'
365a42ca99c615fb6cca461085db2514
dacdf180f42d19fe737d51477a570e5a7ed3c5d3
'2012-05-16T12:21:24-04:00'
describe
'2241' 'info:fdaE20100110_AAACDPfileF20100110_AABOTX' 'sip-files00015.txt'
49bdb54f77493f515766ed9941673172
015abe1ce8dba703dc6aa018b2c9a5b4338f990c
'2012-05-16T12:20:13-04:00'
describe
'43460' 'info:fdaE20100110_AAACDPfileF20100110_AABOTY' 'sip-files00015thm.jpg'
3a1e037351577f85519a1db7d95ea95c
4a382c041b059e07fac1370d2e444e8b5f236de4
'2012-05-16T12:23:55-04:00'
describe
'489400' 'info:fdaE20100110_AAACDPfileF20100110_AABOTZ' 'sip-files00016.jp2'
b2e69fd3d7faf3537950a4e50c669b84
c99c42490fc8e04939cc40d4eac517c7c393ad87
'2012-05-16T12:25:27-04:00'
describe
'495569' 'info:fdaE20100110_AAACDPfileF20100110_AABOUA' 'sip-files00016.jpg'
99bc526a274200744cdf6edea6bc139c
9762ce7a566d0493777415d530195e5fa273bd01
'2012-05-16T12:23:02-04:00'
describe
'61337' 'info:fdaE20100110_AAACDPfileF20100110_AABOUB' 'sip-files00016.pro'
14569a4c9803da858bf9b1be4a18ba9f
fd10f1a46a706108bccbfceaf84a659fee2702f9
'2012-05-16T12:18:49-04:00'
describe
'158453' 'info:fdaE20100110_AAACDPfileF20100110_AABOUC' 'sip-files00016.QC.jpg'
70f6d892c55a3d437630872bdc35f636
685507d6dbd3150f8d89bddc07541f1f34fa38df
'2012-05-16T12:18:57-04:00'
describe
'3918370' 'info:fdaE20100110_AAACDPfileF20100110_AABOUD' 'sip-files00016.tif'
75242b9a1b42b19db6a9ae20ef54c083
d9ecaec4e11f89068aa4fb73e0ecfe9c4dd1c073
'2012-05-16T12:28:28-04:00'
describe
'2449' 'info:fdaE20100110_AAACDPfileF20100110_AABOUE' 'sip-files00016.txt'
cd99713e72b1f1ae9d4266c68f403189
3cfbb92f056033783b3e20aa7bb3efdf5129c16d
'2012-05-16T12:25:34-04:00'
describe
'50413' 'info:fdaE20100110_AAACDPfileF20100110_AABOUF' 'sip-files00016thm.jpg'
54260913f221c7fac759e40ca43ce4ff
a061556bdebe9b1907f34260630270e2adcea1cc
'2012-05-16T12:26:09-04:00'
describe
'2064880' 'info:fdaE20100110_AAACDPfileF20100110_AABOUG' 'sip-files00017.jp2'
4a19f7f4e9e5d5c5fc7f6fd9a6a444d3
e94e777f12695e9ebc95a5337eee42ef9c9e028c
'2012-05-16T12:22:17-04:00'
describe
'561566' 'info:fdaE20100110_AAACDPfileF20100110_AABOUH' 'sip-files00017.jpg'
5ec5f12b559b440ec759e09808463f6a
c037a9b87fd263de36a0e5ab2f85c15b48149a3f
'2012-05-16T12:21:05-04:00'
describe
'35280' 'info:fdaE20100110_AAACDPfileF20100110_AABOUI' 'sip-files00017.pro'
fde18706b029fbb1b789c6068e6792e2
b73a3100fd61ee1116ea275c805d484af3051d7e
'2012-05-16T12:23:58-04:00'
describe
'159432' 'info:fdaE20100110_AAACDPfileF20100110_AABOUJ' 'sip-files00017.QC.jpg'
be63e8fd24bc481f26408c3887370a88
d4dfe12ab3e0955ec252aa27e810d76df2ba0dd8
'2012-05-16T12:26:03-04:00'
describe
'16524202' 'info:fdaE20100110_AAACDPfileF20100110_AABOUK' 'sip-files00017.tif'
7e81b61ca813a8d3024fb62a239e8da3
8cc4ba4e08302d3123f0369e62ddbbcfd14bad41
'2012-05-16T12:19:43-04:00'
describe
'1409' 'info:fdaE20100110_AAACDPfileF20100110_AABOUL' 'sip-files00017.txt'
94a73670aec1b5f3914c0eb6249980c4
9f534f6b782bff5c45878d90fcdb0fd7cbbfec4d
'2012-05-16T12:20:54-04:00'
describe
'48832' 'info:fdaE20100110_AAACDPfileF20100110_AABOUM' 'sip-files00017thm.jpg'
9b972fd45f55c0be1559167a8fa27579
098aaede766cac4425fe1a71b955267d668ed799
'2012-05-16T12:26:02-04:00'
describe
'493784' 'info:fdaE20100110_AAACDPfileF20100110_AABOUN' 'sip-files00018.jp2'
e670d77a263ad3aca92254e09aec2dcf
de030edb1c9aa1ebe409f195f1c16ccbf9aa3fd1
'2012-05-16T12:18:14-04:00'
describe
'508778' 'info:fdaE20100110_AAACDPfileF20100110_AABOUO' 'sip-files00018.jpg'
bfcedaed2616a74d3450608417e7c2ac
1c820f13dc94d7773e076e3dfcf9e3df2f575e1c
'2012-05-16T12:20:51-04:00'
describe
'59933' 'info:fdaE20100110_AAACDPfileF20100110_AABOUP' 'sip-files00018.pro'
9ba3500b0255c0cc0fbce4fbb70ce57b
a2a7466205f2c74faafdf6978c66de2fce6be0fb
'2012-05-16T12:28:29-04:00'
describe
'161405' 'info:fdaE20100110_AAACDPfileF20100110_AABOUQ' 'sip-files00018.QC.jpg'
54b377d79e2a9f8a942ba10836223d29
d9aeb66831891e5bba3891dc2869626cfb6647ca
'2012-05-16T12:26:32-04:00'
describe
'3953096' 'info:fdaE20100110_AAACDPfileF20100110_AABOUR' 'sip-files00018.tif'
efc29a88b692505effd0c355c37a3cec
b9bca6b68d4f438245473292a03386f498d283f7
'2012-05-16T12:21:03-04:00'
describe
'2406' 'info:fdaE20100110_AAACDPfileF20100110_AABOUS' 'sip-files00018.txt'
fc983e3b5db18728ca64a4860b4cb998
d64c9fcb7b74e3fa9a477ed78c92f53bd503ad15
'2012-05-16T12:19:25-04:00'
describe
'47574' 'info:fdaE20100110_AAACDPfileF20100110_AABOUT' 'sip-files00018thm.jpg'
1c72c2b19529acb04c8912815456bb44
2abc40777f87ee8701f283c4361b17c8649eaebd
'2012-05-16T12:27:49-04:00'
describe
'521732' 'info:fdaE20100110_AAACDPfileF20100110_AABOUU' 'sip-files00019.jp2'
8d7903269d2d47d98e229feaf8a59307
8323f52f2eec72ae84781092c50249f9e9295bb5
describe
'538619' 'info:fdaE20100110_AAACDPfileF20100110_AABOUV' 'sip-files00019.jpg'
4025597a7e1464ff8f8c3e0f517dc1ba
3db4f08b4ecc3d8be79fa24427e7708d7d010677
'2012-05-16T12:28:00-04:00'
describe
'63272' 'info:fdaE20100110_AAACDPfileF20100110_AABOUW' 'sip-files00019.pro'
094063d2000957f67fd870a962aab860
3be56f02994212540b6036854fec5e23e1b0224d
'2012-05-16T12:20:02-04:00'
describe
'164498' 'info:fdaE20100110_AAACDPfileF20100110_AABOUX' 'sip-files00019.QC.jpg'
ad9eff2b2a8c0b6b46dadca85c63298e
f8fb790091b2f682aedada34bbaa0dfe7af3c77d
'2012-05-16T12:23:53-04:00'
describe
'4177160' 'info:fdaE20100110_AAACDPfileF20100110_AABOUY' 'sip-files00019.tif'
5a5177e5895892e5d05ced51c83b8796
45712350ae3547962d7fa0939bfafd457b8ca60d
'2012-05-16T12:25:04-04:00'
describe
'2554' 'info:fdaE20100110_AAACDPfileF20100110_AABOUZ' 'sip-files00019.txt'
c0861337907110522f571d7e720a55d6
5138912e6e8e963684912441c3afca678412849b
describe
'47466' 'info:fdaE20100110_AAACDPfileF20100110_AABOVA' 'sip-files00019thm.jpg'
2d5834a89a6b840e207ee073c74df0eb
0fab6cae7b3bef92339f0a9d941f009b93c1b549
'2012-05-16T12:26:00-04:00'
describe
'480473' 'info:fdaE20100110_AAACDPfileF20100110_AABOVB' 'sip-files00020.jp2'
a89f5c5dbd268e5463dbbdd082ec6bcd
6104531120068aaa49334ad1cefc0b13feee9d1f
'2012-05-16T12:20:18-04:00'
describe
'470585' 'info:fdaE20100110_AAACDPfileF20100110_AABOVC' 'sip-files00020.jpg'
ba3831d7997a4716a0faf3361c3ed430
4f6d368627f2fee6645c9492745a76aca2732c10
'2012-05-16T12:19:29-04:00'
describe
'53564' 'info:fdaE20100110_AAACDPfileF20100110_AABOVD' 'sip-files00020.pro'
881955c165823aae8000613cea23488f
9c3474eb1aceb2a92f3968fada5be779f5780ed9
'2012-05-16T12:22:50-04:00'
describe
'151111' 'info:fdaE20100110_AAACDPfileF20100110_AABOVE' 'sip-files00020.QC.jpg'
c0929fb3a637b5014db41c15ec608458
9b9d4aeb192e62b7f919d9f5c68ced48b28558c3
'2012-05-16T12:18:28-04:00'
describe
'3846256' 'info:fdaE20100110_AAACDPfileF20100110_AABOVF' 'sip-files00020.tif'
a3b0003f6cab199fec8a428ff6bc90c3
4681ad6a5b5a23c6c5395afd42e2d9d46d8bfafe
'2012-05-16T12:19:41-04:00'
describe
'2206' 'info:fdaE20100110_AAACDPfileF20100110_AABOVG' 'sip-files00020.txt'
3e3daa65f61748273856b08d5a230a77
8d1f7014ab76aa147554585eacd896928288f95d
'2012-05-16T12:25:00-04:00'
describe
'46455' 'info:fdaE20100110_AAACDPfileF20100110_AABOVH' 'sip-files00020thm.jpg'
a611f8bd3745361751811f7f41b895e7
9657b072b4eaa2efb3096ae9a676b03a79daf061
'2012-05-16T12:26:14-04:00'
describe
'2034403' 'info:fdaE20100110_AAACDPfileF20100110_AABOVI' 'sip-files00021.jp2'
235ddc423b825a87f8f388e571be1a40
4424e751ba4aa9a0ee2132cc3d1615c0f5917be0
'2012-05-16T12:27:11-04:00'
describe
'525408' 'info:fdaE20100110_AAACDPfileF20100110_AABOVJ' 'sip-files00021.jpg'
d8369ee0fde487dd42e94b6b8cf2f2db
bb7c3a90661a7caedca6377d5d5d2a54836743ff
'2012-05-16T12:23:47-04:00'
describe
'17490' 'info:fdaE20100110_AAACDPfileF20100110_AABOVK' 'sip-files00021.pro'
6274fec0207c1384a9abca6c41139212
f9b73b73dda2a25de5b38dd1755450fab2a96c4f
'2012-05-16T12:26:04-04:00'
describe
'151540' 'info:fdaE20100110_AAACDPfileF20100110_AABOVL' 'sip-files00021.QC.jpg'
cf5100af86ffd358b0e4284e6c9c90da
fdd568868cad7e22ce8a944b37c2abdf356d316c
'2012-05-16T12:26:21-04:00'
describe
'16281010' 'info:fdaE20100110_AAACDPfileF20100110_AABOVM' 'sip-files00021.tif'
e93073858ccc8e336d5e64877116984f
a59605f7eba5f573cd5ae206ce6be0de59f7ab7b
'2012-05-16T12:25:59-04:00'
describe
'info:fdaE20100110_AAACDPfileF20100110_AABOVN' 'sip-files00021.txt'
2a9d87084c91354d2ed679add453bd68
f42b71deb03e034541e3aea1804a2100827f7102
describe
'47954' 'info:fdaE20100110_AAACDPfileF20100110_AABOVO' 'sip-files00021thm.jpg'
b1a44378023931e6ca9b75b019827fe7
84671c50e977d312f6cd08668a92f63595d726c7
describe
'486672' 'info:fdaE20100110_AAACDPfileF20100110_AABOVP' 'sip-files00022.jp2'
501691aa54a4cf07697764b7ee106539
f1dea7799e6426923759d35e1cc57e7e8e6edf37
describe
'441652' 'info:fdaE20100110_AAACDPfileF20100110_AABOVQ' 'sip-files00022.jpg'
91f5ff771197bf72ebc40679a934b7a3
0aa88a5c5e8a6b453ebc940ecb063fd4a3970dc8
'2012-05-16T12:22:32-04:00'
describe
'49532' 'info:fdaE20100110_AAACDPfileF20100110_AABOVR' 'sip-files00022.pro'
f3061528d1ef52079f6e8455a14a8f53
1f19c10f62eb1980d969f9d080764a88099ec5d7
'2012-05-16T12:28:18-04:00'
describe
'140972' 'info:fdaE20100110_AAACDPfileF20100110_AABOVS' 'sip-files00022.QC.jpg'
1abb7d04d7a646b3cb94ba90841c5fea
93971c60011e8752c8abbb15f0772a6d08ba3d0a
'2012-05-16T12:20:28-04:00'
describe
'3895854' 'info:fdaE20100110_AAACDPfileF20100110_AABOVT' 'sip-files00022.tif'
c56b40027db212cd08e934db971e7907
979b86aef9fa0bb7c1856c019a5efe7e1f48209f
'2012-05-16T12:24:53-04:00'
describe
'2096' 'info:fdaE20100110_AAACDPfileF20100110_AABOVU' 'sip-files00022.txt'
b3476709c1ac049a6c14fa41ec64e82e
4d1556757049d15441505ba686e3e2bc38b31b49
describe
'45984' 'info:fdaE20100110_AAACDPfileF20100110_AABOVV' 'sip-files00022thm.jpg'
62a397c39e23672c61b6e8d2fba50718
41a95ae45b4fbf8cc701d95265ba9010c6114e74
'2012-05-16T12:26:15-04:00'
describe
'514777' 'info:fdaE20100110_AAACDPfileF20100110_AABOVW' 'sip-files00023.jp2'
280baa91e5d22949aa8f020a14496f3d
29bb2c83c9dc885fcb070d8131ffb857b73ba2a4
'2012-05-16T12:24:42-04:00'
describe
'420258' 'info:fdaE20100110_AAACDPfileF20100110_AABOVX' 'sip-files00023.jpg'
215f0da522179e542fa27627cd380991
26378e51c5c5b4dd592aafb2eca3dee82a81d78d
'2012-05-16T12:18:17-04:00'
describe
'37523' 'info:fdaE20100110_AAACDPfileF20100110_AABOVY' 'sip-files00023.pro'
ef85b4f4d7ca3c355a80067cf8c97fa7
eada7b8f4f0228122846df2a9ddaa255687b4af8
'2012-05-16T12:27:59-04:00'
describe
'125860' 'info:fdaE20100110_AAACDPfileF20100110_AABOVZ' 'sip-files00023.QC.jpg'
9977ce37588dd1a4d22f5a25579bbad2
b914f01eb691e9810169a7a6f45c9ce517f839d5
'2012-05-16T12:19:20-04:00'
describe
'4120852' 'info:fdaE20100110_AAACDPfileF20100110_AABOWA' 'sip-files00023.tif'
f0a9d1dcfa05e5991ed0ee9ab820eb59
58e724148d5cea080de0938dcc199c8377021849
'2012-05-16T12:20:08-04:00'
describe
'1675' 'info:fdaE20100110_AAACDPfileF20100110_AABOWB' 'sip-files00023.txt'
31f346cf3264e5b3edea729d9401aeb1
bfbe75acefaa929078d235474fd959db620cc3b4
describe
'41387' 'info:fdaE20100110_AAACDPfileF20100110_AABOWC' 'sip-files00023thm.jpg'
13639c621572fb6c3c676a148fad9f97
52bf7fbbd27394755fa1deea9fa4c1e9eb77e19e
'2012-05-16T12:22:54-04:00'
describe
'481071' 'info:fdaE20100110_AAACDPfileF20100110_AABOWD' 'sip-files00024.jp2'
8311d6b5cd358fcdcc09caece1ce192f
c82810ebe2d37ccb5531e2290032d1de502a7f89
'2012-05-16T12:27:30-04:00'
describe
'407967' 'info:fdaE20100110_AAACDPfileF20100110_AABOWE' 'sip-files00024.jpg'
80da713b442691c46539cabf34c71eba
c11916260fb59f074dd5aac2ec9ccaa403a7a06d
'2012-05-16T12:25:54-04:00'
describe
'40499' 'info:fdaE20100110_AAACDPfileF20100110_AABOWF' 'sip-files00024.pro'
c2b58175bcf9362acbc61a1042909f54
26e32ab2e790d92e054801212033c81e2c0eee26
'2012-05-16T12:24:44-04:00'
describe
'129538' 'info:fdaE20100110_AAACDPfileF20100110_AABOWG' 'sip-files00024.QC.jpg'
50d269b63f76c36f03a2f9b20b07e693
057a82b0ee661d81a14a084691e9976a40b3642e
'2012-05-16T12:27:36-04:00'
describe
'3851314' 'info:fdaE20100110_AAACDPfileF20100110_AABOWH' 'sip-files00024.tif'
4f21050946d6da1cef461e7cd703e923
1a0b63ac4e2851f4c1b1b228255c43157ea88a3c
'2012-05-16T12:28:37-04:00'
describe
'1794' 'info:fdaE20100110_AAACDPfileF20100110_AABOWI' 'sip-files00024.txt'
a9d154fde35c1b4440c0582f924a505c
89ccb3c7fb5d9b5423b178246a225a7c103b39ea
describe
'42216' 'info:fdaE20100110_AAACDPfileF20100110_AABOWJ' 'sip-files00024thm.jpg'
40cb66e779f30e60bc5d15a33adaf11c
e1903952d177da48baa5c06277538764e92dabc6
describe
'486481' 'info:fdaE20100110_AAACDPfileF20100110_AABOWK' 'sip-files00025.jp2'
2a41058d5154e92677a638e2ad754aaa
cf4dd72b22ee5285960cf17fcb74acd5e4b451f1
'2012-05-16T12:25:15-04:00'
describe
'535963' 'info:fdaE20100110_AAACDPfileF20100110_AABOWL' 'sip-files00025.jpg'
61e2679bb8627292fb27dacd810eba65
539f22ec89831d132fd7de87a33ae9529b87ed2f
'2012-05-16T12:28:01-04:00'
describe
'61205' 'info:fdaE20100110_AAACDPfileF20100110_AABOWM' 'sip-files00025.pro'
598df832fb3fb98abd96720acbd77c29
2465fb823f00c151e13a3ee9eaf162fe4f6efaf7
'2012-05-16T12:20:14-04:00'
describe
'164874' 'info:fdaE20100110_AAACDPfileF20100110_AABOWN' 'sip-files00025.QC.jpg'
6973e89b9fe648fae7efb760e115d7f0
574ee21a0c31fb806724825fc8c4b8e67a5416ff
describe
'3894514' 'info:fdaE20100110_AAACDPfileF20100110_AABOWO' 'sip-files00025.tif'
acf4ed7808e9f14914722bb689de4c08
3f20895091c9666719a753033dbe1c18cb8130a0
'2012-05-16T12:25:02-04:00'
describe
'2471' 'info:fdaE20100110_AAACDPfileF20100110_AABOWP' 'sip-files00025.txt'
de0ccfb4d4c5cd507b39a62d60487a5d
97da58c51212681a7567d68c1b7add730f87a1f1
'2012-05-16T12:27:41-04:00'
describe
'48153' 'info:fdaE20100110_AAACDPfileF20100110_AABOWQ' 'sip-files00025thm.jpg'
97a0d26e65e7127ca0a8cd9673b2486e
13851634670f1d2080afecafa1ba0c9355ff1d92
'2012-05-16T12:28:20-04:00'
describe
'1993142' 'info:fdaE20100110_AAACDPfileF20100110_AABOWR' 'sip-files00026.jp2'
f35229ebe4e15d5674aa22015880bc9b
86dfe45e57356f230fe4930db2a3f2ece9157265
describe
'384985' 'info:fdaE20100110_AAACDPfileF20100110_AABOWS' 'sip-files00026.jpg'
98889609e67cdaa40bfd71166ffae123
af93cb8335e11ce18663c42102aa379f49db3e44
'2012-05-16T12:22:35-04:00'
describe
'5705' 'info:fdaE20100110_AAACDPfileF20100110_AABOWT' 'sip-files00026.pro'
86521713330c81b704fb8b7752fc3cd2
93f49f93a313ff6fb7af3b02ba5617333110d595
describe
'119602' 'info:fdaE20100110_AAACDPfileF20100110_AABOWU' 'sip-files00026.QC.jpg'
5c4883ccd2cad576d2f922f1864a0041
d760e8a6024799e91f01d070af96ef3fbd51affa
'2012-05-16T12:21:46-04:00'
describe
'15950314' 'info:fdaE20100110_AAACDPfileF20100110_AABOWV' 'sip-files00026.tif'
1e27c19677f04e1391883334196ec540
96d92301cfd0c35284971400049f0f74f2b5084e
'2012-05-16T12:23:57-04:00'
describe
'267' 'info:fdaE20100110_AAACDPfileF20100110_AABOWW' 'sip-files00026.txt'
cacf9b2412fd44b93e1854ed501ab8c2
57a031dfb47bdc1a825c0b4552537787434d636c
'2012-05-16T12:24:48-04:00'
describe
'39566' 'info:fdaE20100110_AAACDPfileF20100110_AABOWX' 'sip-files00026thm.jpg'
a992441a410d25edac87b673771e6ae1
9958aa18451854e853f0384c23f38b211b382cd5
'2012-05-16T12:26:29-04:00'
describe
'2024867' 'info:fdaE20100110_AAACDPfileF20100110_AABOWY' 'sip-files00027.jp2'
4ff5c7512019353d173585dc4ee894e2
4b6357f7ebc8b4a754811934593b9a9b57354711
'2012-05-16T12:25:17-04:00'
describe
'436034' 'info:fdaE20100110_AAACDPfileF20100110_AABOWZ' 'sip-files00027.jpg'
65bdf0c0757beb9d9ec2324eeece729f
84bcd7d3b24b43cba030b71e08c236f0258007dd
'2012-05-16T12:20:27-04:00'
describe
'13311' 'info:fdaE20100110_AAACDPfileF20100110_AABOXA' 'sip-files00027.pro'
83225e359ac44c2368703c58347d7bfd
a0561aa3dcb41b1fe4e1417f620b5f29f69eb8bc
'2012-05-16T12:27:17-04:00'
describe
'130341' 'info:fdaE20100110_AAACDPfileF20100110_AABOXB' 'sip-files00027.QC.jpg'
d2648f17dd158550fc6ca64bbda948f2
475295aaab52f9f546cfeac2d652486ebaabed18
'2012-05-16T12:22:56-04:00'
describe
'16204052' 'info:fdaE20100110_AAACDPfileF20100110_AABOXC' 'sip-files00027.tif'
c2dc27c4c00d73696babb158956818b3
c980db05321af3c8bb18223e0fa318e2d0097192
'2012-05-16T12:23:32-04:00'
describe
'615' 'info:fdaE20100110_AAACDPfileF20100110_AABOXD' 'sip-files00027.txt'
7c6ab890ae8e32bd72a78598fdd43c24
25e52d04b4e5fa322f6587ec2ca7731284a9f389
'2012-05-16T12:22:15-04:00'
describe
'40953' 'info:fdaE20100110_AAACDPfileF20100110_AABOXE' 'sip-files00027thm.jpg'
9995c6633dad08a1d7a9d9325cf39a04
64e920118e468eb6c3545a24e0e17e846c46571f
'2012-05-16T12:19:08-04:00'
describe
'2004699' 'info:fdaE20100110_AAACDPfileF20100110_AABOXF' 'sip-files00028.jp2'
1f85d1e8e304f5975919fe6ff1667b56
6688bed46ee76cf9dc87593cabd89229023798d8
'2012-05-16T12:19:46-04:00'
describe
'406947' 'info:fdaE20100110_AAACDPfileF20100110_AABOXG' 'sip-files00028.jpg'
4e6f7b77ba33cf872abffb3ff44c976b
fb9c0dd2e2b8b8122439e73786e2f4698effdf5b
'2012-05-16T12:20:04-04:00'
describe
'40497' 'info:fdaE20100110_AAACDPfileF20100110_AABOXH' 'sip-files00028.pro'
fe0c07dc8359b4e9411fa06e5fe26b60
c36dee888813e28a2f668b274a6c7c8e0c67c535
describe
'123735' 'info:fdaE20100110_AAACDPfileF20100110_AABOXI' 'sip-files00028.QC.jpg'
15a1bb275f3f82be77da223984e7e613
6884bc5d436a5c8074609c3bdae7ab5c3ea9f46f
'2012-05-16T12:19:42-04:00'
describe
'16042698' 'info:fdaE20100110_AAACDPfileF20100110_AABOXJ' 'sip-files00028.tif'
480ac63d229a64e2d2d97df20b6aed19
da2a239ff80a22c129c8e0d362cec4c9c0f8d44d
'2012-05-16T12:19:10-04:00'
describe
'2625' 'info:fdaE20100110_AAACDPfileF20100110_AABOXK' 'sip-files00028.txt'
f80064fb4fe93564884855d710861b71
2e738a9859772b597efdb2a7eba08059dddf97a7
'2012-05-16T12:22:43-04:00'
describe
'41142' 'info:fdaE20100110_AAACDPfileF20100110_AABOXL' 'sip-files00028thm.jpg'
eeec76091d9f500b66afc783bd503de1
f63d4e95e75de66bce40751a755da7ee40d656b2
'2012-05-16T12:27:25-04:00'
describe
'2006086' 'info:fdaE20100110_AAACDPfileF20100110_AABOXM' 'sip-files00029.jp2'
e8ff42da9922b84eb1fa37a33122e68c
e3a40a6e34592e3fa653ef966dd314fd06f23ac4
'2012-05-16T12:19:07-04:00'
describe
'375702' 'info:fdaE20100110_AAACDPfileF20100110_AABOXN' 'sip-files00029.jpg'
7ba09d396a7268f81e9405f44fdaf62c
a7909ee94986bbb7a3a68fff6b006af0aec63f98
'2012-05-16T12:27:42-04:00'
describe
'8978' 'info:fdaE20100110_AAACDPfileF20100110_AABOXO' 'sip-files00029.pro'
bfeeb0e89b5ade6d2cd967d28fbdff2a
14bec60e117a39164b9e8fc87b9836ca32027b65
'2012-05-16T12:18:16-04:00'
describe
'112258' 'info:fdaE20100110_AAACDPfileF20100110_AABOXP' 'sip-files00029.QC.jpg'
2959f68812143a88ac701330f7c6c037
ce442a39961c9f20d31deeefe1b4d5a389df7154
'2012-05-16T12:23:11-04:00'
describe
'16053788' 'info:fdaE20100110_AAACDPfileF20100110_AABOXQ' 'sip-files00029.tif'
927cd28215367c9d5d086713dd0c789e
273e058a19cab5129568b1e01a48b1f1ef840605
'2012-05-16T12:28:31-04:00'
describe
'456' 'info:fdaE20100110_AAACDPfileF20100110_AABOXR' 'sip-files00029.txt'
6762c62ff740b49e1daf13962969fe8b
ceab074c5a2af1b6afedead0862ce6dcd03b79f2
'2012-05-16T12:25:06-04:00'
describe
'37270' 'info:fdaE20100110_AAACDPfileF20100110_AABOXS' 'sip-files00029thm.jpg'
301ee3194b4f6a84517d2fd32b884ca0
b765867d9de1e47c2e79e7c82e8af703b608373c
'2012-05-16T12:25:24-04:00'
describe
'1985277' 'info:fdaE20100110_AAACDPfileF20100110_AABOXT' 'sip-files00030.jp2'
be8c4c2560c8bca6b8b5c896cfc64e2a
fe84c9c3fe92ffd57adf2d6a18ce4220196be5bf
'2012-05-16T12:19:53-04:00'
describe
'170817' 'info:fdaE20100110_AAACDPfileF20100110_AABOXU' 'sip-files00030.jpg'
874e40e4a506b6a89e0aaa89f93575d5
b8d034d42bc2c8c619d84d925a1f1f99c20bacb1
describe
'49814' 'info:fdaE20100110_AAACDPfileF20100110_AABOXV' 'sip-files00030.pro'
76eacf89a1a3c560a5130cc893fadad3
acc02a856622b513507bff299c9d2580c69a7592
'2012-05-16T12:18:48-04:00'
describe
'50583' 'info:fdaE20100110_AAACDPfileF20100110_AABOXW' 'sip-files00030.QC.jpg'
4c1c66fd83dd4d0190e9c4cb4a7bd950
fd8bc69c3e77134e706d02d3963a1080d10abe41
'2012-05-16T12:23:16-04:00'
describe
'15885746' 'info:fdaE20100110_AAACDPfileF20100110_AABOXX' 'sip-files00030.tif'
c0530f00774f0ef3f453219942986495
dd453576afb3aca7d2aa610bd548ce6e6751bf42
'2012-05-16T12:20:20-04:00'
describe
'2469' 'info:fdaE20100110_AAACDPfileF20100110_AABOXY' 'sip-files00030.txt'
95a3baab38c1a18b0a5454ceeb49ad16
300f66a3a6f604d014642a43e882d4bd75a7377e
'2012-05-16T12:27:32-04:00'
describe
'16877' 'info:fdaE20100110_AAACDPfileF20100110_AABOXZ' 'sip-files00030thm.jpg'
ed60222e9af0b013530bf49220570640
67ac74f52d0fd667609630f5353d1d849540e707
'2012-05-16T12:21:17-04:00'
describe
'1902556' 'info:fdaE20100110_AAACDPfileF20100110_AABOYA' 'sip-files00031.jp2'
d649604de8c869109b555819772be81a
670efef8f611583a3ce2016a3b9429c51e49bb93
'2012-05-16T12:25:10-04:00'
describe
'163247' 'info:fdaE20100110_AAACDPfileF20100110_AABOYB' 'sip-files00031.jpg'
d204e92487e2478c95d0a694c8519955
b06bc1fe08937025295b10df66be27e622b51f62
'2012-05-16T12:26:48-04:00'
describe
'43762' 'info:fdaE20100110_AAACDPfileF20100110_AABOYC' 'sip-files00031.pro'
464fcea089ea07d125e28fcd386e238d
881cbffdbee8784e9c1e5962aa853400ffbd4393
'2012-05-16T12:24:04-04:00'
describe
'48265' 'info:fdaE20100110_AAACDPfileF20100110_AABOYD' 'sip-files00031.QC.jpg'
b50e41156d38c675f88e192301c267f3
cbf82e961da96de991fbc0353498d5cc49f7ad09
describe
'15223570' 'info:fdaE20100110_AAACDPfileF20100110_AABOYE' 'sip-files00031.tif'
18139d403564d8695959f38e62acca70
e017f660c399857da1979792d8f490ec1d52e9af
'2012-05-16T12:26:53-04:00'
describe
'2189' 'info:fdaE20100110_AAACDPfileF20100110_AABOYF' 'sip-files00031.txt'
d3c63a4de317b64984345da2a7df68bb
69879b2971bf42e5f7ef019df5461f0c7b9692df
'2012-05-16T12:25:03-04:00'
describe
Invalid character
'15993' 'info:fdaE20100110_AAACDPfileF20100110_AABOYG' 'sip-files00031thm.jpg'
96c7562844d48df9981887dd42ae4cd6
de211d98c70e682c003908ae6a31989128f826dc
'2012-05-16T12:26:28-04:00'
describe
'476347' 'info:fdaE20100110_AAACDPfileF20100110_AABOYH' 'sip-files00032.jp2'
1a9b76d74e03a9c5685722bcf6948184
b09cfd363d355804c11a6c8d36d457db000e0d96
'2012-05-16T12:27:53-04:00'
describe
'569973' 'info:fdaE20100110_AAACDPfileF20100110_AABOYI' 'sip-files00032.jpg'
e3ba768365df523bd6834f5c1d090893
d545d55d600ad7efec6a6f8c7b19be06fb5344c3
'2012-05-16T12:23:01-04:00'
describe
'63879' 'info:fdaE20100110_AAACDPfileF20100110_AABOYJ' 'sip-files00032.pro'
4ce3f58bca083b1159d1076da9f33ed1
8ccba2fd9d28a7c2d3e374c1c98c505b47afba7f
'2012-05-16T12:19:04-04:00'
describe
'173366' 'info:fdaE20100110_AAACDPfileF20100110_AABOYK' 'sip-files00032.QC.jpg'
39a510ecfb7f0d052b2ee264d8bb7748
19426a1ed7e1aafdd51aebfc45eb38ef06633d8b
'2012-05-16T12:21:16-04:00'
describe
'3813298' 'info:fdaE20100110_AAACDPfileF20100110_AABOYL' 'sip-files00032.tif'
9a196047cf9b40946e1686d2250bc631
41a5d65179e8ea048132f81f04e9b9bbdba72411
'2012-05-16T12:24:01-04:00'
describe
'2621' 'info:fdaE20100110_AAACDPfileF20100110_AABOYM' 'sip-files00032.txt'
105bf67106070c528bdaf1bec5723001
11e7cd16d137c21e05dd1cacc0b07d00a07392c7
describe
'49967' 'info:fdaE20100110_AAACDPfileF20100110_AABOYN' 'sip-files00032thm.jpg'
ce376e8f27323120c4d43c15f33fca79
23d690a13b799dd9a3c4395d3793591608a1740d
'2012-05-16T12:25:39-04:00'
describe
'497341' 'info:fdaE20100110_AAACDPfileF20100110_AABOYO' 'sip-files00033.jp2'
464a6ed1c2ed5b880f3491e923a1da09
1da759e1f4ce25835cb4fad4d313738e2a39be92
'2012-05-16T12:24:38-04:00'
describe
'471891' 'info:fdaE20100110_AAACDPfileF20100110_AABOYP' 'sip-files00033.jpg'
ba546857b8e654909a0871bf1ffafe50
97747bb7ad416d79370702e8ce6e43f8ac7e86c0
'2012-05-16T12:26:35-04:00'
describe
'42789' 'info:fdaE20100110_AAACDPfileF20100110_AABOYQ' 'sip-files00033.pro'
bf761b586496ef83d64b2c2ac46e51d3
cfb3a34f2982563689d4882cc9d59472d530cb9a
'2012-05-16T12:25:55-04:00'
describe
'141081' 'info:fdaE20100110_AAACDPfileF20100110_AABOYR' 'sip-files00033.QC.jpg'
8e35986249765b7f9acf4e7cedc28615
e736a2c4ccaf5b1708730bcd2cd9a2d14035efb5
'2012-05-16T12:25:01-04:00'
describe
'3981306' 'info:fdaE20100110_AAACDPfileF20100110_AABOYS' 'sip-files00033.tif'
2e3fc4c431ccec8ce809cd0b21ed2324
898f099cb19a996fdadbfa74a15a33a9dc8be152
'2012-05-16T12:24:30-04:00'
describe
'1881' 'info:fdaE20100110_AAACDPfileF20100110_AABOYT' 'sip-files00033.txt'
5564887392d48492c209225ff827c21e
18204feeed0c0c7a4158edea17ad5bb30f735001
'2012-05-16T12:27:23-04:00'
describe
Invalid character
'40047' 'info:fdaE20100110_AAACDPfileF20100110_AABOYU' 'sip-files00033thm.jpg'
2572446cb3295a155fa903dfa9538606
0b76264c60ef2943e579ce9860251469d04c2f93
'2012-05-16T12:18:32-04:00'
describe
'499284' 'info:fdaE20100110_AAACDPfileF20100110_AABOYV' 'sip-files00034.jp2'
cbe994620a3e0cf94dbe76903a8947e3
531ee5c91d18bc51446c04a6a57fadd8fbc5e5f2
'2012-05-16T12:25:09-04:00'
describe
'539900' 'info:fdaE20100110_AAACDPfileF20100110_AABOYW' 'sip-files00034.jpg'
1ea6dee0dbafbf3bcfb6afe653c9e0eb
37b700169791977eba5f83c9ed04ebf2a92276d7
describe
'63248' 'info:fdaE20100110_AAACDPfileF20100110_AABOYX' 'sip-files00034.pro'
8935b5fc140190b70c476dc2ca0a136e
653ac98f738deb2f0d1ed6d21a54f4d874d56c95
describe
'170467' 'info:fdaE20100110_AAACDPfileF20100110_AABOYY' 'sip-files00034.QC.jpg'
2ebec4d8384773e2c5e233529fec4b82
724f888cbdbd3f2f3b2ffdfa8b5aaa09ad1d7d49
'2012-05-16T12:21:35-04:00'
describe
'3996914' 'info:fdaE20100110_AAACDPfileF20100110_AABOYZ' 'sip-files00034.tif'
12e5609394b46d13f25fb1809fea1e7b
9a7a928e9e29b7eb428ae37af4bc92dfccd40be6
'2012-05-16T12:26:26-04:00'
describe
'2546' 'info:fdaE20100110_AAACDPfileF20100110_AABOZA' 'sip-files00034.txt'
2bce06d67b5747faaf0d12879e5e7f7e
38a16475dd5a36108483e16a55ff397157e8e985
describe
'47065' 'info:fdaE20100110_AAACDPfileF20100110_AABOZB' 'sip-files00034thm.jpg'
764c43cb90017260a39ac805418a71df
eb77cc7d568b7b1f84022cc9b962b8ec3715153d
'2012-05-16T12:25:35-04:00'
describe
'490958' 'info:fdaE20100110_AAACDPfileF20100110_AABOZC' 'sip-files00035.jp2'
d276b634a601236feda1054dcb03568a
be96b93c2da03db6c6dca60d09006079484688d5
'2012-05-16T12:24:33-04:00'
describe
'493516' 'info:fdaE20100110_AAACDPfileF20100110_AABOZD' 'sip-files00035.jpg'
93254257745aa2e5fd12b31fae55ee5d
bb7318168c4efdfa81761c8e8c1cf1a55063135d
'2012-05-16T12:21:44-04:00'
describe
'56710' 'info:fdaE20100110_AAACDPfileF20100110_AABOZE' 'sip-files00035.pro'
bd2558d5e77053749dd1e70650f4f98b
def07dc4d5b2c60d57561f2c619d7130de6172fd
'2012-05-16T12:24:51-04:00'
describe
'153724' 'info:fdaE20100110_AAACDPfileF20100110_AABOZF' 'sip-files00035.QC.jpg'
a0a4d5ebc90025a1616b4afe1455b733
ee67c3a16f49eba13fe24f4d4590c1a19e8c109f
'2012-05-16T12:28:26-04:00'
describe
'3930206' 'info:fdaE20100110_AAACDPfileF20100110_AABOZG' 'sip-files00035.tif'
29a95fdb90e0e5683a3d638a4cceabcc
a055aea73d0b78f5227aa9fc5f90c893f3b2bf81
'2012-05-16T12:26:08-04:00'
describe
'2307' 'info:fdaE20100110_AAACDPfileF20100110_AABOZH' 'sip-files00035.txt'
c7290d42b72d8716cc72db35c6ef25d7
2f2bfe822704f2f65f6a3beb399854f733c42e29
'2012-05-16T12:28:38-04:00'
describe
'45810' 'info:fdaE20100110_AAACDPfileF20100110_AABOZI' 'sip-files00035thm.jpg'
66b5604ed95ebfbc71840220859c80db
f9df6ef78838b3280f642a2357ca8c04fcb95f56
describe
'504710' 'info:fdaE20100110_AAACDPfileF20100110_AABOZJ' 'sip-files00036.jp2'
4d956913e4e210c0275998dcca2bd062
be03ff5e6966717f637e6343a0614835cdfdf10b
describe
'457596' 'info:fdaE20100110_AAACDPfileF20100110_AABOZK' 'sip-files00036.jpg'
e9b6f5406cd4a1f0d534e1b0a1174726
da9bc4bcd44117db2ad9ac85b5e0f1ed49a6b744
describe
'47046' 'info:fdaE20100110_AAACDPfileF20100110_AABOZL' 'sip-files00036.pro'
b54d091a5531cb73775080fbb641e81d
13a9bf075bf389ef67e2e97c0e9ae8b7da682dbe
'2012-05-16T12:22:14-04:00'
describe
'144003' 'info:fdaE20100110_AAACDPfileF20100110_AABOZM' 'sip-files00036.QC.jpg'
bf1226e2d28ffbff08a14256d6a0bd2f
2cc4ce87952b68900abe8e11146963b039fce21e
'2012-05-16T12:25:31-04:00'
describe
'4040214' 'info:fdaE20100110_AAACDPfileF20100110_AABOZN' 'sip-files00036.tif'
b599eb5158b7f194b79ae6cd8682757c
75e4b9cb1290add7ea49890cdd96cf348d9465d9
'2012-05-16T12:19:28-04:00'
describe
'2081' 'info:fdaE20100110_AAACDPfileF20100110_AABOZO' 'sip-files00036.txt'
374f5addd86e084f391ffd24e8e689d0
c6b543c55c55c056b0d3ba5ba861ae56a9ad1cb2
'2012-05-16T12:27:10-04:00'
describe
'40294' 'info:fdaE20100110_AAACDPfileF20100110_AABOZP' 'sip-files00036thm.jpg'
4866a350de6ff5333f0faff2180db001
a4970f6131840e3025cc5b0588a762591e77cae5
'2012-05-16T12:24:52-04:00'
describe
'507414' 'info:fdaE20100110_AAACDPfileF20100110_AABOZQ' 'sip-files00037.jp2'
efe0cc7109deb8886c0b2bb859cc6943
7efb7c7d655eb73cb1d00fe884f5cb2fb1cb0654
'2012-05-16T12:20:38-04:00'
describe
'496413' 'info:fdaE20100110_AAACDPfileF20100110_AABOZR' 'sip-files00037.jpg'
ea8e511c9a699c973e17ab5b0afe9eda
a7bddd56db3d1b8ea99396a7fdd8cd62a4c98947
describe
'54948' 'info:fdaE20100110_AAACDPfileF20100110_AABOZS' 'sip-files00037.pro'
533fe9f39f5a7e06efb49854931bd4b2
e8032afe2e7e1fcc2cb8a0daaae3e4599260dd4e
describe
'152720' 'info:fdaE20100110_AAACDPfileF20100110_AABOZT' 'sip-files00037.QC.jpg'
053747d265bb692ac99cee458de46d52
7a0059208b338e269b5c3f6662bc03ebb7ad8935
'2012-05-16T12:27:40-04:00'
describe
'4061920' 'info:fdaE20100110_AAACDPfileF20100110_AABOZU' 'sip-files00037.tif'
68b4e74fa9a0606d2633a289473079de
fa85a135175bf16d4ad899102cd2244c2a3e28a9
'2012-05-16T12:27:24-04:00'
describe
'2257' 'info:fdaE20100110_AAACDPfileF20100110_AABOZV' 'sip-files00037.txt'
5044dbbd1ae8f3a364744487800c8916
914421c01aff247394791b5426230e99a6530f92
'2012-05-16T12:27:37-04:00'
describe
'45658' 'info:fdaE20100110_AAACDPfileF20100110_AABOZW' 'sip-files00037thm.jpg'
6e569230d5d49448cb83c9c7fc4ae096
8a00f480078c0c38c2e425b1fd090eb6c0d6ad7e
'2012-05-16T12:27:48-04:00'
describe
'495015' 'info:fdaE20100110_AAACDPfileF20100110_AABOZX' 'sip-files00038.jp2'
fa07fb167c707805c13147c336f5b949
b0fc8a0da7ecaf6a83bdc6af5f82a11ae6139f97
'2012-05-16T12:21:32-04:00'
describe
'490570' 'info:fdaE20100110_AAACDPfileF20100110_AABOZY' 'sip-files00038.jpg'
9aad10098f7f4112373acdb80739c88d
d11687baad5505b7fb7d46b7f5c4b08076ef0186
'2012-05-16T12:19:17-04:00'
describe
'52925' 'info:fdaE20100110_AAACDPfileF20100110_AABOZZ' 'sip-files00038.pro'
f63cef4fe716e7bd03b84711a9615ae5
38951a107ba637e5a6642d9b8b6a8dde0e88e2e1
describe
'156743' 'info:fdaE20100110_AAACDPfileF20100110_AABPAA' 'sip-files00038.QC.jpg'
0722f02a5ac44a425b04f168b8459484
cb8b07a961c5a9ff854c5418a998df18f16fb266
describe
'3962740' 'info:fdaE20100110_AAACDPfileF20100110_AABPAB' 'sip-files00038.tif'
ad24b54969a49c5b223564e208e87b80
2c6c9431a5c9127e9479794f5233db08780bc8af
describe
'2222' 'info:fdaE20100110_AAACDPfileF20100110_AABPAC' 'sip-files00038.txt'
92346f4bc0bfdac97b904853dad4a5ac
dd8f04ddeca3b3043b63ed67d26a5128aab03a36
'2012-05-16T12:20:45-04:00'
describe
'42752' 'info:fdaE20100110_AAACDPfileF20100110_AABPAD' 'sip-files00038thm.jpg'
52db42aa674e1d2c749c28ead3cd80f8
0549e5ff85007aa5227649d35d2b7bfa7c057cba
describe
'2002716' 'info:fdaE20100110_AAACDPfileF20100110_AABPAE' 'sip-files00039.jp2'
2811f19a1f13ee7877ba93b5f9d92e4e
a114b1ee62305c6eecc9d0daed698bec5424fe8b
'2012-05-16T12:20:26-04:00'
describe
'610448' 'info:fdaE20100110_AAACDPfileF20100110_AABPAF' 'sip-files00039.jpg'
f174f39460b42a291ce59672db84c0cd
4d8a13c020df343c4a05a46195201c90ebc31ce7
'2012-05-16T12:24:57-04:00'
describe
'36786' 'info:fdaE20100110_AAACDPfileF20100110_AABPAG' 'sip-files00039.pro'
fa1b186394542f5fc5e5e6847ae74ea0
5b8f8ad1fe1450b8f89f4315cac48f52d7aa5dc8
'2012-05-16T12:19:19-04:00'
describe
'171410' 'info:fdaE20100110_AAACDPfileF20100110_AABPAH' 'sip-files00039.QC.jpg'
7ef4f7663bd44b1decb85611252ce403
77eff600cec70e16abe66fa68b9fca271d74c4b0
'2012-05-16T12:25:57-04:00'
describe
'16026880' 'info:fdaE20100110_AAACDPfileF20100110_AABPAI' 'sip-files00039.tif'
10ab207b4e416c5e7f995b32bb35d24d
1ed0d0ea1bf10f0e433b5170c35a432670d326ff
'2012-05-16T12:25:49-04:00'
describe
'1470' 'info:fdaE20100110_AAACDPfileF20100110_AABPAJ' 'sip-files00039.txt'
eb8cfe66ebcb076fd3945cfa62486985
5c272039747c3b2919a1b53b09ee3ab3eb4ffefc
'2012-05-16T12:25:20-04:00'
describe
'49596' 'info:fdaE20100110_AAACDPfileF20100110_AABPAK' 'sip-files00039thm.jpg'
d39b4b534e5536d1bd301ef750769077
740adea74dcb4eeb326c8290e0019c4695e58cf6
describe
'1898292' 'info:fdaE20100110_AAACDPfileF20100110_AABPAL' 'sip-files00040.jp2'
03bd1a383bcd749f87bf166fea4b3f6a
7699e04136f77d382430b803a622c6fb9366fba2
'2012-05-16T12:21:06-04:00'
describe
'615717' 'info:fdaE20100110_AAACDPfileF20100110_AABPAM' 'sip-files00040.jpg'
ad5b67656e48443409c7d9a93383525e
c93d3427ee1fd4b9ea09d9e33a9d5ae67414a2e5
'2012-05-16T12:21:53-04:00'
describe
'34647' 'info:fdaE20100110_AAACDPfileF20100110_AABPAN' 'sip-files00040.pro'
753995296dae67f4b7a8fa9e47181382
a9b5d292ea5c880a0829d3610f32001e557f89d8
'2012-05-16T12:27:55-04:00'
describe
'176445' 'info:fdaE20100110_AAACDPfileF20100110_AABPAO' 'sip-files00040.QC.jpg'
13faf43919e2d3b47f11c836a227fcf6
de53bb9a1d80161774a6621d3c1e08635da14c08
'2012-05-16T12:24:41-04:00'
describe
'15191626' 'info:fdaE20100110_AAACDPfileF20100110_AABPAP' 'sip-files00040.tif'
d3c39b2a756a8acf4c7602f89ba7bd11
6d342e0d2924b5415414820feb7ea59483208b37
'2012-05-16T12:27:39-04:00'
describe
'1399' 'info:fdaE20100110_AAACDPfileF20100110_AABPAQ' 'sip-files00040.txt'
43de8413afd7474c49f7f78cc4bb6c2b
7f7ed9ed7ad9075e1c584f0e8ea7566b331287f7
'2012-05-16T12:23:36-04:00'
describe
'53950' 'info:fdaE20100110_AAACDPfileF20100110_AABPAR' 'sip-files00040thm.jpg'
0323d30001bb88e793d9b76842f59750
afc01af91b15fb4aadc2db108b28ec460dae363b
'2012-05-16T12:24:17-04:00'
describe
'2098042' 'info:fdaE20100110_AAACDPfileF20100110_AABPAS' 'sip-files00041.jp2'
d6962ebf9616c75728d1a66e3a3c3497
53a8d339dad9c944f20ed7ba38fb0a64246b60df
'2012-05-16T12:21:25-04:00'
describe
'232713' 'info:fdaE20100110_AAACDPfileF20100110_AABPAT' 'sip-files00041.jpg'
7809877f6731d96de212f599b27717cc
c9cdcbfa7522b88ab1bca6db97012cb33d16cd4a
'2012-05-16T12:25:48-04:00'
describe
'62980' 'info:fdaE20100110_AAACDPfileF20100110_AABPAU' 'sip-files00041.pro'
407c37cf1ac132eae6e526f9afe0c260
5dd42bde3d4b41a74ac9428b5ae0e7060ae205be
'2012-05-16T12:28:19-04:00'
describe
'69995' 'info:fdaE20100110_AAACDPfileF20100110_AABPAV' 'sip-files00041.QC.jpg'
eb554794d384567725f3e2335c76a6b1
ad1683f8e0b29a5a791d32f84913044ede75c13d
describe
'16787506' 'info:fdaE20100110_AAACDPfileF20100110_AABPAW' 'sip-files00041.tif'
a60c3e8ce0f1d89201519a73c80c99a1
9e636292b377855c6e7006657678f32888c1438d
'2012-05-16T12:24:07-04:00'
describe
'3157' 'info:fdaE20100110_AAACDPfileF20100110_AABPAX' 'sip-files00041.txt'
9835e20daec1462b862e2ab7addc4d3f
7f0b540d61bd99dae254300a80570ff321f9b645
describe
'21390' 'info:fdaE20100110_AAACDPfileF20100110_AABPAY' 'sip-files00041thm.jpg'
1b1f5453b71e04fd44f9ec0252d45ad9
65dd9023c2619abf37ec12a7355d818b5d2dd978
describe
'1973671' 'info:fdaE20100110_AAACDPfileF20100110_AABPAZ' 'sip-files00042.jp2'
7c58a305f731a0d2282bde19aaef0a47
d7c3d1f361a87f19e981ed56afdd15669a2de3b3
'2012-05-16T12:19:22-04:00'
describe
'592434' 'info:fdaE20100110_AAACDPfileF20100110_AABPBA' 'sip-files00042.jpg'
06665ca171b886e250a33bbcb34ea3d3
b2ab69f90fb24caeea292080a0ab9e63ce8233ee
'2012-05-16T12:19:30-04:00'
describe
'28852' 'info:fdaE20100110_AAACDPfileF20100110_AABPBB' 'sip-files00042.pro'
a0c1dca732b5f0b16ae8910aec63d416
7d05b3d72e43a329349c15ff58e9dc8aa900423a
describe
'166273' 'info:fdaE20100110_AAACDPfileF20100110_AABPBC' 'sip-files00042.QC.jpg'
20c33755ef04b686a9685936416b0389
17cec0211933ccfe86b9b2879b6bb2019388d5c2
'2012-05-16T12:21:11-04:00'
describe
'15794856' 'info:fdaE20100110_AAACDPfileF20100110_AABPBD' 'sip-files00042.tif'
bd877aea0cda837fa449c9dfb5a908f0
67028117f1ffe5bb3d07297963d3726144171485
'2012-05-16T12:19:47-04:00'
describe
'1164' 'info:fdaE20100110_AAACDPfileF20100110_AABPBE' 'sip-files00042.txt'
39afe4b7745382e95766130323768061
2d8de2e31b2f840ff057d0d52b41c4dc7e9aa7aa
'2012-05-16T12:24:20-04:00'
describe
'51779' 'info:fdaE20100110_AAACDPfileF20100110_AABPBF' 'sip-files00042thm.jpg'
3bba2e27503708ff48ba6a4f446e2832
953148bbf178d532281c10e4d8fe2fc11cd274b9
'2012-05-16T12:22:31-04:00'
describe
'2003939' 'info:fdaE20100110_AAACDPfileF20100110_AABPBG' 'sip-files00043.jp2'
0239c986a8192896f52a00fed47d7af4
586d59a5466a5c26f6f1a4cc8c04ea36ed6d0879
'2012-05-16T12:24:35-04:00'
describe
'563624' 'info:fdaE20100110_AAACDPfileF20100110_AABPBH' 'sip-files00043.jpg'
80a8ca6a1d3772226c006c81f17c46f3
19bbf96819a3aa86256ffb1873e9f5f8dbfed6db
'2012-05-16T12:22:57-04:00'
describe
'23293' 'info:fdaE20100110_AAACDPfileF20100110_AABPBI' 'sip-files00043.pro'
3faf9ab3e1b8f68658b08d4f5f18a04a
f28fb7c4ab08b5f4498f2604171bce0cfb1ce24d
'2012-05-16T12:19:44-04:00'
describe
'158235' 'info:fdaE20100110_AAACDPfileF20100110_AABPBJ' 'sip-files00043.QC.jpg'
d87a976a4ecb9ccd025f68b296175bd7
b89d561ab8277d491f5e7fd3590d3cc413d769df
describe
'16036778' 'info:fdaE20100110_AAACDPfileF20100110_AABPBK' 'sip-files00043.tif'
b2152687817912d5819dff8be4a7c6e5
9c345877c46bf7f448afcbba8a2e913375d18838
describe
'946' 'info:fdaE20100110_AAACDPfileF20100110_AABPBL' 'sip-files00043.txt'
ffec3e79508dc2efa87c89ee48c1bbf4
02dc8131d87b0e5fe5f4ef3ba9f768624892762e
'2012-05-16T12:23:54-04:00'
describe
'48328' 'info:fdaE20100110_AAACDPfileF20100110_AABPBM' 'sip-files00043thm.jpg'
807991ca1600adcf8bb6916931e6c287
f62b93173d38ee2ed773629e4123301e925d06f0
'2012-05-16T12:25:41-04:00'
describe
'1958880' 'info:fdaE20100110_AAACDPfileF20100110_AABPBN' 'sip-files00044.jp2'
b4115bfb39089be30fa811b2eab2800b
65d2ec645057524b26f033c740b2a9255fd97790
'2012-05-16T12:24:43-04:00'
describe
'505436' 'info:fdaE20100110_AAACDPfileF20100110_AABPBO' 'sip-files00044.jpg'
4c645b7838880db019457775478284ae
7b547396f3ea518c79439edbbdfb7f81f619ad18
'2012-05-16T12:24:09-04:00'
describe
'15045' 'info:fdaE20100110_AAACDPfileF20100110_AABPBP' 'sip-files00044.pro'
a428868f364e4275c2996c052700bd34
95c66dde397f785f06927244824243fc9a222c19
'2012-05-16T12:25:51-04:00'
describe
'138362' 'info:fdaE20100110_AAACDPfileF20100110_AABPBQ' 'sip-files00044.QC.jpg'
f883672e59b5ece18aa54b8432455461
c47d56bd99727561ef8c8c8bb3d059dfab09c77c
'2012-05-16T12:19:45-04:00'
describe
'15676142' 'info:fdaE20100110_AAACDPfileF20100110_AABPBR' 'sip-files00044.tif'
51eacb409183d5a0be70f7569f9e78a4
67aab4749b116267192f0f6f42eaefef5a5afc40
'2012-05-16T12:19:21-04:00'
describe
'713' 'info:fdaE20100110_AAACDPfileF20100110_AABPBS' 'sip-files00044.txt'
45fc62abc4ae453e0b86fecfcd9e6cf8
26e4acfb64f3c8cf63cf0f7a338b4d3f79033039
'2012-05-16T12:27:43-04:00'
describe
'44552' 'info:fdaE20100110_AAACDPfileF20100110_AABPBT' 'sip-files00044thm.jpg'
4497a8c3ad3a7c7f046caec15bf0216c
610a9466fb1f6e82be3b46d98654d4a96f0e1657
'2012-05-16T12:20:19-04:00'
describe
'2013270' 'info:fdaE20100110_AAACDPfileF20100110_AABPBU' 'sip-files00045.jp2'
5d2e2e3dff085cfbe8527ab536909b08
2adf1d6f91bc17367f39a707c56dd65995861004
'2012-05-16T12:27:03-04:00'
describe
'502343' 'info:fdaE20100110_AAACDPfileF20100110_AABPBV' 'sip-files00045.jpg'
ef1750b170968adfae57fa43b460db3a
eff738d174215b156d877a667716d64cc2a82c98
describe
'50115' 'info:fdaE20100110_AAACDPfileF20100110_AABPBW' 'sip-files00045.pro'
716236e6612c458fa6af1efc0867e3d0
03865173c5c223be1588161063127927608fdd14
'2012-05-16T12:23:43-04:00'
describe
'153617' 'info:fdaE20100110_AAACDPfileF20100110_AABPBX' 'sip-files00045.QC.jpg'
5716cbd552404ce8255e0dc9af06d79f
073f2bec3661719c4269aa0ea3b1c48647e3e126
'2012-05-16T12:24:23-04:00'
describe
'16111354' 'info:fdaE20100110_AAACDPfileF20100110_AABPBY' 'sip-files00045.tif'
045733175461bfd2899cab44170f2bb4
3c1087bdd691066d132ccedc857b938dc295b18a
'2012-05-16T12:18:22-04:00'
describe
'2124' 'info:fdaE20100110_AAACDPfileF20100110_AABPBZ' 'sip-files00045.txt'
b7f1c8c50c1d44c696a4de26b5bc9ad2
5016fa63cd017f6aea00270030e8669b565aedc8
'2012-05-16T12:18:53-04:00'
describe
'47822' 'info:fdaE20100110_AAACDPfileF20100110_AABPCA' 'sip-files00045thm.jpg'
447513cf1ff7095879dac7eee407a091
8608a3c6e59c33595e0d124b98c9c42713fda661
'2012-05-16T12:26:10-04:00'
describe
'490848' 'info:fdaE20100110_AAACDPfileF20100110_AABPCB' 'sip-files00046.jp2'
24d8fbd04f67c8a637ba92ed837ee21f
0b385e232b806a78ed469b625b598139636cb145
describe
'508509' 'info:fdaE20100110_AAACDPfileF20100110_AABPCC' 'sip-files00046.jpg'
9ce9515c539e5fdcdbe7a7677f98f72e
b2105d5ca899a0890e20409635446b29d7352deb
'2012-05-16T12:27:31-04:00'
describe
'49974' 'info:fdaE20100110_AAACDPfileF20100110_AABPCD' 'sip-files00046.pro'
238428ee6f932a71a07236bbeb848ba1
8557b3b60404bb5fd5a4504cf68d6d96841aecfc
'2012-05-16T12:26:17-04:00'
describe
'154890' 'info:fdaE20100110_AAACDPfileF20100110_AABPCE' 'sip-files00046.QC.jpg'
f4aec5a8235add0b64bf0b9014058441
71dbf40c2e13ce24162235bd7d84fff9fdaf60a0
'2012-05-16T12:26:54-04:00'
describe
'3929330' 'info:fdaE20100110_AAACDPfileF20100110_AABPCF' 'sip-files00046.tif'
feaf88b199d01db76a2ce4c12d8cd04c
177a5de0aaa2e6567ac8d09e25e2a67fa640d65e
describe
'2107' 'info:fdaE20100110_AAACDPfileF20100110_AABPCG' 'sip-files00046.txt'
c4f3ecf7c24e1bbee2ec413b931b7685
ccbd29c4afc9ec142c121562e710ba62ad7d22cc
describe
'45286' 'info:fdaE20100110_AAACDPfileF20100110_AABPCH' 'sip-files00046thm.jpg'
1e660d4191677cb00f42fb3accc1a74a
744d34b37b1bfa0fda437886326c011c0cc6ab3b
describe
'502513' 'info:fdaE20100110_AAACDPfileF20100110_AABPCI' 'sip-files00047.jp2'
b3883ecc5a5c8cde364e8afe115f4c53
9c405926a92027f7c09e8fe2690e142c4d157a62
'2012-05-16T12:24:16-04:00'
describe
'581670' 'info:fdaE20100110_AAACDPfileF20100110_AABPCJ' 'sip-files00047.jpg'
162782bf1b52dfd51cc2e2d1f057e794
438cec7e8c04fe93eadf5795d6ccc1eb9d26b499
'2012-05-16T12:19:26-04:00'
describe
'64714' 'info:fdaE20100110_AAACDPfileF20100110_AABPCK' 'sip-files00047.pro'
0036b0350a1109599bf4f913a98b7929
a08a1040c417e5e0fc3f77c0751a76b9fcfdd4e4
describe
'174723' 'info:fdaE20100110_AAACDPfileF20100110_AABPCL' 'sip-files00047.QC.jpg'
d7533b5d401adaeaf627ed47f7f67b37
642e37c13bd201605163071130dc2be9a5e9074e
'2012-05-16T12:20:47-04:00'
describe
'4023022' 'info:fdaE20100110_AAACDPfileF20100110_AABPCM' 'sip-files00047.tif'
2b4c87c96a09a656b9bb046d36d546da
2f286151f08fa253c7f28703321249880defe678
'2012-05-16T12:25:21-04:00'
describe
'2548' 'info:fdaE20100110_AAACDPfileF20100110_AABPCN' 'sip-files00047.txt'
f0b84c1da00f84617d5657c7815e9395
358376ede8ec4e9ce96cf62cc83ea4307704bcc0
describe
'48550' 'info:fdaE20100110_AAACDPfileF20100110_AABPCO' 'sip-files00047thm.jpg'
9c46512fdefba4046312d58187c0ca4f
89f26ed463e1d54abf47116ba38b1afaee6cbf24
'2012-05-16T12:21:10-04:00'
describe
'496104' 'info:fdaE20100110_AAACDPfileF20100110_AABPCP' 'sip-files00048.jp2'
bac74ae968c2e17d5fdbb76cc1d27758
cfaea2b6cd7128a285eef0fc5919f837118c5db3
'2012-05-16T12:22:38-04:00'
describe
'462985' 'info:fdaE20100110_AAACDPfileF20100110_AABPCQ' 'sip-files00048.jpg'
466c390a936e9cc557ce2e3b5a960c04
56af2b1a9cabf77cbcb2f6f86f622f22affaca26
'2012-05-16T12:23:42-04:00'
describe
'46990' 'info:fdaE20100110_AAACDPfileF20100110_AABPCR' 'sip-files00048.pro'
74e8e09d5f6b8fdcb6ba1498705a783f
ef0d9683700586c36f24c17ab6c8c2c06df36435
'2012-05-16T12:19:05-04:00'
describe
'141014' 'info:fdaE20100110_AAACDPfileF20100110_AABPCS' 'sip-files00048.QC.jpg'
88b0c4270086661b949d8eb47cd5e24f
729d9a17444325a962b7f1b6dc54dbfa62504dad
'2012-05-16T12:20:15-04:00'
describe
'3971322' 'info:fdaE20100110_AAACDPfileF20100110_AABPCT' 'sip-files00048.tif'
7af4c0fa0321c587e1843dfabb1624bd
781bfe827338ae143a2d5720b83695ec753d1e72
'2012-05-16T12:23:15-04:00'
describe
'1899' 'info:fdaE20100110_AAACDPfileF20100110_AABPCU' 'sip-files00048.txt'
fa7825909597ca5dfc06a1e5cec2f0a3
3990176359de2def8f419c89854585681ebdc0af
'2012-05-16T12:23:21-04:00'
describe
'43354' 'info:fdaE20100110_AAACDPfileF20100110_AABPCV' 'sip-files00048thm.jpg'
f640ca0e5bcde33edf70455d262e7f87
7f9f7067e8daf5d557527abfb8914c5dcffbf9bd
'2012-05-16T12:24:26-04:00'
describe
'503161' 'info:fdaE20100110_AAACDPfileF20100110_AABPCW' 'sip-files00049.jp2'
f1451f9f786984583780260242696ff4
7b834348df3c344623c45d329830f6a380412882
'2012-05-16T12:23:22-04:00'
describe
'378271' 'info:fdaE20100110_AAACDPfileF20100110_AABPCX' 'sip-files00049.jpg'
35814b244d025b401fa0b5ec2fb98520
735785c0074eb38a159f167dff4798491b6e47ee
'2012-05-16T12:20:39-04:00'
describe
'48475' 'info:fdaE20100110_AAACDPfileF20100110_AABPCY' 'sip-files00049.pro'
3d0a9017b514656dcb70b35253041bd9
c0b07a9e958b05facabb52679967611657365cd5
'2012-05-16T12:22:30-04:00'
describe
'123011' 'info:fdaE20100110_AAACDPfileF20100110_AABPCZ' 'sip-files00049.QC.jpg'
673dd6780684342baaede74a54f29c3f
e9fe949eada5a244854eab0de87621cd6fc910f1
describe
'4028088' 'info:fdaE20100110_AAACDPfileF20100110_AABPDA' 'sip-files00049.tif'
32cf6056ca77a6d6084d17984e895e94
c8d7ae45642ce5027ab486911c281a39e834237e
describe
'2133' 'info:fdaE20100110_AAACDPfileF20100110_AABPDB' 'sip-files00049.txt'
d00848148e15360577e0456ad5989aa8
6d4e8a9c8775614f8095352688e321c18c9a5f60
'2012-05-16T12:22:49-04:00'
describe
'38695' 'info:fdaE20100110_AAACDPfileF20100110_AABPDC' 'sip-files00049thm.jpg'
9ab2848bd729fb1b388f72cec6df8b95
3d24ff5adcccdcdcc1f6e4a27c376fe0a8fa4c39
'2012-05-16T12:27:54-04:00'
describe
'458891' 'info:fdaE20100110_AAACDPfileF20100110_AABPDD' 'sip-files00050.jp2'
4a0031555b055be4faa9b65d02470ab2
84bd6611862b29200e1a9f86a1294c73bc3fdfc4
describe
'547089' 'info:fdaE20100110_AAACDPfileF20100110_AABPDE' 'sip-files00050.jpg'
ac379ea393a8d97d42f31c44ac3f37e3
52ce56824286a3d4e454b158cbd58cf7944e6a73
'2012-05-16T12:28:40-04:00'
describe
'55874' 'info:fdaE20100110_AAACDPfileF20100110_AABPDF' 'sip-files00050.pro'
34605e4a67fd6b7e5a425b24ca1b3fd7
bf2aeb5292665eb1f2ebf8695b6fedeea23bfb7c
describe
'170279' 'info:fdaE20100110_AAACDPfileF20100110_AABPDG' 'sip-files00050.QC.jpg'
f763cd242d6e47b587b621385f549c24
321b6dca3cc40d37929a0d4b4763c258c448552b
'2012-05-16T12:28:12-04:00'
describe
'3673634' 'info:fdaE20100110_AAACDPfileF20100110_AABPDH' 'sip-files00050.tif'
975674cdf4d5fd075ccee49f0f5b3ef0
1f35e923dc82e7a90990d6ce0ad2169d3025f26d
'2012-05-16T12:22:39-04:00'
describe
'2277' 'info:fdaE20100110_AAACDPfileF20100110_AABPDI' 'sip-files00050.txt'
4cfe7c06cbf67cd92abd561386f92bc5
7898eebff177f3ba06ff296f335396a2aa8cc11a
'2012-05-16T12:24:25-04:00'
describe
'49290' 'info:fdaE20100110_AAACDPfileF20100110_AABPDJ' 'sip-files00050thm.jpg'
7ae2a307121dfc61bf70ddbf7f214249
e1b95db758d824464a9df65b2846677e1f7d3e20
describe
'454840' 'info:fdaE20100110_AAACDPfileF20100110_AABPDK' 'sip-files00051.jp2'
8be100e7431f0c209890918ad5b87380
2418d7e6dedf479e50835fd8883410cb36e59eef
'2012-05-16T12:21:04-04:00'
describe
'521422' 'info:fdaE20100110_AAACDPfileF20100110_AABPDL' 'sip-files00051.jpg'
808a89a732c1a00a985e6b5fc5b14a51
324bad2be7fdd28af5a670e3ed70b8f84ac24982
'2012-05-16T12:27:58-04:00'
describe
'55709' 'info:fdaE20100110_AAACDPfileF20100110_AABPDM' 'sip-files00051.pro'
618a34cee8e5602fbf909d40093e7fbf
f23dfd0773dd3cf312dedd9855bff553191f3498
'2012-05-16T12:28:02-04:00'
describe
'165862' 'info:fdaE20100110_AAACDPfileF20100110_AABPDN' 'sip-files00051.QC.jpg'
0d8a5a49bd254d0dcc7ea7b4317b5f8e
55c521c60dcc31c35f86601781055e09f769cd50
'2012-05-16T12:19:16-04:00'
describe
'3642458' 'info:fdaE20100110_AAACDPfileF20100110_AABPDO' 'sip-files00051.tif'
f0fe70d87aec1652d24725ed6b5302f6
82195bf6343fb76bdc8a1233d59e338937221dbd
'2012-05-16T12:25:43-04:00'
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPDP' 'sip-files00051.txt'
8b80be2f039965a265b8a5b025709fa1
9452b633703e75a9c1915a4e0895516d6c4bde0b
'2012-05-16T12:26:12-04:00'
describe
'45479' 'info:fdaE20100110_AAACDPfileF20100110_AABPDQ' 'sip-files00051thm.jpg'
9bb6e60db198e2e7dfe84f649eeec523
7e713aa51a6e61de5d63313fd7b62b74e50443b2
'2012-05-16T12:27:29-04:00'
describe
'458601' 'info:fdaE20100110_AAACDPfileF20100110_AABPDR' 'sip-files00052.jp2'
7119871d6fd50c84c160b4e5bd3b53d8
0b931297b35a000a76e162e320bdc9958aeb4051
describe
'457962' 'info:fdaE20100110_AAACDPfileF20100110_AABPDS' 'sip-files00052.jpg'
a00d056c3d0b6dc6730aee9788ef2625
217dac204704ebe8a039729e60d41b67487790ad
describe
'44740' 'info:fdaE20100110_AAACDPfileF20100110_AABPDT' 'sip-files00052.pro'
bb1aa40ae413c5f7e6f92c535c25734f
7fdf828ecde27540f6a7cc2df576dbf13e177a00
describe
'143953' 'info:fdaE20100110_AAACDPfileF20100110_AABPDU' 'sip-files00052.QC.jpg'
f4bdb36a9b1cefc0edb869fb39d07201
e38a8c1bd3c66152b727859ef322fdc525bef014
describe
'3671176' 'info:fdaE20100110_AAACDPfileF20100110_AABPDV' 'sip-files00052.tif'
6da188092fd6ef4c71a9afeab9c6cf62
115004e0c9b1aa3ecce64c8cb353ed15050f52f5
'2012-05-16T12:26:13-04:00'
describe
'2019' 'info:fdaE20100110_AAACDPfileF20100110_AABPDW' 'sip-files00052.txt'
ed58bd0cf9a60d6b5883abf67ec64b4e
8afefbcedd88dd3e14e76f20d0f896b5226bc213
'2012-05-16T12:24:54-04:00'
describe
'42624' 'info:fdaE20100110_AAACDPfileF20100110_AABPDX' 'sip-files00052thm.jpg'
6cd547c9a67e7ea5593e88f9dd0e1794
219d0a83ea1ce24e4fe05ec37849b175124ed608
describe
'479811' 'info:fdaE20100110_AAACDPfileF20100110_AABPDY' 'sip-files00053.jp2'
a83d60321cbfcc310c3491967d9a4b6f
85ad050d50c642567e2a9b19e8c77ca9936fe68d
'2012-05-16T12:20:10-04:00'
describe
'543235' 'info:fdaE20100110_AAACDPfileF20100110_AABPDZ' 'sip-files00053.jpg'
f3a231fd19ab3382fdf54cf19dc8b48e
56c2e5a698d100a13c550e161346bbb298bd1d86
'2012-05-16T12:20:07-04:00'
describe
'57105' 'info:fdaE20100110_AAACDPfileF20100110_AABPEA' 'sip-files00053.pro'
1515275dea306262fca5c9d964bcdd6d
bc8631c26ad56172cc9ea23cadff8a5ed2a5e53f
'2012-05-16T12:19:58-04:00'
describe
'167950' 'info:fdaE20100110_AAACDPfileF20100110_AABPEB' 'sip-files00053.QC.jpg'
eab38fc35c9e12ecce6f1d02a8f48a85
06251991b8bf2c813e0b82677165758c0d224285
'2012-05-16T12:25:46-04:00'
describe
'3841282' 'info:fdaE20100110_AAACDPfileF20100110_AABPEC' 'sip-files00053.tif'
2b4326c19ca5a979b6d03872e642942b
119068174a7d3ebf8ec81e4784e557277134e13e
'2012-05-16T12:25:26-04:00'
describe
'2324' 'info:fdaE20100110_AAACDPfileF20100110_AABPED' 'sip-files00053.txt'
e3019f4c47c17c234cf18add08754bcf
35a934b4908a1718011632bc9a5dc01802dafd58
'2012-05-16T12:20:40-04:00'
describe
'49461' 'info:fdaE20100110_AAACDPfileF20100110_AABPEE' 'sip-files00053thm.jpg'
a52ad77a2f57b1059b01038703a037ae
03a73d56fe80faa3f3d3583a7a8cc0fa4724625e
'2012-05-16T12:24:40-04:00'
describe
'455184' 'info:fdaE20100110_AAACDPfileF20100110_AABPEF' 'sip-files00054.jp2'
c639cb35c0205d55ba60c8c294494baf
55d792f3b87c35b03f41e18c67592efa91afc1ca
describe
'587100' 'info:fdaE20100110_AAACDPfileF20100110_AABPEG' 'sip-files00054.jpg'
6b3f21a2520149875dc68a67873a7916
d7e392df8b936192cec633ffd65d92d8c2fb58cf
'2012-05-16T12:19:11-04:00'
describe
'66457' 'info:fdaE20100110_AAACDPfileF20100110_AABPEH' 'sip-files00054.pro'
1c73fdcc63c01c19eb3f3fedf856d01d
d11f9f7a13d136e0f3568727589e4c262fb5287b
describe
'184872' 'info:fdaE20100110_AAACDPfileF20100110_AABPEI' 'sip-files00054.QC.jpg'
83a7561acf8963fd6f87957c0cadc358
ec7f51c3b886c0ff024e171e4b7908a33d5b786d
'2012-05-16T12:26:20-04:00'
describe
'3644018' 'info:fdaE20100110_AAACDPfileF20100110_AABPEJ' 'sip-files00054.tif'
02f88b800cbf54f124bedadb5dbefd7b
532a756f4ddf658b2d31679d1957b8e4b5e8b297
describe
'2626' 'info:fdaE20100110_AAACDPfileF20100110_AABPEK' 'sip-files00054.txt'
8ce9c71b50edcc4ae5b9a037ae4d150c
ff0741817c71027d47893f6064b6f0abd0fd99b9
describe
'52686' 'info:fdaE20100110_AAACDPfileF20100110_AABPEL' 'sip-files00054thm.jpg'
80d2be5bcaf18db005802d81252463fd
b7358d497763b7918cd67792c18e9050707e3b9a
'2012-05-16T12:20:01-04:00'
describe
'456130' 'info:fdaE20100110_AAACDPfileF20100110_AABPEM' 'sip-files00055.jp2'
7fa0f98b768739e11163d944a9fe7410
4d2c7e0d863bf31f6046b7a1ad7ee0890cb9965c
'2012-05-16T12:28:14-04:00'
describe
'553981' 'info:fdaE20100110_AAACDPfileF20100110_AABPEN' 'sip-files00055.jpg'
808ac7988aec1d4bb5aab8d57079ec02
c714b95b44a95c81ee6cbd30cc62965744d857a8
'2012-05-16T12:27:45-04:00'
describe
'61710' 'info:fdaE20100110_AAACDPfileF20100110_AABPEO' 'sip-files00055.pro'
042e7fdce204152b7b6127cb5cc595ad
164eaa881dd76ee6da57d70ebf589804c839b623
describe
'174023' 'info:fdaE20100110_AAACDPfileF20100110_AABPEP' 'sip-files00055.QC.jpg'
52f2394fc84e7600146925c2583359b5
a04d748683889941d5e1393b281d798234de4bb0
describe
'3651426' 'info:fdaE20100110_AAACDPfileF20100110_AABPEQ' 'sip-files00055.tif'
25293742c8a354174ff3456ad4ff7091
252f6a9112404a82248e5e74a804201cd6e04707
'2012-05-16T12:23:03-04:00'
describe
'2448' 'info:fdaE20100110_AAACDPfileF20100110_AABPER' 'sip-files00055.txt'
883afe0ac309511658b0ef0994099381
9fb4db438c5f95d582752049b6759cb4087be678
describe
'50280' 'info:fdaE20100110_AAACDPfileF20100110_AABPES' 'sip-files00055thm.jpg'
f0fea2c9c63ce2b4a26c6f8ea3696b29
7be250ef4cb829fe7b4d78941e69bb571ee847e2
describe
'2050991' 'info:fdaE20100110_AAACDPfileF20100110_AABPET' 'sip-files00056.jp2'
f05dc7b9695947cea0115b1e2534feed
989458fe6922db35701e8d342ce0914057d68863
describe
'656734' 'info:fdaE20100110_AAACDPfileF20100110_AABPEU' 'sip-files00056.jpg'
abb74edff2ea22fc18eb58e942e02414
864421836ca7d3d6011cc8b6c7cf6c01ff17f1c1
describe
'4019' 'info:fdaE20100110_AAACDPfileF20100110_AABPEV' 'sip-files00056.pro'
3d594b13eb2b1ddc047d06053ed01264
f4cf880f513e5c54aee6c3e8b433d52e1b5ae41c
describe
'173973' 'info:fdaE20100110_AAACDPfileF20100110_AABPEW' 'sip-files00056.QC.jpg'
0b09c47906eb356016bf5a693bb23851
e9f468a0985e9f572647514f7134f0e8f499a5c1
describe
'16413538' 'info:fdaE20100110_AAACDPfileF20100110_AABPEX' 'sip-files00056.tif'
ffe6cf5a55579be43a6e2dfb1373b422
02afe96ef5ce486dc158ef9767ec7e7706ecac81
'2012-05-16T12:25:19-04:00'
describe
'191' 'info:fdaE20100110_AAACDPfileF20100110_AABPEY' 'sip-files00056.txt'
c8f6a4b5f018ecc0dcfdd99b99e80740
931eb287903b67eba62665b473ea29382d5dbcdc
describe
'52076' 'info:fdaE20100110_AAACDPfileF20100110_AABPEZ' 'sip-files00056thm.jpg'
76ea95f8ae04486a4702af78456669af
4550fcae859994005b3d4510c94c624eea3bc1a7
describe
'1991637' 'info:fdaE20100110_AAACDPfileF20100110_AABPFA' 'sip-files00057.jp2'
b6e42fdd819da76fc87f482502af773f
2727282148f98b3cad4ac525559e292a3d143668
describe
'581786' 'info:fdaE20100110_AAACDPfileF20100110_AABPFB' 'sip-files00057.jpg'
661d3291f69dcb0aebd3d5f67488bbff
8047bd2c57cd4299aeb66e726919a5522f67b1fb
describe
'24872' 'info:fdaE20100110_AAACDPfileF20100110_AABPFC' 'sip-files00057.pro'
fe1c94e0e1e45bfb9808de9a3d4bc74f
9e50c44d31a8dda5a2c01d2a44c8ff5117657cd3
'2012-05-16T12:28:11-04:00'
describe
'161395' 'info:fdaE20100110_AAACDPfileF20100110_AABPFD' 'sip-files00057.QC.jpg'
5c08c6d80b56667bf25dd2a87e71ad77
40d3709967e55f400ad08cb4e86068d4c0bf3901
'2012-05-16T12:23:08-04:00'
describe
'15939990' 'info:fdaE20100110_AAACDPfileF20100110_AABPFE' 'sip-files00057.tif'
378fb8b5ba348d11488ab00dcfb474fe
78a708e1d212319df8ac7c32229af74029b44df7
'2012-05-16T12:24:00-04:00'
describe
'1033' 'info:fdaE20100110_AAACDPfileF20100110_AABPFF' 'sip-files00057.txt'
5bd7aa185a1a1304f2ba4add40ec3213
ec0a05599b48b0ade78fc197f585b42472d5b7d0
'2012-05-16T12:22:37-04:00'
describe
'52126' 'info:fdaE20100110_AAACDPfileF20100110_AABPFG' 'sip-files00057thm.jpg'
dc1f9f70dc36aff946ca42d0bf310301
9ee68505582b82fe1bb6a57f0914f4fbc5e5ebc2
'2012-05-16T12:22:03-04:00'
describe
'506354' 'info:fdaE20100110_AAACDPfileF20100110_AABPFH' 'sip-files00058.jp2'
c199924b418563b3ab837513487a666d
37e46c2ca8b4f098388ef2aab805c4cda48ae55c
'2012-05-16T12:21:52-04:00'
describe
'462905' 'info:fdaE20100110_AAACDPfileF20100110_AABPFI' 'sip-files00058.jpg'
30a88d0f9f72f1c852b091ea3bfeb8c4
56e50347b205c8420853933665985ab102d11ffd
'2012-05-16T12:18:38-04:00'
describe
'45753' 'info:fdaE20100110_AAACDPfileF20100110_AABPFJ' 'sip-files00058.pro'
4fef2d727783a6d2dc974045486dd32c
d3d20a0d727ffe1db62661329f8c558bb01f26a7
'2012-05-16T12:22:29-04:00'
describe
'140660' 'info:fdaE20100110_AAACDPfileF20100110_AABPFK' 'sip-files00058.QC.jpg'
794d5982a2ef128525d52e44a57522ef
7c696a35d468b2eed3e484d58272525399d0b4b2
describe
'4053938' 'info:fdaE20100110_AAACDPfileF20100110_AABPFL' 'sip-files00058.tif'
409a8491e483c48a6835ce365c50eae3
a95d8d231e143f5fad4e278b02f4cece9c2e25ec
'2012-05-16T12:20:09-04:00'
describe
'2004' 'info:fdaE20100110_AAACDPfileF20100110_AABPFM' 'sip-files00058.txt'
9602de802b0620facde48fd8d5b290f6
d174eb0dfae740fa2eda70b6c8855bfede29543b
'2012-05-16T12:25:53-04:00'
describe
'40575' 'info:fdaE20100110_AAACDPfileF20100110_AABPFN' 'sip-files00058thm.jpg'
6ecc8eed739cfa2be0086a1d6d6d9f20
8bf8c4f04a0a175a35d98284b3084ced61e9491d
describe
'521147' 'info:fdaE20100110_AAACDPfileF20100110_AABPFO' 'sip-files00059.jp2'
32d30ca0b7797d806842fb59b7b85fe4
507e4df36187ba2cb6dd460471838075a9f66cf1
'2012-05-16T12:19:34-04:00'
describe
'501771' 'info:fdaE20100110_AAACDPfileF20100110_AABPFP' 'sip-filesi.jp2'
186fb6d6805fd83e00867e441cc9f916
cdfbd2ebaa6bf7d84b32ce6361e7b42cebd7315f
'2012-05-16T12:26:24-04:00'
describe
'434863' 'info:fdaE20100110_AAACDPfileF20100110_AABPFQ' 'sip-files00059.jpg'
afea47ea10af287016c4af4c91bd0b8a
d9df431adfe990b9d082e5a5bd490e8125fb7696
'2012-05-16T12:22:07-04:00'
describe
'44628' 'info:fdaE20100110_AAACDPfileF20100110_AABPFR' 'sip-files00059.pro'
d57c5744e73c8bf6c5a0864801d54ac2
a42054638b40e72485b3262353f747e436aa7160
'2012-05-16T12:25:13-04:00'
describe
'135913' 'info:fdaE20100110_AAACDPfileF20100110_AABPFS' 'sip-files00059.QC.jpg'
ae7ec9c57c6206ecc645d3764b6fd7b1
5043afc87feeb8a954ed039319064d5ad9c1b662
'2012-05-16T12:26:11-04:00'
describe
'4171936' 'info:fdaE20100110_AAACDPfileF20100110_AABPFT' 'sip-files00059.tif'
ba3702f3871cb8c4c2d66168aeec7190
2fbbe8f474849507a50d2cffb12418b25a551028
describe
'1989' 'info:fdaE20100110_AAACDPfileF20100110_AABPFU' 'sip-files00059.txt'
715df73f711ec4d9754d99b52d4aba80
54e694bb07a59eb8d04a0ef7b80cba70690d56b7
'2012-05-16T12:21:33-04:00'
describe
'39190' 'info:fdaE20100110_AAACDPfileF20100110_AABPFV' 'sip-files00059thm.jpg'
167b87c53cbfef8340091ba25769c5bf
e00cb57ffeb6118a8408d6962b271d3454cf186a
'2012-05-16T12:27:47-04:00'
describe
'501573' 'info:fdaE20100110_AAACDPfileF20100110_AABPFW' 'sip-files00060.jp2'
2161299d592cd144bae2c5fb64eedf14
a8d8fc0a2160fa2c09502e1460550f1fe9eb0c91
'2012-05-16T12:27:57-04:00'
describe
'422227' 'info:fdaE20100110_AAACDPfileF20100110_AABPFX' 'sip-files00060.jpg'
2d5edcf0a5d313edc8f78f42c9ce2b7a
3c7c3b1a5caacccd240dd01d8c189606d9bf65a9
'2012-05-16T12:22:05-04:00'
describe
'45598' 'info:fdaE20100110_AAACDPfileF20100110_AABPFY' 'sip-files00060.pro'
9341f83b4378d3fbdccac14aa3844e64
ae322bffa30a00c5b130cd5de24d146b9b74b588
describe
'133567' 'info:fdaE20100110_AAACDPfileF20100110_AABPFZ' 'sip-files00060.QC.jpg'
c4339f8dcdee9ff333499101019b87f1
98e458722434bdb5f0fecc985d4b0c599e107bab
'2012-05-16T12:28:17-04:00'
describe
'4015062' 'info:fdaE20100110_AAACDPfileF20100110_AABPGA' 'sip-files00060.tif'
da80a94dae85e074bfcf5e5694479a97
5d317626c4767996cc28a761c7d47a6d009de0d3
'2012-05-16T12:23:48-04:00'
describe
'2047' 'info:fdaE20100110_AAACDPfileF20100110_AABPGB' 'sip-files00060.txt'
f4d1d37c61b18f71ab2fd9a73137b18d
d5f6b8c246f849fe9f4f375ca383015015faf174
'2012-05-16T12:21:12-04:00'
describe
'42438' 'info:fdaE20100110_AAACDPfileF20100110_AABPGC' 'sip-files00060thm.jpg'
a8e51e89623f6ae4bdb44892558560ae
d210ccefe9519213b828169d2d8dd216865b18a3
'2012-05-16T12:19:57-04:00'
describe
'502534' 'info:fdaE20100110_AAACDPfileF20100110_AABPGD' 'sip-files00061.jp2'
ef9435de2bfdd7d2e53cb6f6388b4444
ccb51f7435c5d97d1b87627fe8da08c0dbb97009
describe
'455187' 'info:fdaE20100110_AAACDPfileF20100110_AABPGE' 'sip-files00061.jpg'
90cd022b284a749886b668c29ae749b1
709113bd1560dcd992d0e5e1a03d8487b7ff2356
describe
'51580' 'info:fdaE20100110_AAACDPfileF20100110_AABPGF' 'sip-files00061.pro'
0798b01b08bad251278f39cf17ac85b3
c8f5a9f588cb39a4ab44b5d914e05cce29cba5f2
'2012-05-16T12:25:37-04:00'
describe
'142464' 'info:fdaE20100110_AAACDPfileF20100110_AABPGG' 'sip-files00061.QC.jpg'
e099735e05d2fcb32e8e2eccec7798e0
7ed943a62aa5dd097015e90667fed7c357d415e9
'2012-05-16T12:27:34-04:00'
describe
'4022770' 'info:fdaE20100110_AAACDPfileF20100110_AABPGH' 'sip-files00061.tif'
973c223ff3f1ef3a9d6e514b8bdae587
b9293f79ffd83d0770612cc8b0edc7a9c3f3bba6
'2012-05-16T12:21:56-04:00'
describe
'2183' 'info:fdaE20100110_AAACDPfileF20100110_AABPGI' 'sip-files00061.txt'
1b400e528f99e4229714eccb075340a9
e26bc9f808b8f31d01f9a1b222b330f011193455
describe
'43388' 'info:fdaE20100110_AAACDPfileF20100110_AABPGJ' 'sip-files00061thm.jpg'
72c306292b51b2b073e7571d21237579
b703a9a6b1e36cef107d82bfd9461a17e488f169
describe
'507057' 'info:fdaE20100110_AAACDPfileF20100110_AABPGK' 'sip-files00062.jp2'
f8b12cffef880127ebfd95de5d5cf4ed
1536c42025cef07134a83940bef6c9ee321e0111
'2012-05-16T12:25:33-04:00'
describe
'526808' 'info:fdaE20100110_AAACDPfileF20100110_AABPGL' 'sip-files00062.jpg'
e9f93d39dc65185d079b8b4c24de9927
05423b01525ba9ae99df502fab7fbf90519a509c
'2012-05-16T12:23:51-04:00'
describe
'58872' 'info:fdaE20100110_AAACDPfileF20100110_AABPGM' 'sip-files00062.pro'
8c916aae3d27a68036d7dbb63be71e4c
469354fc46794ab2955291aeb41b1316d4332c4e
describe
'163302' 'info:fdaE20100110_AAACDPfileF20100110_AABPGN' 'sip-files00062.QC.jpg'
9ce6bdb0a5b653ed590ed88dbeb4f0d6
35b3711b5769bf27248c8ddb9ab515951f52af1d
'2012-05-16T12:20:06-04:00'
describe
'4059012' 'info:fdaE20100110_AAACDPfileF20100110_AABPGO' 'sip-files00062.tif'
899808e34ef3ccc23de0f20b9e94191e
b4dd4744f247771086c48c1a75e3956fe8635548
'2012-05-16T12:27:18-04:00'
describe
'2354' 'info:fdaE20100110_AAACDPfileF20100110_AABPGP' 'sip-files00062.txt'
cb6e34e15cbd5e0ab86f57f38685ee47
3b52167ee7d7a1293663732562ae12ef6f813ceb
'2012-05-16T12:21:15-04:00'
describe
'47247' 'info:fdaE20100110_AAACDPfileF20100110_AABPGQ' 'sip-files00062thm.jpg'
1d7403412024fcdb40d36e8efa6934b2
39f8ad134da0375ba254123e8114551c872ff525
'2012-05-16T12:19:15-04:00'
describe
'508669' 'info:fdaE20100110_AAACDPfileF20100110_AABPGR' 'sip-files00063.jp2'
38590e628e1dc6eb8843b9b164904b08
2c463caa90b9930dfac28601465b7d8ccd35689b
describe
'381377' 'info:fdaE20100110_AAACDPfileF20100110_AABPGS' 'sip-files00063.jpg'
11fffd4d91fa87208be1218db475ef8d
ee9287df27fc17f3ca025b161e44b1469641a27c
'2012-05-16T12:24:29-04:00'
describe
'34988' 'info:fdaE20100110_AAACDPfileF20100110_AABPGT' 'sip-files00063.pro'
6a6b6a16cd9ca103fbccd39da1519475
63af08f106479dc34e0c2d5584a690d3e0b5a2c5
'2012-05-16T12:26:18-04:00'
describe
'122088' 'info:fdaE20100110_AAACDPfileF20100110_AABPGU' 'sip-files00063.QC.jpg'
397ff384cbd74c18af6c06c6a945008e
0facf674058fc97dc25ac4668e4a3035438fa0ca
'2012-05-16T12:28:30-04:00'
describe
'4072354' 'info:fdaE20100110_AAACDPfileF20100110_AABPGV' 'sip-files00063.tif'
7eb3c0938f7401c5efbd3f05e94af990
b442adfea5e89f792916e9728ffbf1a7aeaaed74
describe
'1495' 'info:fdaE20100110_AAACDPfileF20100110_AABPGW' 'sip-files00063.txt'
f428be08a80c71a9ddc3693f51e53888
b08c777ee8b9a426d8870992b55c97230f7f1509
'2012-05-16T12:22:45-04:00'
describe
'37530' 'info:fdaE20100110_AAACDPfileF20100110_AABPGX' 'sip-files00063thm.jpg'
d4377951c7e91952cad4459e335fcc53
17f24fb4108fbc5a24ee5e445e96b44404e86493
describe
'507891' 'info:fdaE20100110_AAACDPfileF20100110_AABPGY' 'sip-files00064.jp2'
e7cef315c82d1186bb423249359ed5bf
4ff85e9c2dad960b390820164aa65aa755bb3eaa
'2012-05-16T12:26:59-04:00'
describe
'508763' 'info:fdaE20100110_AAACDPfileF20100110_AABPGZ' 'sip-files00064.jpg'
79daa75906101a43555a5dcc6449be66
a99ecd973a6d77e76c6f214324e757e595774502
describe
'61738' 'info:fdaE20100110_AAACDPfileF20100110_AABPHA' 'sip-files00064.pro'
0100071681746416044aeeca9d2fbe59
f7c9a9b5dcd3d18b66fc7d12d108dd7a242a0ff5
'2012-05-16T12:22:55-04:00'
describe
'162771' 'info:fdaE20100110_AAACDPfileF20100110_AABPHB' 'sip-files00064.QC.jpg'
16483c5bdd0d7fc5cbbe62a4b9020d7f
29a00bc7ad51730d4d7d75ed22746910b99d3ecf
describe
'4065602' 'info:fdaE20100110_AAACDPfileF20100110_AABPHC' 'sip-files00064.tif'
cb9c0dad46fa57192783de54368b2c34
805e7174305964a8488fe15c4d266110390d9e0e
'2012-05-16T12:27:12-04:00'
describe
'2461' 'info:fdaE20100110_AAACDPfileF20100110_AABPHD' 'sip-files00064.txt'
b1111b3ce9647bd402f1bddb5e42bdd2
85df201ee32f9ec9ff9cc75616622294a05d5e22
describe
'47011' 'info:fdaE20100110_AAACDPfileF20100110_AABPHE' 'sip-files00064thm.jpg'
4ccdb16053eab4cf994dd5331bfce087
770391699037e6815d8e1cae829a111a7ffc9073
'2012-05-16T12:23:04-04:00'
describe
'502229' 'info:fdaE20100110_AAACDPfileF20100110_AABPHF' 'sip-files00065.jp2'
fdeea3a3792d5920bb9410b7c9d3e09a
769f85ae388735837d09a49f8161e83f63f652d3
'2012-05-16T12:20:55-04:00'
describe
'579584' 'info:fdaE20100110_AAACDPfileF20100110_AABPHG' 'sip-files00065.jpg'
1eaf1f8350c23d4e2b015269c0a0873d
6d1d1b63ea998764b1d4ba7d6dde6642b83b96ae
'2012-05-16T12:19:01-04:00'
describe
'67499' 'info:fdaE20100110_AAACDPfileF20100110_AABPHH' 'sip-files00065.pro'
fca166a0fd8f8511ea9590db1b77a8a1
5cf259382febac5c6cbaddab2a3ba72e01787c87
'2012-05-16T12:22:20-04:00'
describe
'176253' 'info:fdaE20100110_AAACDPfileF20100110_AABPHI' 'sip-files00065.QC.jpg'
a58294792223b7d8b97a45ceb59fef29
96c9db9d60a53e5d47effdd89a149a4ab85597e4
'2012-05-16T12:18:51-04:00'
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPHJ' 'sip-files00065.tif'
a1ff13d9b2634e86e2fc0f724dce3682
ccd1df2346262903be8703c3b294297ab896e68f
'2012-05-16T12:21:57-04:00'
describe
'2660' 'info:fdaE20100110_AAACDPfileF20100110_AABPHK' 'sip-files00065.txt'
5f24ef67ab24458578d649149b887afb
e1d5171f2b1cb4cab7309459f31db2d281141281
'2012-05-16T12:26:52-04:00'
describe
'50499' 'info:fdaE20100110_AAACDPfileF20100110_AABPHL' 'sip-files00065thm.jpg'
8d372b52b6f98c5b3ee6662b122fe36a
e1fc1a73970430a8181cdd751f8c3cd4b8d870c9
describe
'493540' 'info:fdaE20100110_AAACDPfileF20100110_AABPHM' 'sip-files00066.jp2'
c3a52deb91c7af1c9b2537ede3f9c7d8
e84b6c109f2e3b495605ae898a64fddeea7d55a1
'2012-05-16T12:28:15-04:00'
describe
'539918' 'info:fdaE20100110_AAACDPfileF20100110_AABPHN' 'sip-files00066.jpg'
4f27f615537d937faff5fca3f341fcb7
b61d876a8e57ea73cc2f7d9ff9474ebe66e1e472
'2012-05-16T12:21:07-04:00'
describe
'59449' 'info:fdaE20100110_AAACDPfileF20100110_AABPHO' 'sip-files00066.pro'
e6456b4aeb8771a661c716b5ab31ff8a
d5f969ae323ef9cf4aebc373f82c69420af311c3
describe
'168838' 'info:fdaE20100110_AAACDPfileF20100110_AABPHP' 'sip-files00066.QC.jpg'
ae05a96704a9daa095c89c642ca0a1e8
2590f7f42ec83a7a4f54fc5a79399a31de86262d
describe
'3950790' 'info:fdaE20100110_AAACDPfileF20100110_AABPHQ' 'sip-files00066.tif'
4354a07594fbc4ceb4be0f7ad5270847
919ec53800625afa30b92f34dbd5204e66a7422d
'2012-05-16T12:24:02-04:00'
describe
'2389' 'info:fdaE20100110_AAACDPfileF20100110_AABPHR' 'sip-files00066.txt'
cc631c381de1e44271bf9244dd89733a
67d6742e1d3604377bdb797bfc41d0afcc0071f5
describe
'48096' 'info:fdaE20100110_AAACDPfileF20100110_AABPHS' 'sip-files00066thm.jpg'
3f8ba8d8090db2fb774747d95e5af96e
4f4fd3662163039e951d48052469028b3be7af96
'2012-05-16T12:21:23-04:00'
describe
'505150' 'info:fdaE20100110_AAACDPfileF20100110_AABPHT' 'sip-files00067.jp2'
c5d200e3c37dcf654cc9cb2dfec78234
afa5a4ce58309b81ca75189168a1df7650f0ce58
describe
'542998' 'info:fdaE20100110_AAACDPfileF20100110_AABPHU' 'sip-files00067.jpg'
5acc1222f6a0c4b52c96cc8b4229294c
f2f75be6503782907430fcb0b59db5e7ff6a8cda
'2012-05-16T12:24:08-04:00'
describe
'63678' 'info:fdaE20100110_AAACDPfileF20100110_AABPHV' 'sip-files00067.pro'
c4be2df2646b96e99c8761ae4d16b72c
ac37e20c762ee68bb02e1c048efbdce2b1f59e93
'2012-05-16T12:24:56-04:00'
describe
'168554' 'info:fdaE20100110_AAACDPfileF20100110_AABPHW' 'sip-files00067.QC.jpg'
02c818794df4bea5a99d837fc6e1a219
a8f90fcea6e94b761aa6cb4e05bfca0562668971
describe
'4043746' 'info:fdaE20100110_AAACDPfileF20100110_AABPHX' 'sip-files00067.tif'
ff87f34faa5dfd98a7299f8a74176f2b
98f5b905aceebe889f51d032e5d1e9b6bb58809a
'2012-05-16T12:20:48-04:00'
describe
'2526' 'info:fdaE20100110_AAACDPfileF20100110_AABPHY' 'sip-files00067.txt'
936afa38e5a1b25e63b2a88c6326f559
6d964276c587984da0fb45e0b1c6c0fb5dd106dd
'2012-05-16T12:26:23-04:00'
describe
'49397' 'info:fdaE20100110_AAACDPfileF20100110_AABPHZ' 'sip-files00067thm.jpg'
5a555901cc0f72131d404caf2a3ee5f9
9bb9e9c9da59873675e46cfdbdade6be3582fd69
describe
'512631' 'info:fdaE20100110_AAACDPfileF20100110_AABPIA' 'sip-files00068.jp2'
b75174ae7a415264a7d1b81c04912854
30101ca38c9de350d67b925f10db3dcd835f7944
'2012-05-16T12:26:22-04:00'
describe
'380113' 'info:fdaE20100110_AAACDPfileF20100110_AABPIB' 'sip-files00068.jpg'
2ba92c2f50df26910b1f69d26661e59d
6333d42c56c8a3e0c844b5006b2d153cf284c77d
'2012-05-16T12:18:19-04:00'
describe
'42482' 'info:fdaE20100110_AAACDPfileF20100110_AABPIC' 'sip-files00068.pro'
585b37ec7554608b3322d74d27705b0e
85fb67c59f72e31e75ac02a0dcbf55ba68e54d96
describe
'123185' 'info:fdaE20100110_AAACDPfileF20100110_AABPID' 'sip-files00068.QC.jpg'
be201342083917b5d766bcce55168f81
2e571491aadc20927f686675d4343a313b679dbc
describe
'4103678' 'info:fdaE20100110_AAACDPfileF20100110_AABPIE' 'sip-files00068.tif'
29378bf79ceee705a779d4f06497f2bd
a6b88a05ec355e3c05956248e8cbf3d54afcc74d
'2012-05-16T12:24:22-04:00'
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPIF' 'sip-files00068.txt'
788466527848c75792e5fd74505a4f11
bdccc4a50f07554c5992f35833c087252e7cb693
'2012-05-16T12:28:10-04:00'
describe
'37843' 'info:fdaE20100110_AAACDPfileF20100110_AABPIG' 'sip-files00068thm.jpg'
e4df5871ca867a0f095c619cc6a31cd7
1d32bdee91f19c0d69fabe971596665be54471e0
describe
'509956' 'info:fdaE20100110_AAACDPfileF20100110_AABPIH' 'sip-files00069.jp2'
a454b7d62414353de40162027d539ca7
cf04e9fc9d12a7a4aa626a0a3f81841f18f0cbe6
describe
'507423' 'info:fdaE20100110_AAACDPfileF20100110_AABPII' 'sip-files00069.jpg'
0454c7e773eaec3d4403e20ae6c0b730
48250a67ecb4b8ed9a1f391dc853ae444f0403ac
describe
'59748' 'info:fdaE20100110_AAACDPfileF20100110_AABPIJ' 'sip-files00069.pro'
52951b234f6258d47be104c711a5c2a0
914fb5fc88c037c3286564d12c5c11fa52611b2e
describe
'158100' 'info:fdaE20100110_AAACDPfileF20100110_AABPIK' 'sip-files00069.QC.jpg'
5458c58fd5e85a37a97c4531387afacf
07e278185b005a9080ddc980755e9b7ccf335f17
describe
'4082194' 'info:fdaE20100110_AAACDPfileF20100110_AABPIL' 'sip-files00069.tif'
e00fa8c8a44ab8cc0c921cd6d93f0e2f
d35ebd9a70ad607f81819bbe62c7ab2d73c327bd
describe
'2401' 'info:fdaE20100110_AAACDPfileF20100110_AABPIM' 'sip-files00069.txt'
d2dd362277fef6b9403b0cac027704b3
7677a8918dddacb10545f5aeb4cf1c5ab7ae2df5
describe
'49125' 'info:fdaE20100110_AAACDPfileF20100110_AABPIN' 'sip-files00069thm.jpg'
01999411a6250e3cdaa251696fe81525
570e14d7837c2e179b147d64b92920cae40b2555
'2012-05-16T12:20:21-04:00'
describe
'1990048' 'info:fdaE20100110_AAACDPfileF20100110_AABPIO' 'sip-files00070.jp2'
3c375bfc221d92b8ce9fce0f7f8afc41
c232d4285928868c70a0650bbad190ef11e8bd70
'2012-05-16T12:27:46-04:00'
describe
'392193' 'info:fdaE20100110_AAACDPfileF20100110_AABPIP' 'sip-files00070.jpg'
09b615cbb79a829a0b0d4bf8278d1bf6
6730e4c153ab21859d2205807f882270c48f0d3c
describe
'11196' 'info:fdaE20100110_AAACDPfileF20100110_AABPIQ' 'sip-files00070.pro'
459eb55a8d64e9f186030e51b5c86412
adf8ec395d7acd57e10f1422e0d5f506f178d351
describe
'115223' 'info:fdaE20100110_AAACDPfileF20100110_AABPIR' 'sip-files00070.QC.jpg'
a35565b7fefb34fd0b6d5b493cb56611
8f30377ec3772c28e0214642df0f62c87e09e827
describe
'15925574' 'info:fdaE20100110_AAACDPfileF20100110_AABPIS' 'sip-files00070.tif'
df20edbfd34e3df8fea560f51ac2cd9b
4bea052f17336e0ebc7832417d870bcf07102a94
'2012-05-16T12:28:06-04:00'
describe
'491' 'info:fdaE20100110_AAACDPfileF20100110_AABPIT' 'sip-files00070.txt'
1c53cdd6e7f5b6212dbf31e7d531cd6c
ad1ea6c6d014dbfbecea218b9b2b9ee7930ec5eb
'2012-05-16T12:25:40-04:00'
describe
'37063' 'info:fdaE20100110_AAACDPfileF20100110_AABPIU' 'sip-files00070thm.jpg'
2f3e3ac7d97d7872a324c281b5f700c9
17d2293b2b6c6df42b1e1d493545cc0f772641ef
'2012-05-16T12:21:21-04:00'
describe
'2070810' 'info:fdaE20100110_AAACDPfileF20100110_AABPIV' 'sip-files00071.jp2'
0e9e10398c313a417d957a0a9c139a0a
83fd875fca56033eb8516b181fe0dd28456f5c46
'2012-05-16T12:21:38-04:00'
describe
'418608' 'info:fdaE20100110_AAACDPfileF20100110_AABPIW' 'sip-files00071.jpg'
e637f2750ffd76b61e2a933f1949dc89
94002701ea9268100a98066b019b8265b8af3baa
describe
'40252' 'info:fdaE20100110_AAACDPfileF20100110_AABPIX' 'sip-files00071.pro'
20444f471f7cb8e42fe8cbf0e0b1892a
c9784fdcd10187b6728360f3dc06e0782d3294a2
describe
'124034' 'info:fdaE20100110_AAACDPfileF20100110_AABPIY' 'sip-files00071.QC.jpg'
6c2a6eed72fff73e0739a55d1c92f4ec
688612c027bb7a6977e5c370a02c2e270d54ca57
'2012-05-16T12:24:32-04:00'
describe
'16571668' 'info:fdaE20100110_AAACDPfileF20100110_AABPIZ' 'sip-files00071.tif'
61d8f5a56b57777f02ffc1ae9e617e8a
87eace7be5cd77bcd11900979d52dd1695dee500
describe
'2311' 'info:fdaE20100110_AAACDPfileF20100110_AABPJA' 'sip-files00071.txt'
4217e591534607e98328debcf57621d6
48918295809ff229af335e9a24c9e2b330311aaa
'2012-05-16T12:18:39-04:00'
describe
'41422' 'info:fdaE20100110_AAACDPfileF20100110_AABPJB' 'sip-files00071thm.jpg'
92bf241c8eaee71544fa94d743e51036
ad7b3e95907036815a873c6582eda531f5e2603f
'2012-05-16T12:24:18-04:00'
describe
'493789' 'info:fdaE20100110_AAACDPfileF20100110_AABPJC' 'sip-files00072.jp2'
1fcbf23d76a3c4944d984c1f2035fcf6
9e7c8ceabd9366e9deb69fa85a33bec5166ce6bd
describe
'533124' 'info:fdaE20100110_AAACDPfileF20100110_AABPJD' 'sip-files00072.jpg'
83aa3fd1a2cae3b89951fabe3c56cdb2
cf7df2b6511efaa2a3bfa58fdc4e0421995d55d0
'2012-05-16T12:20:05-04:00'
describe
'58781' 'info:fdaE20100110_AAACDPfileF20100110_AABPJE' 'sip-files00072.pro'
f5d9f94b05bc0bcfa205cd3709067a0e
89a4b229107396ab3a88499cc1be544f840a7dd6
'2012-05-16T12:20:30-04:00'
describe
'165234' 'info:fdaE20100110_AAACDPfileF20100110_AABPJF' 'sip-files00072.QC.jpg'
c46c4b7822ce3088db4c758529209d68
641ad7ff67079c103f8da97d0263408315fcf32b
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPJG' 'sip-files00072.tif'
c1a09b448c107c8f3ba9500f6e147ee3
31a0b7ab0ab4349753bc956411360d93eb3ffb96
'2012-05-16T12:20:57-04:00'
describe
'2405' 'info:fdaE20100110_AAACDPfileF20100110_AABPJH' 'sip-files00072.txt'
58c982b642b05f8cce50d086997044f7
8b69bbf665c78af06cb6b70ea24c4d35d6f1a377
describe
'48820' 'info:fdaE20100110_AAACDPfileF20100110_AABPJI' 'sip-files00072thm.jpg'
284aa40176e701be44e8a80e1c52c211
587083f35bc3486ada32d569f03e483848040e51
'2012-05-16T12:22:42-04:00'
describe
'503837' 'info:fdaE20100110_AAACDPfileF20100110_AABPJJ' 'sip-files00073.jp2'
71d71c84486f6e1724520029c8119564
1fed71ed6f88268eebdb696425307eaccfab944f
describe
'138453' 'info:fdaE20100110_AAACDPfileF20100110_AABPJK' 'sip-files00073.jpg'
1519273970b7f83dd1e660701fe3f1e1
d3b7588182ba6a8dccda5531aad9a468e11bcc09
'2012-05-16T12:24:05-04:00'
describe
'16703' 'info:fdaE20100110_AAACDPfileF20100110_AABPJL' 'sip-files00073.pro'
69c21583803dd79c527a44186bc2f1f9
670a57ac41f00524c6ff0d03365a3901d2cd4136
'2012-05-16T12:27:09-04:00'
describe
'40540' 'info:fdaE20100110_AAACDPfileF20100110_AABPJM' 'sip-files00073.QC.jpg'
f183a212e06b779f6065cd445ac78c3b
db4c5736515be37b0089c532dfd7bfc845824b1b
'2012-05-16T12:19:02-04:00'
describe
'4032198' 'info:fdaE20100110_AAACDPfileF20100110_AABPJN' 'sip-files00073.tif'
f265726615a3925cae257c0869d19f00
3071089830e2842d572405d64dc1a21b94780382
'2012-05-16T12:25:50-04:00'
describe
'952' 'info:fdaE20100110_AAACDPfileF20100110_AABPJO' 'sip-files00073.txt'
8995a222d9c6f58a0f7134e6a66c5b84
e5d83502e88e51918eedf7c7a460069a9b6b73fd
describe
'13144' 'info:fdaE20100110_AAACDPfileF20100110_AABPJP' 'sip-files00073thm.jpg'
bae6bb8d18b48950ac2a668deaec3c4d
ff45b7c1c155511569f665d4cf5ec7843465d2b6
'2012-05-16T12:19:27-04:00'
describe
'506436' 'info:fdaE20100110_AAACDPfileF20100110_AABPJQ' 'sip-files00074.jp2'
c5abe25c5ba1faeb3c94a6ab54eb0ef8
d3e65aeb976f4e2dd3d07666974431c53c4853d9
describe
'497821' 'info:fdaE20100110_AAACDPfileF20100110_AABPJR' 'sip-files00074.jpg'
f129888246c59f8b4c5811f789349f1e
617283b05fbf321c6f1734b16e2c0ef8175f68ef
'2012-05-16T12:20:52-04:00'
describe
'50761' 'info:fdaE20100110_AAACDPfileF20100110_AABPJS' 'sip-files00074.pro'
3d216f8d85ecbd20c7fad160ea70f09e
42527dd5b1761f8904c08c1e6753eaac924494a4
'2012-05-16T12:27:16-04:00'
describe
'153456' 'info:fdaE20100110_AAACDPfileF20100110_AABPJT' 'sip-files00074.QC.jpg'
de0fc4881da4a255fef0abf7336123ee
9952f02832525ffea1afe713c371fbd0a5a71cf1
describe
'4054138' 'info:fdaE20100110_AAACDPfileF20100110_AABPJU' 'sip-files00074.tif'
764c13708aee6eb4dde1f8fcbc9da987
a501f6ca2d1b69efa738dd9ec0fcf000aff351a6
'2012-05-16T12:26:39-04:00'
describe
'2038' 'info:fdaE20100110_AAACDPfileF20100110_AABPJV' 'sip-files00074.txt'
a949cef6b698c6de1f1b6b7c479b3412
181b7b4c4d9dcee1c24d417d887df1491fc9376e
describe
'44837' 'info:fdaE20100110_AAACDPfileF20100110_AABPJW' 'sip-files00074thm.jpg'
3452bf62f6aa409cb570f086a3a8b9a0
b75065d4f2f4419d5b1ce5540e6d93e61255ab80
describe
'512414' 'info:fdaE20100110_AAACDPfileF20100110_AABPJX' 'sip-files00075.jp2'
d70b996e5800de31da45a4e4625b26b7
b48cee04c756d46046f4561043ab412e5c67711f
'2012-05-16T12:26:01-04:00'
describe
'430258' 'info:fdaE20100110_AAACDPfileF20100110_AABPJY' 'sip-files00075.jpg'
b629ba46ae8f01485dba425d117806ac
f1222aba3da179758a69098648be36f6ea2fcea5
'2012-05-16T12:22:21-04:00'
describe
'45919' 'info:fdaE20100110_AAACDPfileF20100110_AABPJZ' 'sip-files00075.pro'
ba98327e78ef20caa77f8a6f0f3496f2
e38318d8da3d8fd714ef15f4180e4d147bac7069
describe
'128864' 'info:fdaE20100110_AAACDPfileF20100110_AABPKA' 'sip-files00075.QC.jpg'
ac457c1dd4eb3635b054039485a4baee
341343636f00094ac00098b77f32ba844b3e81dc
describe
'4101876' 'info:fdaE20100110_AAACDPfileF20100110_AABPKB' 'sip-files00075.tif'
59fecbba221bcf4bdbacec39397f4e5c
7c1bac7f098a8afe18fadbd1c51787db29ece7fe
describe
'2210' 'info:fdaE20100110_AAACDPfileF20100110_AABPKC' 'sip-files00075.txt'
27dbc8da6a9f7424359939344b780b15
18a0853958ce1dc08fef297ae9fd9f2db600bc22
'2012-05-16T12:28:24-04:00'
describe
'41799' 'info:fdaE20100110_AAACDPfileF20100110_AABPKD' 'sip-files00075thm.jpg'
0c93fee83d311c76a3976f6e1d5eba33
9dd8424788057b6ce167f4433c5b4b13b6cbfc70
describe
'551642' 'info:fdaE20100110_AAACDPfileF20100110_AABPKE' 'sip-files00076.jp2'
9cb28055166b941ed4b65a07f05e805e
32a0f8afaf8689fc025a07b14bd644384ba36024
'2012-05-16T12:27:06-04:00'
describe
'153700' 'info:fdaE20100110_AAACDPfileF20100110_AABPKF' 'sip-files00076.jpg'
5a2129e4b378d93d378e560566e35b22
f8da80a0ca346199eadfdec29d607b9c6d63fc64
describe
'42215' 'info:fdaE20100110_AAACDPfileF20100110_AABPKG' 'sip-files00076.pro'
fd2dc7d30052b12b9dead3edbd1fe2cc
48dd2a497d0500343e1ac0eaf5619824b5135c0b
'2012-05-16T12:22:23-04:00'
describe
'47548' 'info:fdaE20100110_AAACDPfileF20100110_AABPKH' 'sip-files00076.QC.jpg'
47dc2329e6718f66b526c2fdc3fb318f
362a21ec6a1c8418d29873533781bc7e4148b90b
describe
'4414898' 'info:fdaE20100110_AAACDPfileF20100110_AABPKI' 'sip-files00076.tif'
5e71f56a80e7a5f192b0a6e5a60334c3
999a4c0d5ae5b1a149cebf7612419ca2f80178cf
'2012-05-16T12:22:51-04:00'
describe
'2743' 'info:fdaE20100110_AAACDPfileF20100110_AABPKJ' 'sip-files00076.txt'
2539f35c6e21e65a02e58d11e2d80e91
241f6c028e7588cc3db2f2620c6b091ca05e5a6e
'2012-05-16T12:25:56-04:00'
describe
Invalid character
'15099' 'info:fdaE20100110_AAACDPfileF20100110_AABPKK' 'sip-files00076thm.jpg'
53049216ec440a36876eb544b4f97af4
a1a08ca823ba6b0aee8745eb07c6c441184af9a8
'2012-05-16T12:18:40-04:00'
describe
'554677' 'info:fdaE20100110_AAACDPfileF20100110_AABPKL' 'sip-files00077.jp2'
40c9e3a8b989b593d41d315ad9b3b263
751c15d9cec15fd53f2d83c9c1b42b3a47b1d2a3
'2012-05-16T12:24:11-04:00'
describe
'140554' 'info:fdaE20100110_AAACDPfileF20100110_AABPKM' 'sip-files00077.jpg'
4c7dcc725c1ec157e266471f2f969f79
c1b1344bf9b538eddf1fb0a8e37e31510aec8f3b
describe
'32753' 'info:fdaE20100110_AAACDPfileF20100110_AABPKN' 'sip-files00077.pro'
226eea30d544acf12fcd9426c0794541
5d3c4914ebb4a05187387ce4eb09dd489a9a929a
describe
'41496' 'info:fdaE20100110_AAACDPfileF20100110_AABPKO' 'sip-files00077.QC.jpg'
0ceabfb058c7f11fe71222a6b99a8be6
59ee7a9802b7b5a98765d3aa879152e635f27cde
describe
'4439420' 'info:fdaE20100110_AAACDPfileF20100110_AABPKP' 'sip-files00077.tif'
1142c11201a1c41c72453f518a8d4f72
d6dba57d10108b5f0d8bcb7c3be10e1927bb0381
'2012-05-16T12:23:56-04:00'
describe
'1625' 'info:fdaE20100110_AAACDPfileF20100110_AABPKQ' 'sip-files00077.txt'
aa752748dd6878555e393f783158f31a
0cdeb0eb1d978a7f9e981ea11c1a1b73863a9cd6
'2012-05-16T12:25:23-04:00'
describe
Invalid character
'13168' 'info:fdaE20100110_AAACDPfileF20100110_AABPKR' 'sip-files00077thm.jpg'
0febdae83cba59d2793feff328d7e3cb
d136b0607b8b0fe557e49bf6799e4f4d29f8a9aa
describe
'518504' 'info:fdaE20100110_AAACDPfileF20100110_AABPKS' 'sip-files00078.jp2'
25477ae44991b324ccf01ca1ed467966
48059ea422307940e82bb35f9cf992c3c1107bcc
describe
'467476' 'info:fdaE20100110_AAACDPfileF20100110_AABPKT' 'sip-files00078.jpg'
7428eae2519467d2294d18ab7c6339b6
b0431c8debe528cd27c48b3296f8a5b811331517
describe
'51725' 'info:fdaE20100110_AAACDPfileF20100110_AABPKU' 'sip-files00078.pro'
c5a59c14fd18e068fee7d7614624b5b7
3d9f99b2540f601ea9ac5ef593179f8341222894
describe
'143022' 'info:fdaE20100110_AAACDPfileF20100110_AABPKV' 'sip-files00078.QC.jpg'
67fcaf305467d9012adc8093dc5444d4
c4cce598ec888022851c91b2de56e0a5123c02b6
'2012-05-16T12:26:05-04:00'
describe
'4150660' 'info:fdaE20100110_AAACDPfileF20100110_AABPKW' 'sip-files00078.tif'
e493d9c8a537d0f8f506ae7ab269ad61
d95f0edcaa52e07dc1174df397ecc7b6c8222ab6
'2012-05-16T12:23:33-04:00'
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPKX' 'sip-files00078.txt'
0c69a890e105e7f93a9fc6f04f55474f
795a0dac179a4954ff13728671aba4bc63e2cba0
describe
'41891' 'info:fdaE20100110_AAACDPfileF20100110_AABPKY' 'sip-files00078thm.jpg'
e38b778b444065b3080b6e38822fbc65
691b106a6e31d54b3e497d573f8a2b554502cd2e
describe
'510633' 'info:fdaE20100110_AAACDPfileF20100110_AABPKZ' 'sip-files00079.jp2'
8f13c3cfb10b5cd9ab60ce3f7e1bba27
a3f657b8153dfe200000e06d18b679b34a4c7f74
'2012-05-16T12:27:13-04:00'
describe
'507996' 'info:fdaE20100110_AAACDPfileF20100110_AABPLA' 'sip-files00079.jpg'
7da9d5c99a895009c35ccc72f28e928e
7ff588f6250ee5c4d575c1895b66ce667b1f8e55
'2012-05-16T12:22:47-04:00'
describe
'54494' 'info:fdaE20100110_AAACDPfileF20100110_AABPLB' 'sip-files00079.pro'
d30d2dc35f8c24163199b6f0e267cc9a
7cf129570097e17bebe4fbb7c630e3db69efd91a
'2012-05-16T12:26:40-04:00'
describe
'156994' 'info:fdaE20100110_AAACDPfileF20100110_AABPLC' 'sip-files00079.QC.jpg'
9aa6ae9d458e7e8d909276a35dd1ab8b
47c2944a7a60645dd1e952802fdcb02df94597fe
describe
'4087644' 'info:fdaE20100110_AAACDPfileF20100110_AABPLD' 'sip-files00079.tif'
a5b62fb0271a6ce97747374c36f1ead5
ac01c2079e3b7b9ae9ef284321ca5e2d4318b3ed
'2012-05-16T12:27:27-04:00'
describe
'2231' 'info:fdaE20100110_AAACDPfileF20100110_AABPLE' 'sip-files00079.txt'
04f5f37776940c457e426a25e4332ede
42fd4679e95ebab1db64f16d6f491d68f723d30b
'2012-05-16T12:20:43-04:00'
describe
'46703' 'info:fdaE20100110_AAACDPfileF20100110_AABPLF' 'sip-files00079thm.jpg'
32a144fffd4f57030ee5f9205b88d282
7d0ee9bd71866edc9d8898b975e4d463f49b0f59
'2012-05-16T12:23:46-04:00'
describe
'1998315' 'info:fdaE20100110_AAACDPfileF20100110_AABPLG' 'sip-files00080.jp2'
97010194607b3dca3a63f395525ae360
9894cd4f8f7cfda158ecb6a0712d2a1c99d2b83d
describe
'138764' 'info:fdaE20100110_AAACDPfileF20100110_AABPLH' 'sip-files00080.jpg'
e934a0cb3ff4c36502b6a8cf8112fddb
8fdc78fabe6e4c75f18a2f2c587b25ec597fbba5
describe
'16740' 'info:fdaE20100110_AAACDPfileF20100110_AABPLI' 'sip-files00080.pro'
4782b70f67f22a409528937130b8735b
b17426faf434caa969ae3af1e1f85ce1e97076d4
describe
'42388' 'info:fdaE20100110_AAACDPfileF20100110_AABPLJ' 'sip-files00080.QC.jpg'
e2d3577c0fc89a77d9b6dc27dfddf82b
4faaf5eaf2ef3f3dc7a33edf87373aa50a7f3621
describe
'15989650' 'info:fdaE20100110_AAACDPfileF20100110_AABPLK' 'sip-files00080.tif'
3779e1e091bb1995cc467379a5af0338
7a613a7ef89a79dfc2b033e5a2bff1c7904203e2
'2012-05-16T12:22:36-04:00'
describe
'1237' 'info:fdaE20100110_AAACDPfileF20100110_AABPLL' 'sip-files00080.txt'
c371470ad799e69f9463d4208a638db2
55503626454014e41211d6383741e45c1f25aa9e
'2012-05-16T12:20:25-04:00'
describe
'13759' 'info:fdaE20100110_AAACDPfileF20100110_AABPLM' 'sip-files00080thm.jpg'
0eea487f86e34459f32f534221049aa0
166b6ebc9616841801c808cfc8e0e88cf07cd348
describe
'489432' 'info:fdaE20100110_AAACDPfileF20100110_AABPLN' 'sip-files00081.jp2'
b1c47909a0131dd01c094f8d7b4d21d6
b324447663dbc1d17289259f6a2a731dcd718560
'2012-05-16T12:23:00-04:00'
describe
'458821' 'info:fdaE20100110_AAACDPfileF20100110_AABPLO' 'sip-files00081.jpg'
6ac58b42f3ccb62f941985328d343d9a
8b25061e187a97c255f1979f678a2389a9e5f545
'2012-05-16T12:26:31-04:00'
describe
'62011' 'info:fdaE20100110_AAACDPfileF20100110_AABPLP' 'sip-files00081.pro'
b42a02f50dc781fbfca9b70116af271c
1a22b51794572986c7b93bf86620869604ffe41c
describe
'152020' 'info:fdaE20100110_AAACDPfileF20100110_AABPLQ' 'sip-files00081.QC.jpg'
59445acfe9dfa83c4cfcd56e6aec6058
9cbc45610dd3ad7fef43f25bfb20c5df153e8f83
'2012-05-16T12:18:46-04:00'
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPLR' 'sip-files00081.tif'
3e0da72638c265fe696539c172f00695
bb507e658397059e589c952f7fccc388684f22ef
describe
'2485' 'info:fdaE20100110_AAACDPfileF20100110_AABPLS' 'sip-files00081.txt'
0327de22480aa2486ff056ba9195eea1
55838941195620769b0141c63f73b38907809766
'2012-05-16T12:21:22-04:00'
describe
'48305' 'info:fdaE20100110_AAACDPfileF20100110_AABPLT' 'sip-files00081thm.jpg'
ceabd96e1259d5e09239728190cebc40
37ed69048c895aa8790094ee5cc7553ed0dc1c26
'2012-05-16T12:28:08-04:00'
describe
'2013283' 'info:fdaE20100110_AAACDPfileF20100110_AABPLU' 'sip-files00082.jp2'
a28c91124751e46fb9cac498a8fd7ba0
bda128dd91ca0039d7f955f52ade2934a1f3824e
'2012-05-16T12:20:49-04:00'
describe
'471884' 'info:fdaE20100110_AAACDPfileF20100110_AABPLV' 'sip-files00082.jpg'
dcdbe8fd7fbb6797c7c710b1264984bc
a58d2b6b1ebfe8f304606d98367f027d99de0a31
'2012-05-16T12:18:45-04:00'
describe
'33992' 'info:fdaE20100110_AAACDPfileF20100110_AABPLW' 'sip-files00082.pro'
a80bd11ebaaffaa8001a9c60d69619a1
137fee79c58aa22d4b3a9537a36a18f8da5031c8
'2012-05-16T12:24:39-04:00'
describe
'137631' 'info:fdaE20100110_AAACDPfileF20100110_AABPLX' 'sip-files00082.QC.jpg'
5fbf6495cc6782f1009e894f160c2576
05acc1f4cece57b6eb190e73e69224117d69125c
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPLY' 'sip-files00082.tif'
1cab2fcf21eeca22b5b3249ef35bd827
4dd88160a95399c8e646ea4e5b976ca51b5c2826
describe
'1506' 'info:fdaE20100110_AAACDPfileF20100110_AABPLZ' 'sip-files00082.txt'
1eb4064315eada20d5b0166883f46bc7
edf2cbc46f62de613f966a45661ecdc6828dd1dc
describe
Invalid character
'42703' 'info:fdaE20100110_AAACDPfileF20100110_AABPMA' 'sip-files00082thm.jpg'
454cd0bf97e44aad38ec9e1559ff33a7
9fd6eda8cd5cf29ff353010593d8038fe1f9c54e
describe
'2015640' 'info:fdaE20100110_AAACDPfileF20100110_AABPMB' 'sip-files00083.jp2'
dec0f6089d3991ef8f68caf05a3a5b71
9f97d67edb90453f683304d15a3dfb89ea4d6878
'2012-05-16T12:22:12-04:00'
describe
'385766' 'info:fdaE20100110_AAACDPfileF20100110_AABPMC' 'sip-files00083.jpg'
c60c88ac231603b34e809e663667de4d
558bc95d483f5b6df60d8b90519c99d2942fe8f5
describe
'14666' 'info:fdaE20100110_AAACDPfileF20100110_AABPMD' 'sip-files00083.pro'
41dd427655e7525bbdaa5f0aafb7369a
bbd13ce880296686672bc3b03022a67786f3e1de
describe
'119922' 'info:fdaE20100110_AAACDPfileF20100110_AABPME' 'sip-files00083.QC.jpg'
e35a32f5857459ceb776a2622c20c3fb
516db92ba96831441857f349cfce2fad4e7ae00f
'2012-05-16T12:18:30-04:00'
describe
'16130220' 'info:fdaE20100110_AAACDPfileF20100110_AABPMF' 'sip-files00083.tif'
7da3147b2e860311f925ea20efed2245
c1692240a4765ac7ebccea5db11503a388f4c4bd
'2012-05-16T12:27:44-04:00'
describe
'774' 'info:fdaE20100110_AAACDPfileF20100110_AABPMG' 'sip-files00083.txt'
71d11c866d8c892629283feea5ec2381
c49a7680ca7cae5a6b47bfdf5ed40dc8e1d8b119
describe
'40511' 'info:fdaE20100110_AAACDPfileF20100110_AABPMH' 'sip-files00083thm.jpg'
86d25dca23dd4e53c2a67656fe8945b4
f9243996035efaef2b9c28234313d6b7423ad2cd
describe
'2053144' 'info:fdaE20100110_AAACDPfileF20100110_AABPMI' 'sip-files00084.jp2'
07b1b5d2f2016a6a8db71322b8c3ce98
4b8e9c2db286bc9be4647625c86dc07b8bd6cb26
'2012-05-16T12:22:46-04:00'
describe
'371441' 'info:fdaE20100110_AAACDPfileF20100110_AABPMJ' 'sip-files00084.jpg'
5c5f247f5c1f35f7557db609b6a18de8
25640373cf085bf16c0dfd7fc1a0cb02a66ceca9
'2012-05-16T12:26:06-04:00'
describe
'17816' 'info:fdaE20100110_AAACDPfileF20100110_AABPMK' 'sip-files00084.pro'
63dac16fc502be72950923c82c0ac935
03af578c919da5cc4123e2e62d0feaae8382da11
describe
'115850' 'info:fdaE20100110_AAACDPfileF20100110_AABPML' 'sip-files00084.QC.jpg'
e7946ca433b477d19a5cd28b256ea14e
d02836bd5c496c2fcf68dcb8f063d9fcefd277d3
describe
'16430276' 'info:fdaE20100110_AAACDPfileF20100110_AABPMM' 'sip-files00084.tif'
f6ecacb9793728528a5e64a2df5e8442
03a719fb25d57906d8254f2161fcf13caac6ea81
'2012-05-16T12:18:26-04:00'
describe
'1065' 'info:fdaE20100110_AAACDPfileF20100110_AABPMN' 'sip-files00084.txt'
07ba48ad4e5ae85b61be47f20e9bcddb
68d279643ba1d8a8d96ebbbd151ae6065f0fe337
'2012-05-16T12:19:06-04:00'
describe
Invalid character
'39078' 'info:fdaE20100110_AAACDPfileF20100110_AABPMO' 'sip-files00084thm.jpg'
62c3bfada9ffd1319c7879f885c62137
ba69e119de5e38ec7d26b69e00b81757a511cc95
describe
'504725' 'info:fdaE20100110_AAACDPfileF20100110_AABPMP' 'sip-files00085.jp2'
595f721a7f6ef251ed06e9ad1d861dc7
7d2f07b9eb7368540cecee6d37050b2fcb7985a1
'2012-05-16T12:24:10-04:00'
describe
'538269' 'info:fdaE20100110_AAACDPfileF20100110_AABPMQ' 'sip-files00085.jpg'
067fd19cd663dbf6aba2060e03180fad
aa97a0dd85cf806f601289e7c423c5cc77360b24
describe
'60874' 'info:fdaE20100110_AAACDPfileF20100110_AABPMR' 'sip-files00085.pro'
70f1c34d8cc3fa2d29158be5b000c2b4
d2e91d9f2d7a9e81332daf579d5c45bb8f31172d
describe
'165031' 'info:fdaE20100110_AAACDPfileF20100110_AABPMS' 'sip-files00085.QC.jpg'
c81bd9e8f4f4eea5ec5c2104a2c9cb60
e1ecc754fc27c44f1304cc95b7ec552569ef5e13
describe
'4040436' 'info:fdaE20100110_AAACDPfileF20100110_AABPMT' 'sip-files00085.tif'
2e06022c3fc55d0b09c7e015e3f3f76b
9b64a5fa486478fff70672dce68c86a566217393
'2012-05-16T12:18:23-04:00'
describe
'2441' 'info:fdaE20100110_AAACDPfileF20100110_AABPMU' 'sip-files00085.txt'
0fb1207a6ae6a359d19b09b4420e4623
6ee869dec8bc002f2c45e3452469a8fc154fc328
'2012-05-16T12:26:34-04:00'
describe
'50698' 'info:fdaE20100110_AAACDPfileF20100110_AABPMV' 'sip-files00085thm.jpg'
def7969fded1624f111c5c1c148d6df0
7cf18b13d7a2356e5cfe061576b413f7894d5fbf
describe
'2072742' 'info:fdaE20100110_AAACDPfileF20100110_AABPMW' 'sip-files00086.jp2'
7d0daa0757b250286f8def888a2c3c87
79c0c83c2559d450c3d22925b878926787a5f219
'2012-05-16T12:25:11-04:00'
describe
'189558' 'info:fdaE20100110_AAACDPfileF20100110_AABPMX' 'sip-files00086.jpg'
8fae87dfe4e8ecef33b4055e69888321
a891eb596d2afb39317d89b3eb2f3a7487540faa
describe
'5783' 'info:fdaE20100110_AAACDPfileF20100110_AABPMY' 'sip-files00086.pro'
62f8727dede6c3de796f0bdc5318f516
943bbd671b130e7fb3b5dfc249cdd0adec68c028
describe
'53314' 'info:fdaE20100110_AAACDPfileF20100110_AABPMZ' 'sip-files00086.QC.jpg'
eacf9fd04559a49e62bf48916123c40f
47931189ada63f8a77b5bd975d4cd9a50ef36f18
'2012-05-16T12:22:13-04:00'
describe
'16585138' 'info:fdaE20100110_AAACDPfileF20100110_AABPNA' 'sip-files00086.tif'
17c45b1ea87fa791383765bb1ee331df
ff31cd12e843934027d208b5071bbec9eceecb6c
'2012-05-16T12:19:37-04:00'
describe
'330' 'info:fdaE20100110_AAACDPfileF20100110_AABPNB' 'sip-files00086.txt'
7b9a36a7f1991361277017b61122cf30
92ac9e1d0151f466bbe3be9fffafd9a7b88e9a68
describe
'17425' 'info:fdaE20100110_AAACDPfileF20100110_AABPNC' 'sip-files00086thm.jpg'
094cebd3db1da0bb9f6bacfead80c920
1878fe704fd4333e5e5d6aecccde1a1f87b1d959
'2012-05-16T12:28:39-04:00'
describe
'2026801' 'info:fdaE20100110_AAACDPfileF20100110_AABPND' 'sip-files00087.jp2'
1e70aa0ce04a8499984ebb2e12d2b415
955b012a49c2c4e579b52534fcde98ec68011743
'2012-05-16T12:26:51-04:00'
describe
'364956' 'info:fdaE20100110_AAACDPfileF20100110_AABPNE' 'sip-files00087.jpg'
f664a350a1171e11d545db0788221b90
5574f0cc4943359532d7c9c798602b41fb67f12a
'2012-05-16T12:22:26-04:00'
describe
'23219' 'info:fdaE20100110_AAACDPfileF20100110_AABPNF' 'sip-files00087.pro'
cf1c2b72bd6ffd05f19687eecf92af1b
86322be82e73ddcf2bf64fcb59baa889912090a3
'2012-05-16T12:25:16-04:00'
describe
'108349' 'info:fdaE20100110_AAACDPfileF20100110_AABPNG' 'sip-files00087.QC.jpg'
94ff1aaf73746e472eb5a2a2a501b839
786b5999bebab3fe639c4950e0a4f209e462e14a
'2012-05-16T12:23:49-04:00'
describe
'16219570' 'info:fdaE20100110_AAACDPfileF20100110_AABPNH' 'sip-files00087.tif'
60816449ca092a31aa0d15c400c8df72
7c438b538ab96c32547082cc91513091512033c0
'2012-05-16T12:25:22-04:00'
describe
'1366' 'info:fdaE20100110_AAACDPfileF20100110_AABPNI' 'sip-files00087.txt'
d61f0b2f46c6c0992fbab37c812ad173
fc1f745346191b744dd081661bcfc955e6cccb1c
'2012-05-16T12:23:27-04:00'
describe
Invalid character
'37061' 'info:fdaE20100110_AAACDPfileF20100110_AABPNJ' 'sip-files00087thm.jpg'
42c8b73f41e96002636f9ee369a2e870
e4c4096dd526c1d146b03cc2a5a4c4c3f7c6884b
'2012-05-16T12:28:43-04:00'
describe
'503188' 'info:fdaE20100110_AAACDPfileF20100110_AABPNK' 'sip-files00088.jp2'
8809723548a9b9433880172535b21338
9dec5b53a3424904f37069503d4ff74cabb898ae
'2012-05-16T12:22:44-04:00'
describe
'475524' 'info:fdaE20100110_AAACDPfileF20100110_AABPNL' 'sip-files00088.jpg'
44f777a56931b9e08d01f3324b217fe1
2ad56bfb81e53f03375009bcb4e436ccfc807f9c
describe
'258832' 'info:fdaE20100110_AAACDPfileF20100110_AABPNM' 'sip-filesi.jpg'
b3e729043b5aaa7f4e075efc725435df
c80c4caf240c83a613524ec4b0bf953da84ba0bb
'2012-05-16T12:23:38-04:00'
describe
'48468' 'info:fdaE20100110_AAACDPfileF20100110_AABPNN' 'sip-files00088.pro'
e3036c19b541e8e76dd794e4eb118194
277253ec59c6032e26dbfec16e83e0fc71de222b
describe
'144437' 'info:fdaE20100110_AAACDPfileF20100110_AABPNO' 'sip-files00088.QC.jpg'
5cdca57ebec40bc167bce3466aba7ea5
eea7039e08d8e3c511f24720a01778a8302a1df1
'2012-05-16T12:21:27-04:00'
describe
'4027990' 'info:fdaE20100110_AAACDPfileF20100110_AABPNP' 'sip-files00088.tif'
5899c05a62a0e7ae2354a7d4ba791b60
942398c8dfd631ba345f8be74590ca5453b3ec5d
'2012-05-16T12:26:58-04:00'
describe
'2035' 'info:fdaE20100110_AAACDPfileF20100110_AABPNQ' 'sip-files00088.txt'
50e4673db2a8b16e1f8fb3fcc3a47b2d
eec7abba1ff9dc9a5f99c742b9ab7a2c7a49407d
'2012-05-16T12:18:15-04:00'
describe
'44186' 'info:fdaE20100110_AAACDPfileF20100110_AABPNR' 'sip-files00088thm.jpg'
2b6231e4826e6509e0e8cb790c5f9aac
073acc12cff4938fe9367d49513b2e05a36d1fd4
describe
'511730' 'info:fdaE20100110_AAACDPfileF20100110_AABPNS' 'sip-files00089.jp2'
b83d508cf0eb77e9d935a21e8ca36bcb
fed04f3ae1fecc1b04d34f97ae9e817ea9bf6ece
'2012-05-16T12:24:59-04:00'
describe
'398168' 'info:fdaE20100110_AAACDPfileF20100110_AABPNT' 'sip-files00089.jpg'
097bc75b8e9efa62a7212747049194a0
640d2c1ecd08d972183771af658a7573dff59bfc
describe
'31067' 'info:fdaE20100110_AAACDPfileF20100110_AABPNU' 'sip-files00089.pro'
661ec97c6163b7dc89256752bf3ee87e
14f48e7138e0bb5fbf13eec46ea2a6e6c58af326
describe
'121888' 'info:fdaE20100110_AAACDPfileF20100110_AABPNV' 'sip-files00089.QC.jpg'
c46956e5c3c2a09c4e3f357c6277d007
07f568a4aadb3b1b071905e579c66c1ba97e47b2
'2012-05-16T12:18:20-04:00'
describe
'4096630' 'info:fdaE20100110_AAACDPfileF20100110_AABPNW' 'sip-files00089.tif'
2a9d727c126ad8be6de3435e8f5ef666
c1590e49b1fe74496953c5402d6082daf258107a
'2012-05-16T12:25:36-04:00'
describe
'1342' 'info:fdaE20100110_AAACDPfileF20100110_AABPNX' 'sip-files00089.txt'
c14cb69ffe54316374feb59fa5e260bc
f2c8ea62fc757cb08a7138b18af18a061d2607cb
'2012-05-16T12:21:00-04:00'
describe
'40450' 'info:fdaE20100110_AAACDPfileF20100110_AABPNY' 'sip-files00089thm.jpg'
e9a85643f8d7c03ebab34fcc20c6fe0d
cd000f08727f499b46b407a9bbc41c9634f37ecb
describe
'506423' 'info:fdaE20100110_AAACDPfileF20100110_AABPNZ' 'sip-files00090.jp2'
021d973f11c7902b5657b82ef5786531
2a807f3cd411987314152e8aa92c1cde954f45a8
describe
'489732' 'info:fdaE20100110_AAACDPfileF20100110_AABPOA' 'sip-files00090.jpg'
fd73c7d6431987af7562b87daa00a877
f50e9fb7ecbb0b0597f1f860bf689d439ef7e935
'2012-05-16T12:18:42-04:00'
describe
'52964' 'info:fdaE20100110_AAACDPfileF20100110_AABPOB' 'sip-files00090.pro'
895452f6cc9086ff90d72a64af5c6cdb
13a1a3a115330302019f2056dd54452543f87c0f
describe
'152939' 'info:fdaE20100110_AAACDPfileF20100110_AABPOC' 'sip-files00090.QC.jpg'
c72d0845ce59c2ca04795bc95e140a58
cb3f8d94c60b1a13c7e77e3260d0ed620d4171a5
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPOD' 'sip-files00090.tif'
4fd16d8d80920e2005df6993aa267a4a
d4029bce0ea54b7d94909fff8b0e14d44d95d184
'2012-05-16T12:23:07-04:00'
describe
'2160' 'info:fdaE20100110_AAACDPfileF20100110_AABPOE' 'sip-files00090.txt'
92cb5bdbd6a8fcbe1079e78498083143
2a6925e794b5842026fd3452cbe96fb0b217fb59
describe
'45718' 'info:fdaE20100110_AAACDPfileF20100110_AABPOF' 'sip-files00090thm.jpg'
d0027c45988d5340846129e7b5b77f06
57576b0050d67f3c8d0831d4562d2ecc6087d6a5
describe
'483639' 'info:fdaE20100110_AAACDPfileF20100110_AABPOG' 'sip-files00091.jp2'
4ea9fdd82486e96309e380914f70b353
a01165789e053c2a562cfd5ffce4e2302a50470f
describe
'489149' 'info:fdaE20100110_AAACDPfileF20100110_AABPOH' 'sip-files00091.jpg'
1492d84521c5d0812960763f9f27e138
a327d030ca882feab870bb64987f3e607ffc5068
describe
'47494' 'info:fdaE20100110_AAACDPfileF20100110_AABPOI' 'sip-files00091.pro'
79fb95f926a6e781aea6c573f766bda4
270f46e67d0c13c23841756c19c2f4d97b00ce09
describe
'150812' 'info:fdaE20100110_AAACDPfileF20100110_AABPOJ' 'sip-files00091.QC.jpg'
3d3b6ed0c1f4e27e8a1f2eb18b624091
a71ae6d46fad8693e5eabc4ce1d07d143f6622c8
'2012-05-16T12:27:19-04:00'
describe
'3871706' 'info:fdaE20100110_AAACDPfileF20100110_AABPOK' 'sip-files00091.tif'
9a494e8ce515ea271c11339be3b35535
6aae439d306989ef26274dae343e75fa1edd8345
'2012-05-16T12:20:33-04:00'
describe
'1995' 'info:fdaE20100110_AAACDPfileF20100110_AABPOL' 'sip-files00091.txt'
1782fe1255ebe6a672564f49c5b9c9ca
ec546773203e60da85c421c9b71ff10847c50047
'2012-05-16T12:24:21-04:00'
describe
'43805' 'info:fdaE20100110_AAACDPfileF20100110_AABPOM' 'sip-files00091thm.jpg'
c3c4a434cc3954c0d78d54dd6e187fee
b3fe0138682a6cf14c7a8bd6d3e112bf6a4da1c1
'2012-05-16T12:19:03-04:00'
describe
'475147' 'info:fdaE20100110_AAACDPfileF20100110_AABPON' 'sip-files00092.jp2'
53dc1c30679fe90fc9545fb3c47425f7
a680ebc35f7cbcc2b7ffdc448a31f649dedbcc5e
'2012-05-16T12:23:18-04:00'
describe
'234937' 'info:fdaE20100110_AAACDPfileF20100110_AABPOO' 'sip-files00092.jpg'
f958d6251bd7cb9df5f8780e7a84f81c
e4f973dc704fe0583fb249b910fa558d720b9150
describe
'3383' 'info:fdaE20100110_AAACDPfileF20100110_AABPOP' 'sip-files00092.pro'
af7c0e81f7563cf258a6cc1910386532
93f1b240f0e05d8cafd0358a5f45bab883af8989
'2012-05-16T12:19:31-04:00'
describe
'67369' 'info:fdaE20100110_AAACDPfileF20100110_AABPOQ' 'sip-files00092.QC.jpg'
857d8e6d27a6e5f1109d56a303bb0bb3
2fe3c135cfff38819f459dbe9b366db903ff042d
'2012-05-16T12:25:45-04:00'
describe
'3805916' 'info:fdaE20100110_AAACDPfileF20100110_AABPOR' 'sip-files00092.tif'
739f0ea729709bc187373bfcf572306b
58133536ec282db2d5e6077fd4a7a5aa4d8d717e
describe
'167' 'info:fdaE20100110_AAACDPfileF20100110_AABPOS' 'sip-files00092.txt'
579c47f01f518560a82ab451c0a0bc84
0628deb7c06cf5b4a8a9896fe19b4a1344bb78a7
'2012-05-16T12:27:04-04:00'
describe
'20420' 'info:fdaE20100110_AAACDPfileF20100110_AABPOT' 'sip-files00092thm.jpg'
a403468ca9db4e6d2bc5a28942fa8369
59a919f5173a1e12a91d96a43ef8a52d2161b91e
describe
'514227' 'info:fdaE20100110_AAACDPfileF20100110_AABPOU' 'sip-files00093.jp2'
6a0800091d142eafb40919323272eb40
09b535ad41076718cd632a777b86f53a0bd80fb6
'2012-05-16T12:26:16-04:00'
describe
'344407' 'info:fdaE20100110_AAACDPfileF20100110_AABPOV' 'sip-files00093.jpg'
699ff8e94e9b4ce0bcaa904926146505
a0408402ab0906849fe792d0f8cfc2245c990141
describe
'42387' 'info:fdaE20100110_AAACDPfileF20100110_AABPOW' 'sip-files00093.pro'
41d67fcf068daf7aab7d0e81964fdae2
07e7bef5f7b501af528858111f6d86cab689d10a
describe
'110992' 'info:fdaE20100110_AAACDPfileF20100110_AABPOX' 'sip-files00093.QC.jpg'
abb0120f64e66149973d5f0b958cb046
fe82ab39e2a301b9bc26c782a7ad7288c96cad75
'2012-05-16T12:18:55-04:00'
describe
'4116378' 'info:fdaE20100110_AAACDPfileF20100110_AABPOY' 'sip-files00093.tif'
d35f25e00614b468217e483e1ca56b73
f278a6492b3188fc28a9278a0b19a431cebd857b
'2012-05-16T12:23:13-04:00'
describe
'1997' 'info:fdaE20100110_AAACDPfileF20100110_AABPOZ' 'sip-files00093.txt'
436a7a8577f38df3cabbaac13e18eb15
bbe23e5ac03330855522e9bb005d4e4f054ee351
'2012-05-16T12:24:37-04:00'
describe
'37168' 'info:fdaE20100110_AAACDPfileF20100110_AABPPA' 'sip-files00093thm.jpg'
1ca06d615e3cf0ff245515e22da834f4
ebb796be26895ab6c5b6da6e03dcc25a92baca24
'2012-05-16T12:18:33-04:00'
describe
'520155' 'info:fdaE20100110_AAACDPfileF20100110_AABPPB' 'sip-files00094.jp2'
e7349c2d59487f3f7c6e0230aee02349
1220da4cb95edb29c9247e8f3a55c014831b63fa
describe
'400655' 'info:fdaE20100110_AAACDPfileF20100110_AABPPC' 'sip-files00094.jpg'
c72aa597a7fb529a497ea6eb187ba80b
3b21dd4f7df3cfdd308126eab1f87a68415c7a58
'2012-05-16T12:19:39-04:00'
describe
'56312' 'info:fdaE20100110_AAACDPfileF20100110_AABPPD' 'sip-files00094.pro'
1f06d54bef698ac178dc5cf8bcc60c1e
84c8a48e74abc90446e3aeb46212de7d7c90f898
describe
'130251' 'info:fdaE20100110_AAACDPfileF20100110_AABPPE' 'sip-files00094.QC.jpg'
b0290c3fa8ec7dd21c90d7d066e0e3ce
2573e17f6c454f7f82adb68f90e0e13fc22d34c2
'2012-05-16T12:24:45-04:00'
describe
'4163910' 'info:fdaE20100110_AAACDPfileF20100110_AABPPF' 'sip-files00094.tif'
0bee9b23ae706a77ce50c490ab6878e2
7e38b0464ff2c491d40f5f71db5a2ec982df7ae3
'2012-05-16T12:26:50-04:00'
describe
'2727' 'info:fdaE20100110_AAACDPfileF20100110_AABPPG' 'sip-files00094.txt'
b3ab3396b1b8e9d3314c4a02711654f3
8ff8080b037ccc88b43651ecdcc6c5c82b9636aa
describe
Invalid character
'info:fdaE20100110_AAACDPfileF20100110_AABPPH' 'sip-files00094thm.jpg'
bdd6403d32313d7c3a398aabfad7de94
7170da47171e07b6066efcf79342bd37620505b3
describe
'520169' 'info:fdaE20100110_AAACDPfileF20100110_AABPPI' 'sip-files00095.jp2'
35491c61986398aee5a290edc593ed91
5fc39f23ffc32c2c239db11f3ddb30d57a3f2e89
describe
'373556' 'info:fdaE20100110_AAACDPfileF20100110_AABPPJ' 'sip-files00095.jpg'
343df1d7aad41eb499fb319dc41aa52b
98ca5725249513b4ad62bb4d5a982aeeaeef59ac
'2012-05-16T12:22:10-04:00'
describe
'47490' 'info:fdaE20100110_AAACDPfileF20100110_AABPPK' 'sip-files00095.pro'
7651905792c5ddaf21bf67e7ed0e990c
a9becd132656ad85bdb10d244a2ef63c415de9d8
describe
'121805' 'info:fdaE20100110_AAACDPfileF20100110_AABPPL' 'sip-files00095.QC.jpg'
3a87bffb26f8017611c2d2cf54099c8b
3174fe8f57c031c29fa27ceca25e15dc8f04773b
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPPM' 'sip-files00095.tif'
80d2548817f66289d3c535d3b3e4ee2f
e957d092a9a22c4fa619f5be874975ba379d2f7a
'2012-05-16T12:22:22-04:00'
describe
'2069' 'info:fdaE20100110_AAACDPfileF20100110_AABPPN' 'sip-files00095.txt'
7e1348d17a4203e93fb6ea9b3423860f
c382fad1ef1ebe08b93ede453ba94a85e5cbed31
'2012-05-16T12:22:59-04:00'
describe
'39108' 'info:fdaE20100110_AAACDPfileF20100110_AABPPO' 'sip-files00095thm.jpg'
7fff53ea22b6a6a33b556bc1e007c5f8
ab51ebded785eea991a8e080b0719775689cd22a
describe
'508162' 'info:fdaE20100110_AAACDPfileF20100110_AABPPP' 'sip-files00096.jp2'
694bbc4b88211d8e025c2e4528b4a0f5
311c38b12101422f30bbdf4e1a0159919e89ef42
describe
'349729' 'info:fdaE20100110_AAACDPfileF20100110_AABPPQ' 'sip-files00096.jpg'
068b1f60f87422628fc6b557b1402dc0
d6d5bbc399dcaefcd6a2fd0c11f2f2e61db1a62e
describe
'37795' 'info:fdaE20100110_AAACDPfileF20100110_AABPPR' 'sip-files00096.pro'
391fa74ef8cf40bdf1ce63c775d22e5c
7cbcc54de0979b0c562ed0e396e6a2f6ac8dfaf5
describe
'112134' 'info:fdaE20100110_AAACDPfileF20100110_AABPPS' 'sip-files00096.QC.jpg'
e1267084112c81b522cb5354429cbaac
e15a7f2f153770f9223a22049ec3a0c81f605198
describe
'4069646' 'info:fdaE20100110_AAACDPfileF20100110_AABPPT' 'sip-files00096.tif'
da2645d126a42d06476817059f6c152f
e5f99eb7c89d3c42f4ec9ba5f7c477e2442f60d4
describe
'1771' 'info:fdaE20100110_AAACDPfileF20100110_AABPPU' 'sip-files00096.txt'
fc2583f2df56d6713ee0be6a9513265d
71b61a1d597974b2ac06372c0ff47b0b154383c8
describe
'35154' 'info:fdaE20100110_AAACDPfileF20100110_AABPPV' 'sip-files00096thm.jpg'
a652d5bfba9a34428d1d0ca5697ff047
368d0b93cc7b231356d1a0f60c81a50c4f60efdf
describe
'522763' 'info:fdaE20100110_AAACDPfileF20100110_AABPPW' 'sip-files00097.jp2'
d774b364dad4d27cef5070bb3c65b2da
0ca9c28cc605259364090e49561a2cedd2fb18c5
describe
'365949' 'info:fdaE20100110_AAACDPfileF20100110_AABPPX' 'sip-files00097.jpg'
71f10d95653d970f17e76f132b013efe
427b2602023dd9ee0ae8d2f6d623f131a41385a8
'2012-05-16T12:26:49-04:00'
describe
'38006' 'info:fdaE20100110_AAACDPfileF20100110_AABPPY' 'sip-files00097.pro'
3541131a2eaa664ccc882a827fa198dd
c30625f5523b8006b424b43cfca7d0c684236b62
describe
'114394' 'info:fdaE20100110_AAACDPfileF20100110_AABPPZ' 'sip-files00097.QC.jpg'
a38dddb3d0285adfb89de1ec5a3c721d
d6e44a5c599f9940ba0672224fc605bcfa7d8808
'2012-05-16T12:23:25-04:00'
describe
'4184646' 'info:fdaE20100110_AAACDPfileF20100110_AABPQA' 'sip-files00097.tif'
96e7dc994ec5b0bdc87c91a89888fdfd
244645d96fb40da4ed683e21f7dc1340bad7ce44
'2012-05-16T12:28:33-04:00'
describe
'1781' 'info:fdaE20100110_AAACDPfileF20100110_AABPQB' 'sip-files00097.txt'
b90d72161d7a35d832e43478c4a7c00c
e85b9ce6de074f67573c9db032115a2a30ee5fa6
describe
'35975' 'info:fdaE20100110_AAACDPfileF20100110_AABPQC' 'sip-files00097thm.jpg'
efd1171e8874301937dc5a670c4aea5d
4b59b058ae94d683057c6a9aa079619082f459d7
describe
'495550' 'info:fdaE20100110_AAACDPfileF20100110_AABPQD' 'sip-files00098.jp2'
e899025339190523bd8c3d4f6378a714
ac26981e39fd4da6955cd8e8ea794a13eeb52577
describe
'417901' 'info:fdaE20100110_AAACDPfileF20100110_AABPQE' 'sip-files00098.jpg'
d0632ae63366924b524ec3fb9bfb380d
4837deab6bb436a3f9e8ad81939946cfe316afb1
'2012-05-16T12:24:49-04:00'
describe
'41865' 'info:fdaE20100110_AAACDPfileF20100110_AABPQF' 'sip-files00098.pro'
14a89345b95badfe595f4193ab573d6f
2bd88f810e33b88aa502743b0c814f9e01ea5b1d
'2012-05-16T12:23:30-04:00'
describe
'126499' 'info:fdaE20100110_AAACDPfileF20100110_AABPQG' 'sip-files00098.QC.jpg'
7f9b030d4f75a66915695d79e569b84b
569cd5675a7cc3b81c006c2811f4ce3fbadaee80
'2012-05-16T12:19:23-04:00'
describe
'3968556' 'info:fdaE20100110_AAACDPfileF20100110_AABPQH' 'sip-files00098.tif'
bb56130c1e7c24953b90f62ad8a8b434
61d09bdf40c63b4a4b872c898edb9cd2ccee586f
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPQI' 'sip-files00098.txt'
295fdb2b83eb5858baa439dae487009a
4f74329602224ef76393e5b025bee60e6805b22a
describe
'37267' 'info:fdaE20100110_AAACDPfileF20100110_AABPQJ' 'sip-files00098thm.jpg'
9d0a7ef35261d1d51f862e0f3a9b673d
4eda57db96967e5ff9279a36c00ff817b6771885
describe
'517132' 'info:fdaE20100110_AAACDPfileF20100110_AABPQK' 'sip-files00099.jp2'
33ea8ef7dcc46ade92eef29525320fa4
750035277a6dfed76395e402f9bef6c256fbafb4
describe
'417629' 'info:fdaE20100110_AAACDPfileF20100110_AABPQL' 'sip-files00099.jpg'
9b66f2c7d78ad59f7c61f07e35c295ab
6cb8482a277315fbc6b319a0c41cabe57520ca08
describe
'48708' 'info:fdaE20100110_AAACDPfileF20100110_AABPQM' 'sip-files00099.pro'
89e23e5497408e81c00ebab352b3a035
829969107bf9ad356c5bfea17b6b1d4720ac7a1f
describe
'125684' 'info:fdaE20100110_AAACDPfileF20100110_AABPQN' 'sip-files00099.QC.jpg'
b55847f726314ce9b304e95b041d28fd
dfaceb1ddfcb033b93724c83b3f860d323bcc473
describe
'4139718' 'info:fdaE20100110_AAACDPfileF20100110_AABPQO' 'sip-files00099.tif'
6d5764f7d49f030a6f3af0c051a92e51
2b5c670893836067a8b42687d54b1576bd054775
'2012-05-16T12:21:34-04:00'
describe
'2498' 'info:fdaE20100110_AAACDPfileF20100110_AABPQP' 'sip-files00099.txt'
fb5a6b69bb777bfed74df9b4f72e2cde
69a80081f1c30be5e10e01f372ecc6d19db6a58a
'2012-05-16T12:26:57-04:00'
describe
Invalid character
'39756' 'info:fdaE20100110_AAACDPfileF20100110_AABPQQ' 'sip-files00099thm.jpg'
0ae82e26831a64dba3832ecefd29b736
23f166714df864c732c62f8bbbbc0159e0f931f0
describe
'517191' 'info:fdaE20100110_AAACDPfileF20100110_AABPQR' 'sip-files00100.jp2'
0825d65c6e98fe97b4ce90fd4b1de088
9dd42e430002d4c7a8ba22b31fcbcd07e656a3d7
describe
'479732' 'info:fdaE20100110_AAACDPfileF20100110_AABPQS' 'sip-files00100.jpg'
b80cbe8e0dbacb0e73e10124e668a5b5
cde2f04ee4fb6fdda888f00300b8228c52b39833
describe
'62645' 'info:fdaE20100110_AAACDPfileF20100110_AABPQT' 'sip-files00100.pro'
a4bbd874df0e7bd6c8293e3c306ad388
71e1feab683d8afcbc0dfae575e936c93497c40b
describe
'146958' 'info:fdaE20100110_AAACDPfileF20100110_AABPQU' 'sip-files00100.QC.jpg'
b2c150352cb94b96afef43145f314a22
332b846c98a2799e110f3b6929fc37594188cbc9
describe
'4140220' 'info:fdaE20100110_AAACDPfileF20100110_AABPQV' 'sip-files00100.tif'
47b07a915538b2165fbeea39eb1ffa59
07f5f9788626c911c83cca767e123bedf3606d22
'2012-05-16T12:21:36-04:00'
describe
'3024' 'info:fdaE20100110_AAACDPfileF20100110_AABPQW' 'sip-files00100.txt'
d5cdaab9a4c9a9308459fd11bd500522
9ef90e6373391482ccce34994282ffdec2262d1e
describe
Invalid character
'43201' 'info:fdaE20100110_AAACDPfileF20100110_AABPQX' 'sip-files00100thm.jpg'
ed0ced7e4d4bfb6c0fcb12d407168017
18ca4dc2da4931a9d7c2e06812cd2eac3b1a2934
describe
'516507' 'info:fdaE20100110_AAACDPfileF20100110_AABPQY' 'sip-files00101.jp2'
3cd70db3c6a85a6a6033441d9ba4929e
1fc00e38f45ece8b13baa96abfd7361e06103708
'2012-05-16T12:22:27-04:00'
describe
'360774' 'info:fdaE20100110_AAACDPfileF20100110_AABPQZ' 'sip-files00101.jpg'
fbe547a6dbfc28334980de8caf4b9967
88d36c184f0017bb69b5a0ca7b7ee3c2b7908bdb
describe
'46498' 'info:fdaE20100110_AAACDPfileF20100110_AABPRA' 'sip-files00101.pro'
d9b236924400cd8acab490871a941a4c
bde191434e385c9723c705a7ae548cb96b734b37
describe
'118502' 'info:fdaE20100110_AAACDPfileF20100110_AABPRB' 'sip-files00101.QC.jpg'
0a69b1b89442124ee9251a26f1befc4f
06f73111169413355796f7c8607005a39e30a7f4
'2012-05-16T12:25:30-04:00'
describe
'4134994' 'info:fdaE20100110_AAACDPfileF20100110_AABPRC' 'sip-files00101.tif'
26a9bbdcb219503287674afc3a6aa83b
4b3f40bc1631b9a972507a1b93c7f60bd6bff0e6
describe
'2376' 'info:fdaE20100110_AAACDPfileF20100110_AABPRD' 'sip-files00101.txt'
6752c56d71a9a801aa0c83e7e60bc637
eeb858e82a15548bbddbf1499c9249f048eeafb3
describe
'38194' 'info:fdaE20100110_AAACDPfileF20100110_AABPRE' 'sip-files00101thm.jpg'
27ef84481751a80d3c75a173a0b55210
1a1f910ac9e4ea2cd222fe378d6198a50b8a99da
describe
'513900' 'info:fdaE20100110_AAACDPfileF20100110_AABPRF' 'sip-files00102.jp2'
14a31302029e419fc2e128736401f655
b450f62db109feb0d02d544807988b1a469f77ae
'2012-05-16T12:22:19-04:00'
describe
'367432' 'info:fdaE20100110_AAACDPfileF20100110_AABPRG' 'sip-files00102.jpg'
cb36574d8c7104d17e4cf196455974f2
ebf7558ad0919bb3e48145037651dacf2554d3b0
describe
'38509' 'info:fdaE20100110_AAACDPfileF20100110_AABPRH' 'sip-files00102.pro'
b0a35069264757a6a5b57b33f83342d7
cc29108e866472b71daf0b426bf94349fbc997ad
describe
'113757' 'info:fdaE20100110_AAACDPfileF20100110_AABPRI' 'sip-files00102.QC.jpg'
f6c36e59d2b1cedfbf944845f7c63858
cc02c087831eef0b5a03d05b1c4cab75c23dbba0
describe
'4114120' 'info:fdaE20100110_AAACDPfileF20100110_AABPRJ' 'sip-files00102.tif'
055102236ba623e23ea341c37b357968
29b99644891758ab53080a82e61df547a526aa2c
'2012-05-16T12:23:52-04:00'
describe
'1824' 'info:fdaE20100110_AAACDPfileF20100110_AABPRK' 'sip-files00102.txt'
911a16954840a050d747db5d91f83a43
8d6b6f16706b84df586d1dd600f88a74e6f9b1cf
describe
'35444' 'info:fdaE20100110_AAACDPfileF20100110_AABPRL' 'sip-files00102thm.jpg'
2dada85c119edf74b4342cf16ed34046
76597c5bea986f0506ade4172921b143ca7a601f
describe
'502052' 'info:fdaE20100110_AAACDPfileF20100110_AABPRM' 'sip-files00103.jp2'
2b879ffae005b09c69a80d072358ec31
0a5979e9b7f3555c6f68c88a13f4225ebfe41783
'2012-05-16T12:21:51-04:00'
describe
'377755' 'info:fdaE20100110_AAACDPfileF20100110_AABPRN' 'sip-files00103.jpg'
0e0c4ffaf7be885a7c99dda970483d5e
bdef453d8c8599c43071cc0d35a0052d4be85acc
describe
'41388' 'info:fdaE20100110_AAACDPfileF20100110_AABPRO' 'sip-files00103.pro'
93cfccda8fee7dd1820a0cd9fd5b3b1c
49e0bc80a3ff1251a9fe60a64b958dceb2f33a16
'2012-05-16T12:24:55-04:00'
describe
'116665' 'info:fdaE20100110_AAACDPfileF20100110_AABPRP' 'sip-files00103.QC.jpg'
862cf910f8314a201e4b10649208f686
8c5854a7b1bc03070b50d0f2f90fb3137098645b
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPRQ' 'sip-files00103.tif'
3dc40ea103b8f8d6b3c75e3b962538b2
4f896f3724c06290162bcc7b9438bcf905755618
'2012-05-16T12:26:41-04:00'
describe
'1874' 'info:fdaE20100110_AAACDPfileF20100110_AABPRR' 'sip-files00103.txt'
21148c5401c69e24be813901311c7c47
39566bdf8d33a52d5618b6895e8e47b0204b0f62
describe
'38404' 'info:fdaE20100110_AAACDPfileF20100110_AABPRS' 'sip-files00103thm.jpg'
6942e1fba4fca81458712269672db711
64c405c42dd5329253936abe2fb2640db1cc994a
'2012-05-16T12:18:54-04:00'
describe
'515569' 'info:fdaE20100110_AAACDPfileF20100110_AABPRT' 'sip-files00104.jp2'
9c3f4066e109b03c836fd5dc2a5e1003
04d4680fc294a6a56f020234acd4a4587583e487
'2012-05-16T12:21:29-04:00'
describe
'400817' 'info:fdaE20100110_AAACDPfileF20100110_AABPRU' 'sip-files00104.jpg'
a61ce74b567d14a979a315206ab14fe2
0cbdc64de2f255f8a2db689409a3b48a7d533d15
describe
'48499' 'info:fdaE20100110_AAACDPfileF20100110_AABPRV' 'sip-files00104.pro'
1a38ddbcf6164bd3a621a16c6fe1aee2
6db74a80fc41eb5e8b4d0bf255ae4f82e01d9895
'2012-05-16T12:22:40-04:00'
describe
'124788' 'info:fdaE20100110_AAACDPfileF20100110_AABPRW' 'sip-files00104.QC.jpg'
66ffebb0cf8b6ede184affd3dba64b3c
95f77a34cc26b224ee9ab3ee4ff5bd2f051fba9a
describe
'4127170' 'info:fdaE20100110_AAACDPfileF20100110_AABPRX' 'sip-files00104.tif'
8a5f014b2472812f1380a1d8aa6aba33
b5a758f43791f1794443306802fc35bbd5d68d32
'2012-05-16T12:27:15-04:00'
describe
'2374' 'info:fdaE20100110_AAACDPfileF20100110_AABPRY' 'sip-files00104.txt'
df60c2327059259a0d89f6a40337e841
9431390ed2555a5720ff3a72755bbeedaf4ec829
describe
'38266' 'info:fdaE20100110_AAACDPfileF20100110_AABPRZ' 'sip-files00104thm.jpg'
95faad17cdec835e4d2cefe8026b8c27
3d9842405f1e71c555d0740db6c2c8056a7b4b05
describe
'501258' 'info:fdaE20100110_AAACDPfileF20100110_AABPSA' 'sip-files00105.jp2'
70c12da3d15bcff2ba8b218a4086f9d6
b94271d47f4f1b5f85073271bd22b84b853ad577
describe
'389454' 'info:fdaE20100110_AAACDPfileF20100110_AABPSB' 'sip-files00105.jpg'
551689fca214bca6ab016965fdda2e2e
fd536572634fbc7fc22cf420b19b43afb95b374b
describe
'43851' 'info:fdaE20100110_AAACDPfileF20100110_AABPSC' 'sip-files00105.pro'
de19fca327b9226d90086e515e562a3d
8040da7a4b20b1aef408f3e68e00799b79caa2e7
describe
'120883' 'info:fdaE20100110_AAACDPfileF20100110_AABPSD' 'sip-files00105.QC.jpg'
be5b315be808898cb496718f73f0338d
4ab6c6444fae0c062b178736037d6bb08e90cf33
'2012-05-16T12:18:43-04:00'
describe
'4012530' 'info:fdaE20100110_AAACDPfileF20100110_AABPSE' 'sip-files00105.tif'
6f2acde142b72f447a466257b6495e61
db3aac899f7d169de7d56d1caf87f724a33ea9ca
describe
'2077' 'info:fdaE20100110_AAACDPfileF20100110_AABPSF' 'sip-files00105.txt'
da28f9b41a26093e5a17d62150c50b87
238217a25e5026ce78b61356d1a915e7c8d576f0
'2012-05-16T12:28:16-04:00'
describe
'36078' 'info:fdaE20100110_AAACDPfileF20100110_AABPSG' 'sip-files00105thm.jpg'
b58da5da03df5bbf71f7f68b74be0f51
181c3e0caa6b1974fee89826090c08a527740a4f
'2012-05-16T12:22:06-04:00'
describe
'496294' 'info:fdaE20100110_AAACDPfileF20100110_AABPSH' 'sip-files00106.jp2'
079621b30ad1a7bdb838952c40b3a6b7
cd4f82baefc7f7078f39c3e44c114886c598dd52
describe
'354305' 'info:fdaE20100110_AAACDPfileF20100110_AABPSI' 'sip-files00106.jpg'
8a5fc058b7a4f310858d15e4302b781e
4c625f6b4bf57f07e1cbae6fde248deb67066867
'2012-05-16T12:23:41-04:00'
describe
'36022' 'info:fdaE20100110_AAACDPfileF20100110_AABPSJ' 'sip-files00106.pro'
3caee2a825690947f12b52c24b4cb863
78cf41e3964f79b043d1016a93aae80bfed90271
describe
'114579' 'info:fdaE20100110_AAACDPfileF20100110_AABPSK' 'sip-files00106.QC.jpg'
35073dca3e0e0643f6e58d8dd6dcd778
6e85459e86cb17ac4e05c4066b2a782a8c6a8f19
'2012-05-16T12:22:41-04:00'
describe
'3973506' 'info:fdaE20100110_AAACDPfileF20100110_AABPSL' 'sip-files00106.tif'
f38ade8fdb813056ffec6ce754444660
70b1b09c037345ed80e19f21bb161a64c5dac4b6
'2012-05-16T12:28:27-04:00'
describe
'1827' 'info:fdaE20100110_AAACDPfileF20100110_AABPSM' 'sip-files00106.txt'
e196f45e02657c720a9bf9afb60edc80
374d1dd36ff081782431f11add3a35bef9b8716f
'2012-05-16T12:18:58-04:00'
describe
'33596' 'info:fdaE20100110_AAACDPfileF20100110_AABPSN' 'sip-files00106thm.jpg'
3e4b7b29dea6660c072085a586b0e5e5
1f5822b3b6225e99e8c5557d1be7b45acbfebf5b
describe
'514262' 'info:fdaE20100110_AAACDPfileF20100110_AABPSO' 'sip-files00107.jp2'
7a963a6949b368cf5cfe9d88155d7f26
61645f554e5accbb863e127cd1abfedee3afab81
describe
'394748' 'info:fdaE20100110_AAACDPfileF20100110_AABPSP' 'sip-files00107.jpg'
d7011a25d80b93bbaa1c41a36f507a1e
120a64c705aa3d9500d97e75bd140fe21e369f3c
describe
'44145' 'info:fdaE20100110_AAACDPfileF20100110_AABPSQ' 'sip-files00107.pro'
46a0f1e07547fbe476f1c6a0a0ea2ac9
15da1cc724c01a9188b0344ebe3ed63ebbe309a5
describe
'119556' 'info:fdaE20100110_AAACDPfileF20100110_AABPSR' 'sip-files00107.QC.jpg'
3757eddd47a6694ded94e2ef45b02dd3
040d8b970eba4d5826208837e32a09aa81cd766f
'2012-05-16T12:24:47-04:00'
describe
'4116778' 'info:fdaE20100110_AAACDPfileF20100110_AABPSS' 'sip-files00107.tif'
69a448b5a2efbd5c917c56154f613fcc
ef070c096fd6e8bae0b4f7466ef5588f68483c87
'2012-05-16T12:23:20-04:00'
describe
'2211' 'info:fdaE20100110_AAACDPfileF20100110_AABPST' 'sip-files00107.txt'
db5bea7b23c00427f4c964b0f76c27b2
911b07ec938801673d1269fd7881789427a99634
describe
'38462' 'info:fdaE20100110_AAACDPfileF20100110_AABPSU' 'sip-files00107thm.jpg'
687ef415afe661fda27706f3e66e1dc5
1be2c5b58caff4f9a1f1e5e44e61f35894afde09
'2012-05-16T12:21:42-04:00'
describe
'508052' 'info:fdaE20100110_AAACDPfileF20100110_AABPSV' 'sip-files00108.jp2'
7a5223ac58f94a963d7e925d61f32bbc
463b2f0af51172cb5c8e6cb4d9decf82bac77315
describe
'378382' 'info:fdaE20100110_AAACDPfileF20100110_AABPSW' 'sip-files00108.jpg'
aadd96e6333eb129ea925f6a067713a9
dfa26daab2524811d85bcb70105e57b3fb4b4e9d
'2012-05-16T12:18:25-04:00'
describe
'37836' 'info:fdaE20100110_AAACDPfileF20100110_AABPSX' 'sip-files00108.pro'
0ae54079c5ffa3fdbdee5218feca9fb2
654a0bf923b9249be1b7b09aa292b598a2993710
describe
'115556' 'info:fdaE20100110_AAACDPfileF20100110_AABPSY' 'sip-files00108.QC.jpg'
1da4fe62c18ae6f2e70cfa127b0b0299
6063b5f9d292f7094e9769db2271ca09f88881a0
describe
'4067162' 'info:fdaE20100110_AAACDPfileF20100110_AABPSZ' 'sip-files00108.tif'
b07496968394384430d47ac24116562a
07ae349c42a6b0638d269d76ad5834762479f312
describe
'1766' 'info:fdaE20100110_AAACDPfileF20100110_AABPTA' 'sip-files00108.txt'
a2a0353fed839b43ad6c37a00f37ef5d
82e3f42d8c462bd2f2ee8eb26a5a4d16ad654373
describe
'36518' 'info:fdaE20100110_AAACDPfileF20100110_AABPTB' 'sip-files00108thm.jpg'
0733dad46f1f4f34659e7a77fddbd20f
f6babe49e26a2bf8ffc413ab00ed637cb644106c
'2012-05-16T12:20:50-04:00'
describe
'504131' 'info:fdaE20100110_AAACDPfileF20100110_AABPTC' 'sip-files00109.jp2'
478e6a06cb86f17ff0f378ce61e09163
dc9039ad65f4a380af4c7471d60ec8a1fe5f3a69
describe
'377071' 'info:fdaE20100110_AAACDPfileF20100110_AABPTD' 'sip-files00109.jpg'
c8801dfeec4ca5f2e5fb3f14ca57c708
b6204864449c533cc4bee533b56d5481d57153ec
describe
'44422' 'info:fdaE20100110_AAACDPfileF20100110_AABPTE' 'sip-files00109.pro'
84ed3dee782df4abb54b5ef6b5717ba7
cb24b6281eb8918172d3fd982ba5e77b8c1103ef
describe
'119670' 'info:fdaE20100110_AAACDPfileF20100110_AABPTF' 'sip-files00109.QC.jpg'
f6ff04ff819bb005556f7e05eb965d68
0f4a77bf31fc340f7cd162ed34802ee16fe0b09b
describe
'4035946' 'info:fdaE20100110_AAACDPfileF20100110_AABPTG' 'sip-files00109.tif'
82dcaa1761265eb705fd8f8a67d8a3c0
3a6b87dd55a921fe078c4b059190831f857d3f26
'2012-05-16T12:27:38-04:00'
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPTH' 'sip-files00109.txt'
b2ccfc16c02825788ac2058d7eb3c8c8
cbb7ddfb4f8f89f398bf9b6581d8dddc101023fa
describe
'36129' 'info:fdaE20100110_AAACDPfileF20100110_AABPTI' 'sip-files00109thm.jpg'
dc3b99d1346379cf0f28c1a07bf6cc00
63d04969d8588ee992be2d78aea2d25e620cf9a7
describe
'515219' 'info:fdaE20100110_AAACDPfileF20100110_AABPTJ' 'sip-files00110.jp2'
9d75f8515efc6d420ba6efc8dc7a6fc9
b7f1646079eb198d70ac65a22b68085433e6a4cb
describe
'366000' 'info:fdaE20100110_AAACDPfileF20100110_AABPTK' 'sip-files00110.jpg'
5adabdebe38d810fb2332c0180abb66f
3911fe6077449974e518d856c73f95c7ea6e0da4
'2012-05-16T12:23:29-04:00'
describe
'37537' 'info:fdaE20100110_AAACDPfileF20100110_AABPTL' 'sip-files00110.pro'
46e3fddd4ca0e51ccfe2c5e3ff77ec33
78131264d5c71acf9daf816b0139bb68889b276e
'2012-05-16T12:18:59-04:00'
describe
'115533' 'info:fdaE20100110_AAACDPfileF20100110_AABPTM' 'sip-files00110.QC.jpg'
ead4e83ad098826eab8891e44d43f15d
6b0d94e288c27024bcec95989d66b6c3dd5992af
describe
'4124354' 'info:fdaE20100110_AAACDPfileF20100110_AABPTN' 'sip-files00110.tif'
b8bca7bf5cb4502b039936be8411f86f
dc30a74dc001770f551d263f4902ab65289c4763
describe
'1672' 'info:fdaE20100110_AAACDPfileF20100110_AABPTO' 'sip-files00110.txt'
7ce4723a48f881235b8ac26fce543018
4933ac8b8dc3ba173a61f8b777285ad0754c49df
describe
'36090' 'info:fdaE20100110_AAACDPfileF20100110_AABPTP' 'sip-files00110thm.jpg'
4b54f01eef84e66d327ac248f84e292c
4d64eb2f570a51c8651815703ab5a6c5e3f5fa57
describe
'515783' 'info:fdaE20100110_AAACDPfileF20100110_AABPTQ' 'sip-files00111.jp2'
c73da3e57fdba658eca7ad31e2f33117
35879414344fad1aadf28641ea9017882e0e0998
'2012-05-16T12:20:29-04:00'
describe
'335348' 'info:fdaE20100110_AAACDPfileF20100110_AABPTR' 'sip-files00111.jpg'
47585f2e1edcb6cbe68a92987116fa6a
1d765b40728b4915b8954f1b6b273469160c8415
'2012-05-16T12:21:14-04:00'
describe
'37242' 'info:fdaE20100110_AAACDPfileF20100110_AABPTS' 'sip-files00111.pro'
554b61a70f90cdae69f5b203c59c0471
2e3492ee5add8e2e72452c743f1dc394433f6f6c
describe
'113201' 'info:fdaE20100110_AAACDPfileF20100110_AABPTT' 'sip-files00111.QC.jpg'
6b6ff8fc859260e8375f2a5df7bae651
1415aee89f258763402e7a06fb5b5cfdbfce6d21
'2012-05-16T12:20:58-04:00'
describe
'4129878' 'info:fdaE20100110_AAACDPfileF20100110_AABPTU' 'sip-files00111.tif'
bf1356461a5231dba8aadf01fc266ae8
07023b80b511e2e6902f22c4883f326e7424a717
'2012-05-16T12:28:07-04:00'
describe
'1709' 'info:fdaE20100110_AAACDPfileF20100110_AABPTV' 'sip-files00111.txt'
7cba1e60926bfa3fd5a8d6142c489aa2
859040f152533e49f799a082761e24907dfd4df3
describe
'33921' 'info:fdaE20100110_AAACDPfileF20100110_AABPTW' 'sip-files00111thm.jpg'
9ca49a2739d8d89d4bf0066ff38eb8d0
ff39be03cf726aaa7ff14da9adefc87d518384d1
describe
'490262' 'info:fdaE20100110_AAACDPfileF20100110_AABPTX' 'sip-files00112.jp2'
076356a907400c5ada5d2d35447e2a7c
090606a6e52917a5361c2861082c19bd58c4e90f
describe
'319359' 'info:fdaE20100110_AAACDPfileF20100110_AABPTY' 'sip-files00112.jpg'
4dd9d7868703a01486570cfdfd928caa
f106c8c25b4d2e38d9560f19c1c960810b3839e5
'2012-05-16T12:28:44-04:00'
describe
'24767' 'info:fdaE20100110_AAACDPfileF20100110_AABPTZ' 'sip-files00112.pro'
1d1eaad792bf414fbbaf233e3769e78f
ba220f98caafd4e97c9f5b5910d6799967184521
describe
'100267' 'info:fdaE20100110_AAACDPfileF20100110_AABPUA' 'sip-files00112.QC.jpg'
3ba7c1326128b614a85c48eaa4d3e8ff
4b52f9ecefe059a63cfb83af15d1f2579973a8eb
describe
'3925000' 'info:fdaE20100110_AAACDPfileF20100110_AABPUB' 'sip-files00112.tif'
941975e8ae762c3d74f39130f2814f5b
a1242d92e3f456882824a042e3d3d09210fce869
describe
'1173' 'info:fdaE20100110_AAACDPfileF20100110_AABPUC' 'sip-files00112.txt'
1044490b30636b8bba936e33e4d2b41a
a13ce9450fd94f55bec2358a9bbdb624c5102123
'2012-05-16T12:24:28-04:00'
describe
'28363' 'info:fdaE20100110_AAACDPfileF20100110_AABPUD' 'sip-files00112thm.jpg'
8b0c9fdc22adf8d71884b44aabf42d26
0b45f43d6377418fa3819b5e598498168fbe0845
describe
'480107' 'info:fdaE20100110_AAACDPfileF20100110_AABPUE' 'sip-files00113.jp2'
08ac8e4fc0bfe65e6492f8940abead03
98ed63e6f1ca2d6dd960d1b80468b4da1c6695c2
describe
'411683' 'info:fdaE20100110_AAACDPfileF20100110_AABPUF' 'sip-files00113.jpg'
f02de8d61c7de49229ce78fb1a75d34f
0f9b9b180eab838490738279ce6311a87b48682a
'2012-05-16T12:20:44-04:00'
describe
'50685' 'info:fdaE20100110_AAACDPfileF20100110_AABPUG' 'sip-files00113.pro'
f44ac705fb12670e9d6c037262757d68
416cded26a57ef45d19ab053ea76cd00d5272406
describe
'131508' 'info:fdaE20100110_AAACDPfileF20100110_AABPUH' 'sip-files00113.QC.jpg'
0ffce380ea13bdee0201fbc4561feec7
d406c6c7e33f76d2730b4b5899c339054bbb538a
'2012-05-16T12:20:56-04:00'
describe
'3843314' 'info:fdaE20100110_AAACDPfileF20100110_AABPUI' 'sip-files00113.tif'
9ee296969304bf9db843ac6e498230a1
17eabbaff32c2bb2924fccb734f5718aa56ea2e4
describe
'2388' 'info:fdaE20100110_AAACDPfileF20100110_AABPUJ' 'sip-files00113.txt'
31a4b561ce3bfae6c90643579c759b7c
ec15b9ee8278d02750067e2a0721282e06448508
describe
'43287' 'info:fdaE20100110_AAACDPfileF20100110_AABPUK' 'sip-files00113thm.jpg'
784713c6326f6b923dd8cc8c618306fa
cba544b036b570276dd8fc428ed965348ef4a349
describe
'498572' 'info:fdaE20100110_AAACDPfileF20100110_AABPUL' 'sip-files00114.jp2'
b1b8b4c36f2a85f6bfa51e65cda177b7
57023ec69583b3810227de549723d7ee6ac264f2
'2012-05-16T12:18:24-04:00'
describe
'409009' 'info:fdaE20100110_AAACDPfileF20100110_AABPUM' 'sip-files00114.jpg'
ebd11b5bf745b4586b8b1fbc80b089a6
4311da986d8bd2089ee5ea6be3343f4fb3022dd6
describe
'47664' 'info:fdaE20100110_AAACDPfileF20100110_AABPUN' 'sip-files00114.pro'
4779796fd7c019e396ea8d44a2decb48
5170b9fd772d6135273fcffcde4caa227a78f4bb
describe
'127813' 'info:fdaE20100110_AAACDPfileF20100110_AABPUO' 'sip-files00114.QC.jpg'
0e3e3abc3739190b53ab49f58742e2f7
9f2c9d394b27683834242071d236007d022a9172
describe
'3991246' 'info:fdaE20100110_AAACDPfileF20100110_AABPUP' 'sip-files00114.tif'
4e794dc3f0337052ff95aba64c49953d
2e8d98f2b5de4ea2f33b2d72304b014114f13a86
describe
'2265' 'info:fdaE20100110_AAACDPfileF20100110_AABPUQ' 'sip-files00114.txt'
61f105399b520de933c4a38f4d275597
60dfb1f1eac56c2583f810342894d07cb47f5929
describe
'42017' 'info:fdaE20100110_AAACDPfileF20100110_AABPUR' 'sip-files00114thm.jpg'
b8a17048292cf944fbd5fed73831f511
6be7d3b042db46f071b7bffd775cbfeca5783dd2
describe
'495318' 'info:fdaE20100110_AAACDPfileF20100110_AABPUS' 'sip-files00115.jp2'
f9a22862fc31a521a1f36b132887c429
d40953bf3cbfbd283a6fd2d6886f8dbf05204db9
describe
'429939' 'info:fdaE20100110_AAACDPfileF20100110_AABPUT' 'sip-files00115.jpg'
a7e05d83db749bfdcaefbacab24631f8
dde329a239c5480e66effaa2a61807224848fe67
'2012-05-16T12:22:11-04:00'
describe
'50957' 'info:fdaE20100110_AAACDPfileF20100110_AABPUU' 'sip-files00115.pro'
1a29c8bccdaeed1257287192eef09fe1
cfd844e832944f092b4a1aa464a878e296baa6f3
describe
'132019' 'info:fdaE20100110_AAACDPfileF20100110_AABPUV' 'sip-files00115.QC.jpg'
b8f8d610dbca781b8e2014c19ce59831
d0c69347e5291da4d2cf5b4833e047c681f12bc0
describe
'3965096' 'info:fdaE20100110_AAACDPfileF20100110_AABPUW' 'sip-files00115.tif'
bd23082201d53391ed39070c0bde1b28
c8dbf0883d887ed1bf3837d5e5646c98ca446baf
describe
'2408' 'info:fdaE20100110_AAACDPfileF20100110_AABPUX' 'sip-files00115.txt'
b210ceb9bb98a821d2933e2631005aec
4577c34ac5abbafd882a4d2ab76a2bdf40ad5d77
'2012-05-16T12:28:21-04:00'
describe
'43720' 'info:fdaE20100110_AAACDPfileF20100110_AABPUY' 'sip-files00115thm.jpg'
afdefa6fb02fb5205aab181fc17e7853
7b9a0e642b0148c48f91c9d66643841b06bc85f3
describe
'471008' 'info:fdaE20100110_AAACDPfileF20100110_AABPUZ' 'sip-files00116.jp2'
f5d06f0a3a5503cbcd544f3f56ca660e
361b6d94ca35d5496f9c65f07b09543b7d5e9202
'2012-05-16T12:19:38-04:00'
describe
'326988' 'info:fdaE20100110_AAACDPfileF20100110_AABPVA' 'sip-files00116.jpg'
ecff33495897c22355c22cbff5412c78
ca7ef07382692af0b312deb2725afcd28e7a2324
describe
'30660' 'info:fdaE20100110_AAACDPfileF20100110_AABPVB' 'sip-files00116.pro'
93c4ca52626edd662cd37de123110822
6fb5e98937cc1f9faf6b3675d6788c3744d210f7
describe
'103184' 'info:fdaE20100110_AAACDPfileF20100110_AABPVC' 'sip-files00116.QC.jpg'
ff4f45f0cdd421dcb6f3cfa866eda3ae
159bc291be9e1a9c27faad348e88092f652020c7
describe
'3770700' 'info:fdaE20100110_AAACDPfileF20100110_AABPVD' 'sip-files00116.tif'
7a8281c5d8262c110ac2a2bc7002e691
6865d13c574e02cb8901c3aabadfaa28c86a8bd6
describe
'1455' 'info:fdaE20100110_AAACDPfileF20100110_AABPVE' 'sip-files00116.txt'
1836cbbe7f06e824c26318fb51d5a6b1
03ef28f099fc938416b05a3e295d7cdef485f9bb
describe
'32924' 'info:fdaE20100110_AAACDPfileF20100110_AABPVF' 'sip-files00116thm.jpg'
7b84577b9646b28b0eaaca18ec245c94
43ae35d4db3b2bfa79e3241aecfae6abbd731316
describe
'479918' 'info:fdaE20100110_AAACDPfileF20100110_AABPVG' 'sip-files00117.jp2'
c2fc5d3b0a67ccfa1f93838312bc0248
d8739876a9da43330d12af3d03498753dc7bb4a4
describe
'450987' 'info:fdaE20100110_AAACDPfileF20100110_AABPVH' 'sip-files00117.jpg'
3fc44c64259d440879a399a04bf18b96
d54f88f4d8b26bb83b67fc2b24957f9da789b6c5
describe
'62757' 'info:fdaE20100110_AAACDPfileF20100110_AABPVI' 'sip-files00117.pro'
07331f44e4bcca0752767e8067cf9845
98fdf6bc24603ea235d25df66674ec13aa772477
describe
'6084' 'info:fdaE20100110_AAACDPfileF20100110_AABPVJ' 'sip-filesi.pro'
cf76c5fa8fe1cc65ff8f03418ee71e20
5ea81de98cb8455766f9e99fd690cb4c72302022
describe
'132350' 'info:fdaE20100110_AAACDPfileF20100110_AABPVK' 'sip-files00117.QC.jpg'
ea3af6c118190e6255185638e0343b0d
8d5c19f6f64b91af01157c5c8af9cf6bda722178
describe
'3842072' 'info:fdaE20100110_AAACDPfileF20100110_AABPVL' 'sip-files00117.tif'
8d88de1ccb510d3a58531f2f0b76e574
40fd5496539eaaf5fd873b19cb66c9e405a0498a
'2012-05-16T12:22:52-04:00'
describe
'2769' 'info:fdaE20100110_AAACDPfileF20100110_AABPVM' 'sip-files00117.txt'
7a51424c83e0489ef0adeee6d66aa149
608d26afba5900f1053e890a6af39a10b1abf112
'2012-05-16T12:21:26-04:00'
describe
'42899' 'info:fdaE20100110_AAACDPfileF20100110_AABPVN' 'sip-files00117thm.jpg'
8efe9b873055412bbe2e9b38672c618e
e5c45ddc079a7a8ed94fc35e500c4f3e213731e8
describe
'532100' 'info:fdaE20100110_AAACDPfileF20100110_AABPVO' 'sip-files00118.jp2'
0bff1f0d5d66fa20401c6e7543faad8b
32a60245b1209b7195f920315f33cc94717cb51d
describe
'425167' 'info:fdaE20100110_AAACDPfileF20100110_AABPVP' 'sip-files00118.jpg'
d7169f005f2e1f2d16d637703b86d659
7ad36a3d5436151478d0c5c65bb598e55dd8eacb
'2012-05-16T12:25:18-04:00'
describe
'65485' 'info:fdaE20100110_AAACDPfileF20100110_AABPVQ' 'sip-files00118.pro'
51cb730ce47986622b6e6eaa85ff9824
79ff5ec205dbd11dfe421a2163e9823de0cc87d9
describe
'123572' 'info:fdaE20100110_AAACDPfileF20100110_AABPVR' 'sip-files00118.QC.jpg'
4760b2ab5aee49d82f1af2ffebe5307a
f41ee97cc34bcfd6a9aedc47b360bf94b776d34e
'2012-05-16T12:28:36-04:00'
describe
'4259554' 'info:fdaE20100110_AAACDPfileF20100110_AABPVS' 'sip-files00118.tif'
564e2a360cddf93d5c1a9e434ee5820e
fce6316cecc8ac353057454e19b836aab8d53d70
describe
'2819' 'info:fdaE20100110_AAACDPfileF20100110_AABPVT' 'sip-files00118.txt'
11dbd2e218e6671e57a6f62d3623c202
823a89962595384000cd02d674b9169df7276b0d
'2012-05-16T12:21:37-04:00'
describe
'38862' 'info:fdaE20100110_AAACDPfileF20100110_AABPVU' 'sip-files00118thm.jpg'
52714bc7059a5f5826f8bd7980961205
ed8748b66fbb4002832ae43c2efb0b11defe2429
describe
'415179' 'info:fdaE20100110_AAACDPfileF20100110_AABPVV' 'sip-files00119.jp2'
9b95e9019feec21f9cd6bb4569b16a8e
12fc56a99a4bc38f39c00b8c12e8e0db96e9bb8f
describe
'241795' 'info:fdaE20100110_AAACDPfileF20100110_AABPVW' 'sip-files00119.jpg'
4cb75dd7ec121647f85e9eb8b2d965b1
ee0319a124b210050cae577ba151016821b506a5
'2012-05-16T12:19:35-04:00'
describe
'6519' 'info:fdaE20100110_AAACDPfileF20100110_AABPVX' 'sip-files00119.pro'
f8af45aff43c34eff124a3f0c99556c9
824abb4e27cf7f7011667c128b201c28d9d87441
describe
'68877' 'info:fdaE20100110_AAACDPfileF20100110_AABPVY' 'sip-files00119.QC.jpg'
7d9459c1d3d75d39da9ed2f1494210af
726f61c375d3942d02019a032fda780ad5f7dc21
describe
'3323794' 'info:fdaE20100110_AAACDPfileF20100110_AABPVZ' 'sip-files00119.tif'
a1ff88e094ff1751dde7b4ba41c216f8
39d778dc41f40a68f59d95377e5176536969f829
describe
'304' 'info:fdaE20100110_AAACDPfileF20100110_AABPWA' 'sip-files00119.txt'
6533897bb78dfc7338a6cb06c634f704
051f87a77d43e6df6fb27437842dccd3b1c2b82a
describe
'19332' 'info:fdaE20100110_AAACDPfileF20100110_AABPWB' 'sip-files00119thm.jpg'
47f4040312c7c571115ecf93cfef203a
f7008a8265d95fa6fcb818b311d6c3c5545439c8
describe
'75682' 'info:fdaE20100110_AAACDPfileF20100110_AABPWC' 'sip-filesi.QC.jpg'
b764100da1c5c1c3a5f027ff5fd1df16
2b8f644f27238eda8f217447b9aec2d664d65d06
describe
'4017518' 'info:fdaE20100110_AAACDPfileF20100110_AABPWD' 'sip-filesi.tif'
86e57f318584daaf6949ad7a8bde83dd
b76185d93383c5dbfc3b2e81bc36b96327caa66d
'2012-05-16T12:26:36-04:00'
describe
'404' 'info:fdaE20100110_AAACDPfileF20100110_AABPWE' 'sip-filesi.txt'
482443556d03666dfa884d6467ff8e71
9c1e754c4e038c8286bdb4a9c1367ad3b25e3fcb
'2012-05-16T12:20:41-04:00'
describe
'449515' 'info:fdaE20100110_AAACDPfileF20100110_AABPWF' 'sip-filesii.jp2'
03cac9310b530bde902d6ff5f34887af
9b2a408cf15dd025961e7ca3d39108cc55ce9653
describe
'246019' 'info:fdaE20100110_AAACDPfileF20100110_AABPWG' 'sip-filesii.jpg'
e5a3dbca056db8a64d00e94e9fe6f081
a21a29d8be890ec01305b56fbfcb92a8e0cd76d6
describe
'8706' 'info:fdaE20100110_AAACDPfileF20100110_AABPWH' 'sip-filesii.pro'
48d4bdc2da2e1ae398cc685f87eb6969
8c97c229c56737b754f7e58ab30d1e2b753bda6f
describe
'79755' 'info:fdaE20100110_AAACDPfileF20100110_AABPWI' 'sip-filesii.QC.jpg'
16d853bb3eea4c20124669fb934ef653
7528ddc30e001022bcba0082f7a35ee06a067f1a
describe
'3959360' 'info:fdaE20100110_AAACDPfileF20100110_AABPWJ' 'sip-filesii.tif'
252258c2eec5932ba86f25eb62ac1628
b1b199ff0d8a2fdda1c79e1ce382a1f3ab4276da
describe
'511' 'info:fdaE20100110_AAACDPfileF20100110_AABPWK' 'sip-filesii.txt'
2a9b5060ac31d27e3aba7f3c8c40ea14
98f767260b1e1a531a21f1849eeaf54f076b7f3a
'2012-05-16T12:22:16-04:00'
describe
'487725' 'info:fdaE20100110_AAACDPfileF20100110_AABPWL' 'sip-filesiii.jp2'
4cf1cf9d4d077d2e4f967a9cd4027a70
34a1a99c47e6f03892bad0342b2c8abb42b3ad1e
'2012-05-16T12:23:26-04:00'
describe
'330794' 'info:fdaE20100110_AAACDPfileF20100110_AABPWM' 'sip-filesiii.jpg'
d7bc6167ab06b1efd3e1eb52b9444d9b
37da29fcddf6615927222731f1692c0285c9b8be
describe
'23000' 'info:fdaE20100110_AAACDPfileF20100110_AABPWN' 'sip-filesiii.pro'
2c5203354f933d7b71c471e44308f3e2
bc3b35a9063cf88d11b23853ff1445ba0def8949
describe
'104768' 'info:fdaE20100110_AAACDPfileF20100110_AABPWO' 'sip-filesiii.QC.jpg'
bd49f68c7f27fdd4e8cc11bf03e36f92
e464a02045e2295463be3a1ac84728ce94d87493
'2012-05-16T12:19:48-04:00'
describe
'3904806' 'info:fdaE20100110_AAACDPfileF20100110_AABPWP' 'sip-filesiii.tif'
b28d0690b839ebb4631301857e2ceaa8
769b5cd1511ffa48ff5446b0cb671ae4ec35f732
describe
'1088' 'info:fdaE20100110_AAACDPfileF20100110_AABPWQ' 'sip-filesiii.txt'
4985b078914649d95443b811452b5099
304fedbd10e56b0e54f1ca48369c20816a4b5c33
'2012-05-16T12:27:26-04:00'
describe
'32230' 'info:fdaE20100110_AAACDPfileF20100110_AABPWR' 'sip-filesiiithm.jpg'
53a36c58e81cc8e0be05fd00bb6837f1
cbcdcbd4343b16648a9d2aa05512d2cbe2792c48
describe
'29466' 'info:fdaE20100110_AAACDPfileF20100110_AABPWS' 'sip-filesiithm.jpg'
5eec431cccd8ac509f2371d0900d3a92
1dec395d738102120312e6543e0b3efdbe6f9b0d
describe
'27263' 'info:fdaE20100110_AAACDPfileF20100110_AABPWT' 'sip-filesithm.jpg'
67038826f0d435fa8dd44f54462125a8
7ec5f8fdc1b652f66c9386cb884a35b841461545
'2012-05-16T12:26:30-04:00'
describe
'251586' 'info:fdaE20100110_AAACDPfileF20100110_AABPWU' 'sip-filesiv.jp2'
83580488c467437efc50ce600646c241
d5e2503afbfd9e7a79527212d2f965f7162ccfb8
'2012-05-16T12:20:53-04:00'
describe
'179738' 'info:fdaE20100110_AAACDPfileF20100110_AABPWV' 'sip-filesiv.jpg'
7789556063a2061705ba755e7c0bfc85
c41d4bb7fff4c55a57fe6ab7ccc17a44d6f29fb1
'2012-05-16T12:25:44-04:00'
describe
'3925' 'info:fdaE20100110_AAACDPfileF20100110_AABPWW' 'sip-filesiv.pro'
d59baf11cea5a69f6200cf4b1ea99bcc
2824c179f5a61f8f71642e81e19e9ea28ea47a56
'2012-05-16T12:22:58-04:00'
describe
'59399' 'info:fdaE20100110_AAACDPfileF20100110_AABPWX' 'sip-filesiv.QC.jpg'
58568651d2de37a413e41101b20c080b
530c732388495b153664f53609f418569699fc5e
describe
'3555848' 'info:fdaE20100110_AAACDPfileF20100110_AABPWY' 'sip-filesiv.tif'
26831d024e4157972e1400d8c81c3854
f5080ac588039f340c181e0f85dcf695c3fe1260
describe
'313' 'info:fdaE20100110_AAACDPfileF20100110_AABPWZ' 'sip-filesiv.txt'
312d0d7de9144978ba63cb1ea4c3590b
843b3ffb2a646ac8ba849b086c4607cd5e886c04
describe
'21928' 'info:fdaE20100110_AAACDPfileF20100110_AABPXA' 'sip-filesivthm.jpg'
9cce8868208f8a459f17dfbbc6eaf2fc
29bec6dd3c0fb163530ae2bf96cdf79973865c9e
describe
'508387' 'info:fdaE20100110_AAACDPfileF20100110_AABPXB' 'sip-filesix.jp2'
d0a68ed3c661ddf98631828ee149c914
55793eebd124df3ff8badf3253671cb731011ffa
describe
'350656' 'info:fdaE20100110_AAACDPfileF20100110_AABPXC' 'sip-filesix.jpg'
69ecea14ba14e121927e8c23805f8dde
8f43b3f26f04909c876903c1eb5c35772ed45bf3
describe
'32546' 'info:fdaE20100110_AAACDPfileF20100110_AABPXD' 'sip-filesix.pro'
1c1c7e73b7c0375b9fa267a5d4477b01
52a21ba71225dfdd113de27d1bdf4dccaf38b446
describe
'99042' 'info:fdaE20100110_AAACDPfileF20100110_AABPXE' 'sip-filesix.QC.jpg'
6c3901efbe45f0aa8907894a982abec7
75fb7145a2bd6db12174229dd563e99324ed5654
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPXF' 'sip-filesix.tif'
be57bb120c894d7b088397ced3a31338
70ea012483797a0941b53ce413bb1f01c0c6c0f9
'2012-05-16T12:24:03-04:00'
describe
'1507' 'info:fdaE20100110_AAACDPfileF20100110_AABPXG' 'sip-filesix.txt'
6a0c75f127e3f4e5811cca9975cba3a2
b1ac7032af5a27a04a3112857072b8bd068e682e
describe
'29019' 'info:fdaE20100110_AAACDPfileF20100110_AABPXH' 'sip-filesixthm.jpg'
a2b4b388f15aaaa9d2c800c80bd382ef
ed390157bcb489683365d9c6c9df26c478cce568
describe
'4269711' 'info:fdaE20100110_AAACDPfileF20100110_AABPXI' 'sip-filesplate1.jp2'
fe4f2865b0de418ba024426adca847b7
882bd4467452eba2dc1646a765c9b76fc686557d
describe
'664898' 'info:fdaE20100110_AAACDPfileF20100110_AABPXJ' 'sip-filesplate1.jpg'
5d8fcd14a98d6849eceb8b09c986baa0
2237ef204ff187e7323819850923babf319e8cfe
describe
'103328' 'info:fdaE20100110_AAACDPfileF20100110_AABPXK' 'sip-filesplate1.pro'
1c8d67b1e0c4dd2bc5c660d2f57cca70
c08dd84cb9f7fc5e1beae2aa326a34c40af67d9d
describe
'189816' 'info:fdaE20100110_AAACDPfileF20100110_AABPXL' 'sip-filesplate1.QC.jpg'
755edd625e6064f27e10089462885e96
7f1eb670f9e43133ce8da984cd2acbe71dcb7568
describe
'102477804' 'info:fdaE20100110_AAACDPfileF20100110_AABPXM' 'sip-filesplate1.tif'
89aac8250cecdeab2aea2a716be9b534
e0c0e7c47d5cc49d022c5735d4de23711367e1e7
'2012-05-16T12:26:46-04:00'
describe
'4490' 'info:fdaE20100110_AAACDPfileF20100110_AABPXN' 'sip-filesplate1.txt'
47e386e91ee996ac80821e4009e9a5f5
ff9bd2019e248c49439b5dc71c1387b045e9dcd0
describe
Invalid character
'54108' 'info:fdaE20100110_AAACDPfileF20100110_AABPXO' 'sip-filesplate1thm.jpg'
af7db3e051844bc8e11919c5d830f7b9
bfe197f53ac8f7e7f497636dc1932465c51d7cd5
describe
'1170451' 'info:fdaE20100110_AAACDPfileF20100110_AABPXP' 'sip-filestable9.jp2'
a4dc627fc1a0211e32f65b63ec75a4d5
524309097765933653d0caf344bc46722290b657
'2012-05-16T12:23:10-04:00'
describe
'126783' 'info:fdaE20100110_AAACDPfileF20100110_AABPXQ' 'sip-filestable9.jpg'
879a371b81a9b4e837a90cb68843c8d8
44e3998224a6460b4928fa27ec4734529c2e1b21
describe
'75266' 'info:fdaE20100110_AAACDPfileF20100110_AABPXR' 'sip-filestable9.pro'
eb365353091410dd3c58b0d3729f774c
904a68d22240626bc860108efab947132119e957
'2012-05-16T12:18:50-04:00'
describe
'42845' 'info:fdaE20100110_AAACDPfileF20100110_AABPXS' 'sip-filestable9.QC.jpg'
73717057c7037b2e5bfeb7a6c8f1bdd3
6eef0cb5c251c9a1a9da92e38e0d7fae04a5d823
describe
'10228032' 'info:fdaE20100110_AAACDPfileF20100110_AABPXT' 'sip-filestable9.tif'
57d6390a969d799a74edb09f232052bb
778ecdad2af1ecf935c92121fe02fbdb80ad7567
'2012-05-16T12:22:48-04:00'
describe
'3527' 'info:fdaE20100110_AAACDPfileF20100110_AABPXU' 'sip-filestable9.txt'
9aae8259789a808d9e545c7d1c958428
080967259eb323de65441a4626655b443be98f1a
'2012-05-16T12:22:28-04:00'
describe
Invalid character
'14107' 'info:fdaE20100110_AAACDPfileF20100110_AABPXV' 'sip-filestable9thm.jpg'
8fff7d8ce19d0045fab2dfb161f0a7bc
d63d68702352d39a3ea3a59a411acaf52c681236
describe
'155998' 'info:fdaE20100110_AAACDPfileF20100110_AABPXW' 'sip-filesUF00000234_00001.mets'
a9c2d86b1c2301c8a240641c52221546
cf0bdb6c462e31322b26f232c4e793fb78367aa1
'2012-05-16T12:21:39-04:00'
describe
TargetNamespace.1: Expecting namespace 'http://www.uflib.ufl.edu/digital/metadata/ufdc2/', but the target namespace of the schema document is 'http://digital.uflib.ufl.edu/metadata/ufdc2/'.
'2015-10-09T15:51:21-04:00' 'mixed'
xml resolution
http://www.uflib.ufl.edu/digital/metadata/ufdc2/ufdc2.xsd
BROKEN_LINK schema http://www.uflib.ufl.edu/digital/metadata/ufdc2/ufdc2.xsd
The element type "div" must be terminated by the matching end-tag "
".
TargetNamespace.1: Expecting namespace 'http://www.uflib.ufl.edu/digital/metadata/ufdc2/', but the target namespace of the schema document is 'http://digital.uflib.ufl.edu/metadata/ufdc2/'.
'332392' 'info:fdaE20100110_AAACDPfileF20100110_AABPXZ' 'sip-filesv.jpg'
3c80e3881397792370ca4b0b429de4eb
1e5a3109236a4cdd624afbf5f048dd901cb1dcb3
'2012-05-16T12:26:37-04:00'
describe
'376906' 'info:fdaE20100110_AAACDPfileF20100110_AABPYA' 'sip-filesvi.jpg'
35d0c0ce270714649e328683ae27cd5d
dbab8f93b86a68b2e2d61df70fbc994b4a50277a
describe
'348473' 'info:fdaE20100110_AAACDPfileF20100110_AABPYB' 'sip-filesvii.jpg'
f0d42b5467f459f07b55e95ce324406b
6128a1425e4f38ec1b86faa970c39ab799fa8b84
describe
'410442' 'info:fdaE20100110_AAACDPfileF20100110_AABPYC' 'sip-filesviii.jpg'
20c59e194638a1a0b7a1c976a081735d
6273c70594423d9b640ae1b463fd08406144985c
describe
'223654' 'info:fdaE20100110_AAACDPfileF20100110_AABPYD' 'sip-filesx.jpg'
dbdf8f79bfbb6154887624a11ed32366
7e92c8cdf3bb5ecea343fd8d9623c2297816afbc
describe
'432676' 'info:fdaE20100110_AAACDPfileF20100110_AABPYE' 'sip-filesxi.jpg'
f05d084ac011ca387524b96f846a5748
b05d398cea37c0481dc7f7bd327e7ffb8d7bdc4a
'2012-05-16T12:21:45-04:00'
describe
'494070' 'info:fdaE20100110_AAACDPfileF20100110_AABPYF' 'sip-filesv.jp2'
da7bef53c525d96100d20e5ae25a2df6
9f58fd909dd579afdd2d01e3587b121f645e1abd
describe
'470314' 'info:fdaE20100110_AAACDPfileF20100110_AABPYG' 'sip-filesvi.jp2'
68efbb1d60ce81d0e59650cd3be0d0e8
f38a6e14345f137cd0172864fc7be823bce020db
describe
'479682' 'info:fdaE20100110_AAACDPfileF20100110_AABPYH' 'sip-filesvii.jp2'
55dd93c920f6be881ddb55412205825e
34155b0e5b26e33a95412679bd2da782d6258689
'2012-05-16T12:19:49-04:00'
describe
'495464' 'info:fdaE20100110_AAACDPfileF20100110_AABPYI' 'sip-filesviii.jp2'
821774ac1c96f63a742595d289aabc28
04ab4300563d920a95c8c135d57bab37123a42aa
describe
'543347' 'info:fdaE20100110_AAACDPfileF20100110_AABPYJ' 'sip-filesx.jp2'
9f96fa3531d18e84095fee7e9b34fe7a
43152f0532070e15333d5c49f26548bde4deef53
'2012-05-16T12:20:31-04:00'
describe
'515924' 'info:fdaE20100110_AAACDPfileF20100110_AABPYK' 'sip-filesxi.jp2'
162700bde232e2fef9e0516c6c34a4cb
841ddb5c1b9556b06cbeb08b9116b47e1527d29a
describe
'3955806' 'info:fdaE20100110_AAACDPfileF20100110_AABPYL' 'sip-filesv.tif'
830c4d12e2601f934e6f36002d44081d
3489998d1b1ec858f6185db97f5f3aed41619d86
'2012-05-16T12:25:25-04:00'
describe
'3766514' 'info:fdaE20100110_AAACDPfileF20100110_AABPYM' 'sip-filesvi.tif'
c65a4c41cdae21a0be59a0e810d2384e
3f211f08638cbabd84cbf0a8566088f6b79f9473
describe
'3840080' 'info:fdaE20100110_AAACDPfileF20100110_AABPYN' 'sip-filesvii.tif'
48dccc61095af312f3d9f54f6b5d7976
9434b00ea5c3ff6eacbdcdbe385e263b7f0d2c1e
describe
'3966248' 'info:fdaE20100110_AAACDPfileF20100110_AABPYO' 'sip-filesviii.tif'
600e8b19091533dbf04fc934e3c1cc9f
36d997a60d1f97ad0cb2918efba3a67e82ee4949
describe
'4349402' 'info:fdaE20100110_AAACDPfileF20100110_AABPYP' 'sip-filesx.tif'
38a7ce98ffcd6918aa25e8557c73923f
0efb58f63a478d57e2b8db3b0343286276075a39
'2012-05-16T12:18:41-04:00'
describe
'4132486' 'info:fdaE20100110_AAACDPfileF20100110_AABPYQ' 'sip-filesxi.tif'
a2d519074605104645130a97c5b05dbf
b6756927e86b39451fabd613fe7075d7a03ccd53
'2012-05-16T12:19:40-04:00'
describe
'82045' 'info:fdaE20100110_AAACDPfileF20100110_AABPYR' 'sip-filesv.pro'
b4a3fda6654af5e2053b76883813e5de
db2cfce8286470c1164a91d4a250f94f54d921a0
describe
'49526' 'info:fdaE20100110_AAACDPfileF20100110_AABPYS' 'sip-filesvi.pro'
5d20978b585c4d0285adbc6b0f99cdb3
e261fa3be96110544d4997f7847389671d07ecc6
'2012-05-16T12:27:28-04:00'
describe
'73551' 'info:fdaE20100110_AAACDPfileF20100110_AABPYT' 'sip-filesvii.pro'
cc5a5b02b8a2843eaa4a55d10ae72e93
c38a9bf732a4242a2dcfee08d906f9b4690f97e5
describe
'84355' 'info:fdaE20100110_AAACDPfileF20100110_AABPYU' 'sip-filesviii.pro'
2cdadd1c910db4b184b04ec6651c423d
7d94b6dd4e56d79b464fd7a8665bbc62cba7ce48
describe
'218' 'info:fdaE20100110_AAACDPfileF20100110_AABPYV' 'sip-filesx.pro'
85b19ae13b89ec4aa112f5715bc732c0
802b9de507ee21cc060ef701a67a5991a881789d
describe
'49738' 'info:fdaE20100110_AAACDPfileF20100110_AABPYW' 'sip-filesxi.pro'
a42de73915e3ad2c2c6fa525e7c26b07
013fd83422d602003e5ee46ea715cbfef1c8105c
describe
'3710' 'info:fdaE20100110_AAACDPfileF20100110_AABPYX' 'sip-filesv.txt'
66868d54b7f71a98b404d3394751a4ff
1cc70286ba0713c0dd36a8d1b6e0952019c51992
describe
'2956' 'info:fdaE20100110_AAACDPfileF20100110_AABPYY' 'sip-filesvi.txt'
0e6124a80772612da3e572760ca779f1
90c523025165b736c6af9f0acb11acbec1f847c2
describe
'3262' 'info:fdaE20100110_AAACDPfileF20100110_AABPYZ' 'sip-filesvii.txt'
f9e1ed683d971c3cb7131d2710d49024
beef0752b646d191c39d8517056e7a6ef0c56928
describe
'3791' 'info:fdaE20100110_AAACDPfileF20100110_AABPZA' 'sip-filesviii.txt'
efed0f07d3f1565d5f81dc0600ed20aa
16c599c7d128a1dc782a318280e049b8fa1d3360
describe
'3' 'info:fdaE20100110_AAACDPfileF20100110_AABPZB' 'sip-filesx.txt'
bc949ea893a9384070c31f083ccefd26
cbb8391cb65c20e2c05a2f29211e55c49939c3db
describe
'1976' 'info:fdaE20100110_AAACDPfileF20100110_AABPZC' 'sip-filesxi.txt'
da1a1e2d361cc55d823ae8dda5f176c2
bb6f67597ee1600820562a3626e2c53868708d72
describe
'199911' 'info:fdaE20100110_AAACDPfileF20100110_AABPZD' 'sip-filesUF00000234_00001.xml'
375b742ab26d3f19871b8c1c63f6740c
a189e3da1e933dfdeebdc9115de4c28d2c577158
describe
TargetNamespace.1: Expecting namespace 'http://www.uflib.ufl.edu/digital/metadata/ufdc2/', but the target namespace of the schema document is 'http://digital.uflib.ufl.edu/metadata/ufdc2/'.
'2015-10-09T15:51:20-04:00'
xml resolution
http://www.uflib.ufl.edu/digital/metadata/ufdc2/ufdc2.xsd
http://www.uflib.ufl.edu/digital/metadata/ufdc2/ufdc2.xsd
The element type "div" must be terminated by the matching end-tag "".
TargetNamespace.1: Expecting namespace 'http://www.uflib.ufl.edu/digital/metadata/ufdc2/', but the target namespace of the schema document is 'http://digital.uflib.ufl.edu/metadata/ufdc2/'.
'109589' 'info:fdaE20100110_AAACDPfileF20100110_AABPZE' 'sip-filesv.QC.jpg'
50c449908a1f1de759b8979e6ef4cad0
920a1ef1f5a719d03603e03ab3acb6b197277943
'2012-05-16T12:18:47-04:00'
describe
'110820' 'info:fdaE20100110_AAACDPfileF20100110_AABPZF' 'sip-filesvi.QC.jpg'
d8e0399d067719bace03ffc0c82664fb
50c1db2121999c37202ea4c14a29e4d48b0610b7
describe
'113241' 'info:fdaE20100110_AAACDPfileF20100110_AABPZG' 'sip-filesvii.QC.jpg'
5bc0cc5a57392d6c83ac378236b5e0b1
78f320a0af8e1c693143fb6a9d00f705191bdcc1
describe
'133361' 'info:fdaE20100110_AAACDPfileF20100110_AABPZH' 'sip-filesviii.QC.jpg'
a8e7a0c050815c9d3c457c6223cda3cd
6c60675004fd29fc52ea05205dabeee7d6a90040
'2012-05-16T12:21:43-04:00'
describe
'38773' 'info:fdaE20100110_AAACDPfileF20100110_AABPZI' 'sip-filesviiithm.jpg'
fe4dc7bfa5d035febbca78af4dd515fa
eb994b06fff4163cda89deab9076c3aac8e95cf6
describe
'33716' 'info:fdaE20100110_AAACDPfileF20100110_AABPZJ' 'sip-filesviithm.jpg'
c652a05aa2779f94cb5b52e62de28280
1a6d87990763c66021992e84100e68459eb171bf
describe
'34978' 'info:fdaE20100110_AAACDPfileF20100110_AABPZK' 'sip-filesvithm.jpg'
6e88e2186c82d7f7cb057dbb9bbaca02
67734f96420b48e2d50d2095cc482bd2454a86ef
describe
'30642' 'info:fdaE20100110_AAACDPfileF20100110_AABPZL' 'sip-filesvthm.jpg'
f85bd335e0d07b9c183c6e076dca3a89
db538fc07cb34e48da105ee7dd0fc31d3f617ae5
describe
'61351' 'info:fdaE20100110_AAACDPfileF20100110_AABPZM' 'sip-filesx.QC.jpg'
9fcc36101620588bd33058bb6b9aa9cc
eee712ac3783ac258c210964c103ebf24115024b
describe
'137443' 'info:fdaE20100110_AAACDPfileF20100110_AABPZN' 'sip-filesxi.QC.jpg'
95808421791cd1cf7e8ab9ab5c3105fd
3c7d68265d681013cd736c97807a7da780d9d9f5
describe
'info:fdaE20100110_AAACDPfileF20100110_AABPZO' 'sip-filesxithm.jpg'
7acff065280bf12d72037bf880af39aa
5b7d6b3800ae956833b2e7fbb512e53b9a86c792
describe
'18883' 'info:fdaE20100110_AAACDPfileF20100110_AABPZP' 'sip-filesxthm.jpg'
c85c378f44f43bac9d87547df99750ef
7ff2ff932b5c37809c5e93701851f37d1b04ca88
describe