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 Introduction
 Lithostratigraphy
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 Tables and figures


FGS



Core drilling project, Lee, Hendry and Collier Counties ( FGS: Open file report 37 )
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 Material Information
Title: Core drilling project, Lee, Hendry and Collier Counties ( FGS: Open file report 37 )
Series Title: ( FGS: Open file report 37 )
Physical Description: 44 p. : ill., map ; 28 cm.
Language: English
Creator: Green, Richard C
Campbell, Kenneth M ( Kenneth Mark ), 1949-
Scott, Thomas M
Publisher: Florida Geological Survey
Place of Publication: Tallahassee
Publication Date: 1990
 Subjects
Subjects / Keywords: Hydrogeology -- Florida -- Hendry County   ( lcsh )
Hydrogeology -- Florida -- Lee County   ( lcsh )
Hydrogeology -- Florida -- Collier County   ( lcsh )
Geology -- Florida -- Hendry County   ( lcsh )
Geology -- Florida -- Lee County   ( lcsh )
Geology -- Florida -- Collier County   ( lcsh )
Genre: government publication (state, provincial, terriorial, dependent)   ( marcgt )
bibliography   ( marcgt )
non-fiction   ( marcgt )
 Notes
Statement of Responsibility: by Richard C. Green, Kenneth M. Campbell and Thomas M. Scott.
Bibliography: Includes bibliographical references (p. 12-13)
General Note: Cover title.
Funding: Digitized as a collaborative project with the Florida Geological Survey, Florida Department of Environmental Protection.
 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: aleph - 001751890
oclc - 25643418
notis - AJG4829
System ID: UF00001036:00001

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Table of Contents
    Title Page
        Title Page 1
        Title Page 2
    Introduction
        Page 1
        Page 2
    Lithostratigraphy
        Page 2
        Page 3
        Page 4
        Page 5
        Page 6
        Page 7
        Page 8
        Page 9
        Page 10
        Page 11
    Selected bibliography
        Page 12
        Page 13
    Tables and figures
        Page 14
        Page 15
        Page 16
        Page 17
        Page 18
        Page 19
        Page 20
        Page 21
        Page 22
        Page 23
        Page 24
        Page 25
        Page 26
        Page 27
        Page 28
        Page 29
        Page 30
        Page 31
        Page 32
        Page 33
        Page 34
        Page 35
        Page 36
        Page 37
        Page 38
        Page 39
        Page 40
        Page 41
        Page 42
        Page 43
        Page 44
        Copyright
            Main
Full Text










State of Florida
Department of Natural Resources
Tom Gardner, Executive Director




Division of Resource Management
Jeremy Craft, Director




Florida Geological Survey
Walt Schmidt, State Geologist and Chief






Open File Report 37



Core Drilling Project: Lee,
Hendry and Collier Counties


by


Richard C. Green, Kenneth M. Campbell
and Thomas M. Scott


Florida Geological Survey
Tallahassee, Florida
1990


...........




















































SC1E?~CI









Core Drilling Project: Lee, Hendry
and Collier Counties

INTRODUCTION

In June 1988, the Florida Geological Survey (FGS) and the

South Florida Water Management District (District) entered into a

contract (#88-188-0675) to conduct a joint project in Lee, Hendry

and Collier Counties. The objectives of this project were: to

increase the geologic/hydrogeologic well data available in these

counties, to translate existing lithologic descriptions of wells

within the district to computer format and to add this data to the

District computer data base. These objectives were met by the

translation of over 180 existing well logs to computer format, by

drilling and evaluating the data for six cores, and merging all of

this data with the existing FGS and District computer data bases.

Six cores were drilled by the FGS at locations specified by

the District (Figure 1). Geophysical logs were run on each core by

District personnel. After completion of drilling and logging, five

of the coreholes were plugged by District contractors. The

remaining corehole was reamed and a monitor well constructed. The

cores are listed below:

Lee County

W-16242; South Seas Plantation #1, 760' TD, monitor well

(T45S, R21E, S26)

W-16523; Koreshan #1, 822' TD

(T46S, R25E, S33A)








Hendry County

W-16329; Hilliard Brothers #1, 740' TD

(T44S, R32E, S16B)

W-16387; U.S. Sugar #1, 662' TD

(T44S, R34E, S09B)

Collier County

W-16434; Collier Corp. #1, (Immokalee), 715' TD

(T47S, R30E, S03B)

W-16505; Fakahatchee Strand #1, 702' TD

(T50S, R30E, S06C)

Detailed stratigraphic columns for each core are included as

Figures 2-7 (Attached).

LITHOSTRATIGRAPHY

Suwannee Limestone

The Oligocene-age Suwannee Limestone underlies all of Lee,

Hendry and Collier Counties, consisting of white to beige

recrystallized limestone containing abundant microfossils, quartz

sand and trace amounts of phosphate. The top of the Suwannee

Limestone is encountered between 550 and 1000 feet below National

Geodetic Vertical Datum (NGVD), with the shallowest occurrences

being in northwest Lee County and the deepest in central Hendry

County (Wedderburn et al., 1982; Peacock, 1983 and Klein et al.,

1964). Sediments of the Suwannee Limestone form part of the

Floridan aquifer system. The Suwannee was encountered in both Lee

County cores (W-16242 and W-16523) (Figures 2, 7-9). The pick for

the top of the Suwannee Limestone was based upon an overall








Hendry County

W-16329; Hilliard Brothers #1, 740' TD

(T44S, R32E, S16B)

W-16387; U.S. Sugar #1, 662' TD

(T44S, R34E, S09B)

Collier County

W-16434; Collier Corp. #1, (Immokalee), 715' TD

(T47S, R30E, S03B)

W-16505; Fakahatchee Strand #1, 702' TD

(T50S, R30E, S06C)

Detailed stratigraphic columns for each core are included as

Figures 2-7 (Attached).

LITHOSTRATIGRAPHY

Suwannee Limestone

The Oligocene-age Suwannee Limestone underlies all of Lee,

Hendry and Collier Counties, consisting of white to beige

recrystallized limestone containing abundant microfossils, quartz

sand and trace amounts of phosphate. The top of the Suwannee

Limestone is encountered between 550 and 1000 feet below National

Geodetic Vertical Datum (NGVD), with the shallowest occurrences

being in northwest Lee County and the deepest in central Hendry

County (Wedderburn et al., 1982; Peacock, 1983 and Klein et al.,

1964). Sediments of the Suwannee Limestone form part of the

Floridan aquifer system. The Suwannee was encountered in both Lee

County cores (W-16242 and W-16523) (Figures 2, 7-9). The pick for

the top of the Suwannee Limestone was based upon an overall








decrease in quartz sand and phosphate, an overall increase in

fossil content, and a general increase in carbonate lithology from

a mudstone or wackestone to a packstone or grainstone.

Hawthorn Group

The Miocene-Pliocene age Hawthorn Group unconformably overlies

the Suwannee Limestone. Scott (1986, 1988) raised the Hawthorn

Formation to Group status and erected new formations within the

Group statewide. The Hawthorn Group in south Florida consists of

two formations: the Arcadia Formation (Hawthorn carbonate unit and

Tampa Limestone of previous usage) and the Peace River Formation

(Hawthorn siliciclastic unit of previous usage).

Arcadia Formation

The Arcadia Formation consists predominantly of white, light

gray and yellowish gray, poorly to well indurated, calcilutitic and

very finely crystalline limestone (wackestone to mudstone),

dolomitic limestone and dolostone. The Arcadia contains variable

amounts of clay, silt, quartz and phosphate sand with occasional

phosphate gravel. Beds of clay, silt-sized dolomite and quartz

sand are common. The Arcadia is commonly fossiliferous (primarily

oysters, pectens and bryozoans, with diatoms and foraminifera in

some clayey intervals). The top of the Arcadia is found at

approximately 150 feet below NGVD in northwestern Lee County and

dips to the southeast to over 400 feet below NGVD in southeastern

Collier County (Scott, 1988). The Arcadia Formation was

encountered in all six of the cores drilled for this project

(Figures 2-10). The top of the Arcadia Formation in these cores








was picked based upon a change from predominantly siliciclastic

sediments to predominantly carbonate sediments.

Peace River Formation

The Peace River Formation (Scott, 1988) consists of the "upper

Hawthorn siliciclastics" of prior usage as well as the

siliciclastics previously placed in the Tamiami Formation (Parker,

1951, Parker et al., 1955) and the Murdock Station and Bayshore

Clay Members of the Tamiami Formation (Hunter, 1968). The Peace

River Formation consists primarily of white, light gray and light

olive, interbedded, poorly to moderately indurated sands, silts,

clays and carbonates. The siliciclastic components are dominant.

Carbonate material is primarily calcilutite or silt-sized dolomite.

All lithologies typically contain variable amounts of quartz and

phosphate sand. The top of the Peace River Formation is

encountered at approximately 0 feet NGVD in northern Lee County

dipping slightly to the south-southeast in Lee and Hendry Counties

then to the southwest in Collier County where it is found

predominantly between 100 and 150 feet below NGVD (Scott, 1988).

The Peace River Formation was encountered in all six cores. In

three of the cores (W-16242, W-16387, and W-16523) (Figures 2, 3,

6-10) the top of the Peace River Formation was picked as a change

from sandy limestones of the Tamiami Formation to very fine to fine

sands, silts, and clays with minor phosphate and carbonate. In the

three remaining cores (W-16329, W-16434, and W-16505) (Figures 3-5,

8, 10), the presence of thick sequences of coarse siliciclastics

made the picking of the top of the Peace River Formation difficult.








In general, the Peace River Formation pick in these cores was made

based upon a decrease in grain size from the medium to very coarse

sands of the "Miocene coarse clastics" to very fine to fine sands

with minor phosphate and carbonate. This pick is made more

difficult in these three cores due to the fact that the recovery of

sediments in this interval was generally poor, with most of the

samples consisting of bags of cuttings which represented five feet

or more of samples.

Sediments of the Hawthorn Group form the both intermediate

aquifer system and intermediate confining unit which includes the

mid-Hawthorn aquifer and sandstone aquifer, and the lower, mid- and

upper Hawthorn confining zones (Wedderburn et al., 1982; Smith and

Adams, 1988). The confining characteristics of the Hawthorn Group

sediments also serve to confine the Floridan aquifer system. Water

from the producing zones in the Hawthorn is better quality in

general than the underlying Floridan aquifer system (Wedderburn et

al., 1982).

Undifferentiated Coarse Siliciclastics

A thick sequence of coarse quartz sand and gravel is present

in Hendry and Collier Counties which, in the past, has been

informally called the "Miocene coarse clastics" and placed in the

upper part of the Hawthorn Formation (Peacock, 1983) or Peace River

Formation of the Hawthorn Group (Knapp et al., 1986; Smith and

Adams, 1988; Campbell, 1988). In addition to being informal, the

term "Miocene coarse clastics" is misleading as at least part of

this unit is probably Pliocene in age. Three cores (W-16329, W-









16434, and W-16505) (Figures 3, 5-6, 8, 10), all had a thick

sequence of coarse siliciclastic material present overlying the

Peace River Formation. These siliciclastics are

uncharacteristically coarse for the Peace River Formation, and have

been referred to as undifferentiated sands, clays and shells until

further information becomes available for the area.

Smith and Adams (1988) report that these coarse siliciclastics

form a northeast-southwest trending trough on top of the fine sands

and silts of the Peace River Formation in Hendry and Collier

Counties. These three cores fall along the axis of this trough.

The top of the coarse siliciclastics in these three cores range

from approximately 50 to 70 feet below NGVD, with a thickness of

290 to 300 feet (Figures 8 and 10). These thicknesses are

considerably greater than the ones shown by Smith and Adams (1988).

This may be due to the fact that large portions of the recovery in

the coarse siliciclastic section consists of cuttings which have

been homogenized and have potentially had fine grained matrix

material washed out during drilling, thus making the contact

between the base of the coarse siliciclastic material and the top

of the Peace River Formation difficult to pick with certainty.

Tamiami Formation

The Tamiami Formation of Parker (1951) and Parker et al.

(1955) has been restricted by later authors .(Hunter, 1968; Hunter

and Wise, 1980 a and b; Scott, 1988). The Tamiami as used in this

report reflects these changes and consists of the Ochopee and

Buckingham Limestone Members and the Pinecrest Sand Member. Some








difficulty arises in identifying the Tamiami where sand sediments

are devoid of shell material and recognizable limestone units are

not present.

The Tamiami consists primarily of yellowish gray, shelly,

quartz sandy, slightly phosphatic limestone with calcilutite or

recrystallized calcite matrix. Molds of aragonitic fossils are

common. Quartz sand, shell content and induration are variable.

The top of the Tamiami Formation in the area ranges from a

high of approximately 25 feet above NGVD in eastern Lee County to

as much as 45 feet below NGVD along the coastal portions of Lee

County (Wedderburn et al., 1982), and as much as 60 feet below NGVD

in southeastern Hendry County. Elsewhere the Tamiami is found

primarily between 0 feet NGVD and 20 feet above NGVD (Knapp et al.,

1986; Smith and Adams, 1988). The Tamiami Formation is missing in

the northwest and northeast corners of Hendry County (Smith and

Adams, 1988). The Tamiami Formation was encountered in all of the

cores except for W-16329 (Figures 2, 4-10), where it is apparently

absent. The top of the Tamiami Formation was picked as being a

moderately sandy to very sandy yellowish gray shelly limestone with

numerous fossil molds. In W-16523, the Tamiami Formation was much

sandier than in the other cores. In this core, the Tamiami

Formation is a very calcareous, slightly phosphatic, fine grained

quartz sand.

Caloosahatchee and Fort Thompson Formations

The Caloosahatchee and Fort Thompson Formations of previous

usage are undifferentiated in this report due to the lack of









lithologic characteristics on which to differentiate the units.

These units were originally defined based on the fossils they

contain. The fossiliferous sands and carbonates of these units are

often less than 10-feet thick. The undifferentiated Caloosahatchee

and Fort Thompson Formations are present in two of the cores from

the study (W-16387 and W-16505) (Figures 4, 6, 8 and 10). These

formations are poorly represented in these cores. The tops of

these formations were picked as a moderately to highly

recrystallized, slightly sandy, fine-grained limestone.

Undifferentiated Sands, Clays and Shells

Undifferentiated Pleistocene-Holocene age sediments overlie

the Caloosahatchee-Ft. Thompson sediments or the Tamiami Formation

in each of the cores from this study. These sediments vary from

unfossiliferous quartz sands to very fossil.iferous sands and shell

beds, thin "marl" beds and organic-rich sediments. The undif-

ferentiated sediments generally occur as thin beds less than 10-

feet thick. However, along the coast these units can exceed 20-

feet thick.

Sediments belonging to the undifferentiated coarse

siliciclastics, Tamiami, Caloosahatchee and Ft. Thompson Formations

and the undifferentiated sands and clays comprise the surficial

aquifer system (Wedderburn et al., 1982; Knapp et al., 1986; Smith

and Adams, 1988). The surficial aquifer system contains two

aquifers, the water table and lower Tamiami which are separated by

a leaky confining zone (Tamiami confining beds).

CORE AND CUTTINGS-DESCRIPTIONS








Lithologic descriptions utilizing the Well Log Data System

were made for the six cores drilled for this study and entered in

the Florida Geological Survey's wellfile data base. A binocular

microscope was utilized in describing the lithologic

characteristics of each of the cores. The major characteristics

described and recorded included sample color, porosity, lithology,

induration, cement type, accessory minerals, and fossils.

Formation tops were determined based primarily on lithologic

criteria. Rock colors were based on the Geological Society of

America's Rock Color chart (Geological Society of America, 1984).

Appendix I contains complete lithologic descriptions of each of the

six cores described in this study.

RADIOCHEMISTRY AND X-RAY DIFFRACTION STUDIES

In addition to the microscopic description of the cores,

selected samples from one of the cores, W-16242, are currently

being analyzed for their uranium concentration and U234/U238 activity

ratio as part of the research for a Master's thesis at Florida

State University. As part of this thesis, it was decided to

analyze the bulk mineralogy of these samples in order to determine

what relationship, if any, the mineralogy has with the distribution

of uranium within the sediments. For this reason, each of the

twenty-six samples chosen for uranium work was analyzed for bulk

mineralogy by means of an x-ray diffractometer (XRD). The clay-

sized fraction from each of these samples will be analyzed in order

to determine the specific clay minerals present.

Selected intervals from the remaining five cores from this








study were also sampled for XRD analysis of their bulk mineralogy.

Due to the presence of thick intervals of coarse siliciclastic

material in three of the cores, (W-16329, W-16434 and W-16505)

there are large gaps in the intervals chosen for XRD analyses of

bulk mineralogy. In general, the intervals chosen for XRD analysis

were those in which the mineralogy was uncertain based upon visual

inspection of the core under a binocular microscope. X-ray

diffraction studies are useful for the identification of the

various minerals in a sample, but are semi-quantitative, at best,

for determination of the mineral abundance or percentage. In order

to analyze the bulk mineralogy of the samples, approximately 20-30

grams of the sample was ground to a fine powder. This procedure

insured homogeneous mixing of the sample and reduced the chance of

preferential orientation of certain minerals during analysis. A

split from the sample was then placed in a planchet (sample holder)

and placed into the x-ray diffractometer. The diffractometer

records the x-ray reflections as peaks, both in digital and analog

form. Every mineral exhibits a characteristic series of peaks,

which are used to determine the presence of the mineral. The x-

ray pattern for each sample begins at a 2-theta angle of four

degrees so that all major mineral peaks could be identified.

The results of the XRD analysis are listed in Table 1. The

sample depth is listed in the first column of each table. The

subsequent columns are for the minerals identified. Mineral

abundances were determined from the relative peak heights. When

possible, estimates of relative abundances were made, with 1, 2,








3... representing abundance in descending order. Two forms of

calcium carbonate (Caco3), calcite and aragonite, are common, and
-
dolomite, a calcium-magnesium carbonate, (CaMg(C03)2) is also

common. Phosphate minerals are present in numerous samples. The

type of phosphate abundant in sediments from the Hawthorn Group in

the area is carbonate-fluorapatite, (Calo(PO4)6(F, OH, CO3)2,

commonly known as francolite (Cathcart, 1989). This mineral is a

form of apatite in which fluorine and carbonate ions partially

substitute for hydroxyl groups.

CONCLUSIONS

This project has resulted in the addition of over 180

additional lithologic descriptions to the computer data bases of

the FGS and the District. The cores drilled provide much needed

"anchor points" for stratigraphic and hydrogeologic projects and

fill critical gaps in the geologic data base. These sample sets

will be utilized in future studies, providing an ongoing benefit.

The Hendry County cores drilled for this project are the only cores

in Hendry County at the present time. Additional core drilling

projects are needed in this and other portions of the District to

fill the gaps in the geologic data base and provide a better

understanding of the geohydrologic framework of southern Florida.









SELECTED BIBLIOGRAPHY


Campbell, K.M., 1988, Summary of the geology of Collier County,
Florida: Florida Geological Survey Open File Report 25, 14 p.

Cathcart, J.B., 1989, Economic geology of the land pebble phosphate
district of Florida and its southern extension, in Scott,
T.M., and Cathcart, J.B., editors, Florida Phosphate Deposits,
Field Trip Guide Book T178, 28th International Geological
Congress, p. 18-38.

Geological Society of America, 1984, Rock color chart: The
Netherlands, Huyskes-Enschene.

Hunter, M.E., 1968, Molluscan guide fossils in Late Miocene
sediments of southern Florida: Transactions, Gulf Coast
Association of Geological Societies, Vol. xviii, p. 439-450.

1978, What is the Caloosahatchee Marl? Hydrogeology
of South Central Florida, Southeastern Geological Society,
Publication No. 20, p. 61-88.

and Wise, S. W., 1980a, Possible restriction and
redefinition of the Tamiami Formation of South Florida.
Points of discussion: Florida Scientist, Vol. 43, Supplement
No. 1, p. 42.

1980b, Possible restriction and
redefinition of the Tamiami Formation of South Florida:
points of further discussion, in Gleason, P.J., ed., Miami
Geological Society, 1980 Fieldtrip Experience, p. 41-44.

Klein, H., Schroeder, M.C., and Lichtler, W.F., 1964, Geology and
ground-water resources of Glades and Hendry Counties, Florida:
Florida Geological Survey Report of Investigations 37, 101 p.

Knapp, M.S., Burns, W.S., and Sharp, T.S., 1986, Preliminary
Assessment of the ground-water resources of western Collier
County, Florida: South Florida Water Management District
Technical Publication 86-1, part 1, 142 p.

Missimer, T.M., 1978, The Tamiami-Hawthorn Formation contact in
southwest Florida: Florida Scientist, Vol. 41, No. 1, p. 33-
39.

Parker, G.G., 1951, Geologic and hydrologic factors in the
perennial yield of the Biscayne Aquifer: Journal of the
American Water Works Association, v. 43, pt. 2, p. 817-834.

Ferguson, G.E., and Love, S.K., 1955, Water resources
of southeastern Florida: U.S. Geological Survey Water Supply
Paper 1255, 965 p.








Peacock, R., 1983, The post-Eocene stratigraphy of southern Collier
County, Florida: South Florida Water Management District
Technical Publication 83-5, 42 p.

Peck, D.M., 1976, Stratigraphy and paleoecology of the Tamiami
Formation in Lee County, Florida: M.S. Thesis, Florida State
University, 249 p.

Slater, D.H., Missimer, T.M., Wise, S.W., and O'Donnell,
T.H., 1979, Stratigraphy and Paleoecology of the Tamiami
Formation in Lee and Hendry Counties, Florida: Gulf Coast
Association of Geological Societies Transactions, Vol. 29, p.
328-341.

Scott, T.M., 1986, A Revision of the Miocene lithostratigraphic
nomenclature, southwestern Florida: Transactions, Gulf Coast
Association of Geological Societies, v. 36, p. 553-560.

1988, Lithostratigraphy of the Hawthorn Group
(Miocene) of Florida: Florida Geological Survey Bulletin 59,
148 p.

Slater, D.H., 1978, The stratigraphy and paleoecology of the
Tamiami Formation in Hendry County, Florida: M.S. Thesis,
Florida State University, Department of Geology, 163 p.

Smith, K.R., and Adams, K.M., 1988, Ground-water resource
assessment of Hendry County, Florida: South Florida Water
Management District Technical Publication 88-12, part 1, 109
p.
Wedderburn, L.A., Knapp, M.S., Waltz, D.P., and Burns, W.S., 1982,
Hydrogeologic Reconnaissance of Lee County, Florida: South
Florida Water Management District Technical Paper 88-2, part
1, 192 p.








TABLE 1

BULK X-RAY DATA FOR SELECTED INTERVALS


Well 16242


SOUTH SEAS #1 CORE


Calcite Aragonite Dolomite


Francolite Clay


Depth
(feet)

41.5
47.0
52.0
60.0
63.0
70.0
80.0
85.0
90.0
100.0
115.0
159.0
252.5
291.0
354.0
400.0
436.0
515.0
546.0
553.0
575.0
639.0
727.0


KEY

The numbers 1,2,3,4... refer to the relative abundances
according to the relative intensities of the XRD pattern in
the bulk analyses.


?=probable (not positive ID)


Quartz


2
2

2
3
2

3
1
tr
tr
2
2
1
2
tr
2
2
tr
2


3?


tr= trace amounts








HILLIARD #1 CORE


Depth
(feet)

77.5
415.0
438.0
470.0
550.0
596.8
645.0


Quartz Calcite


Well 16387


Depth
(feet)

32.0
98.0
141.0
204.0
262.0
316.0
378.5
443.7
511.3
581.5
608.0
640.0


Aragonite


Dolomite Francolite


U.S. SUGAR #1 CORE


Quartz Calcite Aragonite


Dolomite Francolite


KEY

The numbers 1,2,3,4... refer to the relative abundances
according to the relative intensities of the XRD pattern in
the bulk analyses.


?=probable (not positive ID)


Clay


3


1
1
2


Clay


Well 16329


tr= trace amounts








IMMOKALEE # 1 CORE


Calcite


Aragonite


Dolomite Francolite


Well 16505

Depth Quartz
(feet)


FAKAHATCHEE STRAND # 1 CORE

Calcite Aragonite Dolomite Francolite


370.0
400.0
590.8
673.0
681.5
697.5


KEY

The numbers 1,2,3,4... refer to the relative abundances
according to the relative intensities of the XRD pattern in
the bulk analyses.


?=probable (not positive ID)


Depth
(feet)

140.0
188.0
498.0
510.0
573.0
631.0


Quartz


1
1
3
3
2
2


Clay


Clay


Well 16434


tr trace amounts








KORESHAN # 1 CORE


Calcite Aragonite


Dolomite


Francolite Clay


KEY


The numbers 1,2,3,4... refer to the relative abundances
according to the relative intensities of the XRD pattern in
the bulk analyses.

tr=trace amounts ?=probable (not positive ID)


Quartz


1
1


Depth
(feet)

57.0
89.0
173.0
336.5
518.7
531.0
578.0
793.0


Well 16523

























KEY
* CORES DRILLED FOR STUDY
PREVIOUSLY DRILLED CORES


LOCATION MAP FOR STRATIGRAPHIC COLUMNS
AND CROSS SECTIONS


.... 4 I~






FIGC l.


COMMENTS

noll
SANDY
2:iovF-r


FEET

- 0
*NGVD



- 20




- 40




- 60


vnMo, no


Ch


SOUTH SEAS ttf CORE


LOCATION,
COUNTY LEE
T 45S R 21E S 26
LAT= N 26D 31M 29S
LONG= V 82D 11M 29S
TD. 760'
ELEVATION, 02'


OISYI,C:

0130, VI,2 ____


VAR:CQMY .


HATCHING PATTERN KEY


NO SAMPI F


FILL



SILT/ V.F. SAND


FINE SAND


SANDY SHELL BEDS


SHELLY SAND


W-16242


UDSC
P. RECOV
Y' C,M
CU,Y1Z3_
NO, OVA
"nuns.


- 0B


--100
-tao




- 120



-- 140



-- 160


- 200


Y37,n


C2MOY3





2 IOMIlY?


050Z0I'Y
0,Y3,M
CIOY3Z


"'*"'
"~*:'''
.a;
::ii


~tgj~






240




260





2-- 80


''


.~


.,
i




;
r' L


PCRV


Y2CSMT


R IHDRI~li


- 300





-320





- 340


SCSX2Y:72

C2YIOZR



010YICS5



T3CUSY5
Y705(:




040Y2 .VA
Y25, r n
Vs a, Y.

. 040Y30 A
V I'.CZ, A

Shon400Y?

MO05.







nivi
nY i,, ,



05Y3D, n-r


MDI r T




flyYI


fly IfYI,1


VI fl1'Wf


360




-- 380





400





420




440


CLAYEY, SIIELLY SAND



DOLOMITIC SAND



PHOSPHATIC, CLAYEY SAND




PHOSPHATIC, SANDY CLAY



SANDY LIMESTONE



FRESH WATER LIMESTONE



PHOSPHATIC, S.NDY LIMESTONE



MUDSTONE



PACKS TONE/VACKESTONE



GRAINSTONE



MOLDIC LIMESTONE



MOLDIC DOLOMITE



BLDSIL!T/ FINE CRYSTALLINE I



P10'SPHATrT., SANDY DnLUMITE







- 460
VYIS3MO

VA CLAY

n t V-.l Mo FnPRMATI.ti ABBPRE\/V AT !I'
--480
Y101 UDSC = UNDIFFERENTIATED SAND, CLAY AND

Y- Vf 5P TMINM TAMIAN:I FORMATION
500- PCRV = PEACE RIVER FORMATION
- 500 viOQlOMo
ARCA = ARCADI, FORMATION

Yton v:M SWNN = SUVANNEE LIMESTONE

- 520
_- SYv20M

ARCA

- 540 V3us5r,D
VnYGI1Y35



- 560 VYX2CTo
"D,C,H,VF



-- 500 -
015V1

Y205
- 600 Y405

Y5020IR5


- 620
VY505,MO

YVI2V:MO

Y0I|V:MD
- 640
Y5015,C


02YIT,P
-- 660 2YITP
NIIPLS

Viol


- 690


Mnflt O








_DCm ,VT
52 COMMENT KEY

- 580 -
0 A= CALCAREOUS
01SYI B= CHERT
C CLAY
S Y205 D= DOLOMITE
- 600 Y405 Gm GYPSUM
H= HEAVY MINERALS
I- IRON STAIN
Y5020R5 J= MICA
L- LIMESTONE
-- 620 M CALCAREOUS MUD
Pa PYRITE
Y0 5a,1M 0= XUARTZ SAND
Y ~ 02vOmiO R- CALCITE SPAR
T= SILT
- 640 YlVIoIVO X= PHOSPHATE GRAVEL
Y501s5, Y= PHOSPHATE SAND
Z= SHELLS
BIOT- BIOTURBATED
02YIT,P CU CUTTINGS
- 660 HMOI HOLDIC POROSITY
VI = VUCIULAR POROSITY
S~ SPLS Vi= VERY, e.g. V4MOe VERY MIl
VIO 0O01 TRACE
_____ 7. IUCSTIONABLE
- 680 VAm VARIABLE
SHI HIGHLY RECRYSTALLIZED
LOW LOV RECRYSTALLIZATION
NOLDIC REXT- RECRYSTALI SIZED
C-Go COARSE 1T GRANULE SIZE
S700 3 M-C= MEDIUM Tn COARSE SIZE R
SMOLDoICr V-C VERY FINE Tn MICROCRYSI
POORRpF PERM= POSSIBLY HIGH PERMEABII I
Ci, m MUD= 4UDSTt~N
WAC= VACKE SIIRIE
IP r vF N PAC= PACKS TII
SMD,REXT
MniDIC
-| NOTE:
740 mn or ALL MNUMERS IN COMfMNTS
REFER TO PERCENIAiES

v!m nit, NGVvS NATIONAL G Fne TIC VERTICAL

FOR MORE DETAILED INrTmnATitN
tlN r T CfRt lW rPRIPTlNW










FIGURE 3


W-16329


HILLIARD #1 CORE


COHMENTS


I-mi~


FINE


FEET

0



-20
- NGVD


- 40



-60


upsc


- Z20,C2,Y
22s,120
NOSPL.S
X3,Y2,CU


LOCATIONt
COUNTYi HENDRY
T 44S R 32E S 16 B
LAT= N 26D 39M 50S
LONG= V 81D 08M 18S
T.D. 740'
ELEVATIONs 25'


: VIJl


HATCHING PATTERN KEY


,i SAAPLCS


SILT/ VJF. SAND


FINE SAND


MEDIUM SAND


Yp,CS,J1


80



100



120



140


CU, Y4,CI


-: vc


160



- 180


Y:',CI,VF


"'

' :
:;' ~ ;






















































MT.. Yrl t oi


I


Y2,CI,VF


- 180


- 200




- 220




- 240




- 260


A4. r...4.F -


UDSC *
IaaB~g


I
; il: (



r C,VI,A




F-C,A,C


Y1,010s,A

VA


y.t mln Il
('130," s I


- 280


- 300


- 320




- 340




- 360




--- 'm


'P.'














.I.


MEDIUM SAND



COARSE SAND



LIMY SAND



PHOSPHATIC SAND



PHOSPHATIC SAND AND SHELLS



PHOSPHVTIC. CLAYEY SAND




CLAYEY, SHELLY SAND



LIMY, SHELLY SAND



SANDY CLAY



PHOSPHATIC. SANDY CLAY



PHOSPHATIC, SANDY LIMESTONE



SANDY LMESTONE



MUDS TONE



PHISPIIATIC. SANDY XLfINtTE


*


~t~t~





















PCRV


VI-,H.',H
U.pS,V4,I





2lSY4YZ1:
Y1 ., A I



DIS;91A T
I IOUbY. I

M-S.YIU
Olu15Y I0



&USY ISC?



D1COY7

I'(NY 10,D

Y35rS,l

6S.,r !, V50
Y I2r 'A


I.JI.Y2
YSOI-,A
Y21,I ,MU

I30Y ITC
TUICOYtXI

Y2,T


- 380


PHOSPHATIC, SANDY DOLOMITE *



PHOSPHATIC, SANDY, CLAYEY DOLOMITE



DOLOSILT/ FINE CRYSTALLINE DOLOMITE







FORMATION ABBREVIATIONS:



UDSC UNDIFFERENTIATED SAND, CLAY AND SHELLS
PCRV = PEACE RIVER FORMATION
ARCA = ARCADIA FORMATION




* NOTE'
THE SEDIMENTS IN THIS INTERVAL
ARE UNCHARACTERISTICALLY COARSE
FOR THE PEACE RIVER FORMATION.
FOR THIS REASON THEY HAVE BEEN
DESIGNATED AS UNDIFFERENTIATED
SANDS, CLAYS AND SHELLS UNTIL
MORE INFORMATION FROM THE AREA
IS AVAILABLE.


- 400


- 420


-- 440'




- 460




- 480




- 500


- 520


540




- 560


- 580


ll lY',,lA lI








COMMENT KEY


--- 560 ?





- 580




- 600




- 620




640




- 660










700


03 Y5 VF
T315YlCBS
1UIoYSX1

Y2, T


YIT,D?'

1, Y5,
T., 02Y1M



1 01 Y '1'

030Y7Y I
OBYbvY?

A94.2b. !,'




litaUl!f
O(:YSBDOb








Sl'ir i.



P,,,j Ill i
Y-D-, -,,VF







I Iir.Yv. (
'...1ni i n


ALL NUMBERS IN COMMENTS
REFER TO PERCENTAGES


NGVD- NATIONAL GEDBETIC VERTICAL DATUM

FOR MORE DETAILED INFORMATION
CONSULT CORE ESCRIPTIIN


ARCA


Az
b-
C=
D=


1=
J=
G-
L=
M=
P=
01
RA
T=



BLOT=
CU-
NM=
VU=
Via
00=
?=
VA=
HI=
LOV=
REXT=
C-G=
M-C.
V-0=
PERM=
MUD=
VAC=
PAC=


CALCAREOUS
CHERT
CLAY
DOLOMITE
GYPSUM
HEAVY MINERALS
IRON STAIN
MICA
LIMESTONE
CALCAREOUS MUD
PYRITE
QUARTZ SAND
CALCITE SPAR
SILT
PHOSPHATE GRAVEL
PHOSPHATE SAND
SHELLS
BIOTURBATED
CUTTINGS
MOLDIC POROSITY
VUGULAR POROSITY
VERY. e.g. ViMO VERY MOLDIC
TRACE
QUESTIONABLE
VARIABLE
HIGHLY RECRYSTALLIZED
LOV RECRYSTALLIZATION
RECRYSTALLIZED
COARSE TO GRANULE SIZE RANGE
MEDIUM TO COARSE SIZE RANGE
VERY FINE TO MICROCRYSTALLINE
POSSIBLY HIGH PERMEABILITY
MUDSTONE
VACKESTONE
PACKSTONE


- 720




.. 740









W-16387


FIGURE 4


COMMENTS


U,S, SUGAR CORE

U.S. SUGAR #tt CORE c


.1, UDSC LOCATION,
COUNTYi HENDRY
T 44S R 34E S.09 B
v:,,lIII FTMP/CALOOS LAT= N26D 40M 55S
LONG= 8BOD 56M 13S
T.D. 662 FEET
ELEVATION, 14'
T.D. 662'


- 0


- NGVD
- 20




40



- 60




I-- 80


NO SAMPLES


FILL



SILT/ V.F. SAND



FINE SAND



MEDIUM SAND



SANDSTONE



PHOSPHATIC SAND



PHOSPHATIC, SANDY CLAY


FEET


HATCHING PATTERN KEY


- 100




- 120


- 140



-- .160








200


1.1, ,A'llr

I M,A


V.N111o. i
............. JL i


V I *I :i



t U ',


V ,,l .1


'




- 2n0




- 240




260




280




300


- 320


-- 340




--360




- 380


litI. 1.y **L,


'IEfi F Jii "


IA lV I ,A
y:.,,V:t


PCRV


VI*, VI t.

Y*sc, VF




VF-F





_ v.',tA


DOLOMITIC CLAY



SANDY CLAY



SANDY LIMESTONE



HOLDIC LIMESTONE



HUDSTONE



PACKSTONE/VACKESTONE



CLAYEY LMESTONE


INTEREDDED LL AND IOLMIITE



SANDY DOLBTE



LODS.IT/ FwE CRTSTALLINE DOLOMTE


ul.'ot I,D
1I IP... tlF D

1IIl'- l0, T



VI'l.. Wi ,


- 400


-FORMATION ABBREVIATIONS:


T/CSL *
FTMP/CALOUS w


TMH
PE"K
ARCA


UIFTERENTIATE SANR CLAYT n SMELLS
UtMFCERENTMTE FORT TitmPSM/

TAMRIMW ruMTMI
PEACE oIVER fIMav W
rCAMA ra rrmWTm


- 4?0


-- 440


ill'.. IA




.1. T .1
sr.. ,,, l.j


- 4", I


1:1,- IiVF





COMMENT KEY

480 U03:'I I A- CALCAREOUS
SB CHERT
C= CLAY
0 t'XY2 D= DOLOMITE
:-oY2c G= GYPSUM
500 L y*,,,.vo Hu HEAVY MINERALS
: Q1,.,- I= IRON STAIN
J= MICA
L= LIMESTONE
fiSYST M= CALCAREOUS MUD
520 P, PYRITE
Q= QUARTZ SAND
Y2S,CV-F R= CALCITE SPAR
ARCA T= SILT
X- PHOSPHATE GRAVEL
540 2OYM Y PHOSPHATE SAND
Z= SHELLS
BIOT= BIOTURBATED
CU= CUTTINGS
MO= MOLDIC POROSITY
560 025Y I0s VU VUGULAR POROSITY
T2003 V= VERY, e.g. VMO= VERY MOLDIC
00- TRACE
Ei A 7= QUESTIONABLE
05Y1 VA= VARIABLE
580 0ST HI- HIGHLY RECRYSTALLIZED
S02S2T25 LOVI LOV RECRYSTALLIZATION
i, V, c REXT= RECRYSTALLIZED
S 01YVF-F C-G= COARSE TO GRANULE SIZE RANGE
Q1Y1T M-C= MEDIUM TO COARSE SIZE RANGE
- 600 V-O= VERY FINE TO MICROCRYSTALLINE
S' YTPERM= POSSIBLY HIGH PERMEABILITY
Sy m MUD= MUDSTONE
VAC= WACKESTONE
6 y" IPAC= PACKSTONE

:' NOTE'
a1YACM
..PS ALL NUMBERS IN COMMENTS
:-640 lBo -REFER TO PERCENTAGES
01VY4", C

nv "IYCMO NGVD- NATIONAL GEODETIC VERTICAL DATUM
- 660. 057, M
FOR MORE DETAILED INFORMATION
CONSULT CORE DESCRIPTION.

- 680





FIGURE 5

S/V-16434


FEET


IMMOKALEE #1 CORE


COMMENTS


F-M,SOIL
VFF,C UDSC
f4uZ25m1L
o, 010.)o'

: TM,0,n


--NGVD


40 .




- 60




-80


21 CCIi


C2P11%.LSY

M85,'VA


M1oz3 2C,


LOCATION,
COUNTY' COLLIER
T 47S R 30E S 03 B
LAT= N 26D 25M 28S-
LONG= V 81D 18M 28S
T.D. 715'
ELEVATION' 25'


Mn, Us-.20
SN,o2o0-4.


HATCHING PATTERN KEY


MIOZSY2C


IQ1 SMULU


;zvazu


TI'.C2YI



TI,.C2Yl


dCYITS
T.*,ZSClY


NiOSPLS


h. ..g ,*.
4;' ..


I 1 '"


SLT/ VF. Sam



FI E SW



P63" SAM



CIom -F



P rrS"


- 180



- 140


-- I60


- Io


- 2"


O I-I-.-:.:.


U7 7' "












- 220


X.,c vc


PjaSip.


- 240




- 260 .....




- 280 '







-.-' r


- 340




- 360


- 380


Y.',M c;



r, Y.', .


,I: l)'Y I


*1! mnn


UDSC m


U


M::Y*',I'





i, .Y", r m


XI Y3Hi; ;'
D.' ;:,X.
nnv.'X1


- 400


PHOSPHATIC, CLAYEY SAND



LIMY SAND



LINY, SHELLY SAND


CLAYEY SAND



SANDY CLAY



PHOSPHATIC. SANDY CLAY



SANDY LIMESTONE



PHOSPHATIC. SANDY LIMESTONE



HUDSTONE



PACKSTONE/VACKESTONE



SDOLOSILT/ FINE CRYSTALLINE DOLOMITE



PHOSPHATIC, SANDY DOLOMITE


PCRV





,,' ,. .,' .



i;;'



'*r. : ',.




S 400 "' PHOSPHATIC, SANDY DOLOITE
D.r:, X1
.- PCRV
C I YSL )

i -M;:.SZ- FORMATION ABBREVIATIONS:

1M(|Z 1 .111
UDSC UNWlFERCmATED SAND CLAY ANM SHELLS
THIN TANIAMI FOATION
v ,,Mi PCRV PEACE RIVER FORMATION
- 460 Mi | ,'".- nACA ARCAM A FOMATION

II, y., I11

-- 43 NOTE:
vYmUIj .-.'. 'THE SrEBBANS I IMtS IMNTi 'WAL
S r ARE UWCHACTERISTICALL COARSE
SFOR THE PEACE RIVER FORIATEI
S1,: aFOR nrs REASuO, WE mWVE EE
500 uoS.cP INE MTE AS iWFFERONTIOATE
K 1 SAMIS CLATS AN SHELLS WmTIL
,!"I a V.1ISS AVAILABLE.

52 P KI. Y,.-PI






crn





nIo, v.1,l COMMENT KEY
Y30, T
540 3s A= CALCAREOUS
S Y anil' B= CHERT
C= CLAY
Y2D D= DOLOMITE
Y IItoletX t G. GYPSUM
60 S Y:IOuoxX H= HEAVY MINERALS
I IRON STAIN
1YIOC x-a J= MICA
ARCA L= LIMESTONE
O, C,,D MH CALCAREOUS MUD
580 P= PYRITE
Ma y 1 YiM'.... O QUARTZ SAND
"+ tY1R= CALCITE SPAR
i H IT= SILT
1 5'1a *.- .1' X= PHOSPHATE GRAVEL J
600 :lT:o,D" Y= PHOSPHATE SAND
Z= SHELLS
BIOT= BIOTURBATED
u T i.aP" CU= CUTTINGS
MO= HOLDIC POROSITY
620 A VU= VUGULAR POROSITY
'xi :. Rl Vi= VERY. e.g. VMO= VERY MOLDIC
00= TRACE
"l e. Vii QUESTIONABLE
: Min .VA= VARIABLE
640 ?% (I, Y.I HI= HIGHLY RECRYSTALLIZED
II! a LOV= LOV RECRYSTALLIZATION.
+g '. Pj My:: REXT= RECRYSTALLIZED ,
I' Ml[, ol#Y!, C-G= COARSE TO GRANULE SIZE RANGE
.i'i^ NMiHIn.> M-C= MEDIUM TO COARSE SIZE RANGE
660 V--O VERY FINE TO MICROCRYSIALLINE
SS PERM= POSSIBLY HIGH PERMEABILITY
'.' <:, MUD= MUDSJONE
VAC= VACKESTONE
.. 1 .'. PAC= PACKSTONE
68o :L N .

NOTE:
S rtln', 'IlIX
P o ."- ALL NUMBERS IN COMMENTS
REFER TO PERCENTAGES

""Mil,'eh "
*' I ; : I .
- 720 NGVD= NATIONAL GEODETIC VERTICAL DATUM

FOR MORE DETAILED INFORMATION


Y LUSNlfC CORE DES N.








FIGURE 6


W-16505


COMMENTS


M20, C UDSC
020021 10 T /CAIIOS
OIOI IfRU


cuv:Y
CU, 0CYZ


HORIcn l0


- 0


- NGVD
- 20



- 40



- 60


Ho, UY1W
no,YIn2O
X Y2M2Z2
VYWZ2CU
ajrcY212


HATCHING PATTERN KEY


NO SAMPLES


FIN3 SMS


REID" S"M


M3YIIIXI


FEET


FAKAHATCHEE STRAND #1 CO


LOCATION,
COUNTY, COLLIER
T 50S R 30E S 06 C
LAT= N 26D 08M 52S
LONG= V 81D 21M 28S
T.D. 702'
ELEVATION 13'


- 120


- 140


- t60


M2Y1
yvxtZl

M2ZlXtY2






M2Y~ItIXI


-.- 1t0


Im







180




200




220




- 240



- 260




- 280


M2YIZIX)






Mn-





ZIS1VC-G


020


UDSC n


Lii


- 300



- 320








360
-- 340. ;:



- 360'




- 380:




- 400


ZIOHIT

MOZ20RHY
MOY3M3OZ
MlCoY22
CU-450'





M20Y2,D?




D20Y2C2T


D=oYlCIT




D40YBCT


n.IOYBzr.

CI SD-.UYL


PCRV


COARSE %4ND



SANDSTONE



SLIMY SAND



D )OLOMITIC SAND


UNCONSOLIDATED SHELL BEDS



CONSOLIDATED SHELL BEDS



i SANDY CLAY



LIHY CLAY


SANDY LIMESTONE



MOLDIC LIMESTONE



PHOSPHATIC. SANDY LIMESTONE



M UDSTONE


PACKSTONE/VACKESTONE



GRAINSTONE



|f \PHOSPHATIC. SANDY DOLOMITE










380 D40YOCT s mo
GRAINSTONE


n0ioYSZrC PCRV
- 400 PHOSPATIC SANDY DOLOMITE
r 5D04JY5


D D-5Cl O lY HMOLDIC DOLOMITE
420

c FORMATION ABBREVIATIONS:

UDSC UNDIFFERENTIATED SANDL CLAY AND SHELLS
440 i.M5 '5
FTMP/CALOOS a UNDIFFERENTIATED FORT THOMPSON/
AL OOSAHATCHEE FORMATIONS
v"404, MJ THIN a TAMIAMI FORMATION

460 Mr~YR0ao PCRV m PEACE RIVER FORMATION
Y I YI-,'D ARCA ARCADIA FORMATION
Mu 1202
2,, Vs,*..i NOTE'
a l4804 r,1, r li THE SEDIMENTS IN THIS INTERVAL
0 ARE UNCHARACTERISTICALLY COARSE
FOR THE PEACE RIVER FORMATION.
vIM FOR THIS REASON THEY HAVE BEEN
DESIGNATED AS UNDIFFERENTIATED
SANDS, CLAYS AND SHELLS UNTIL
MICRE INFORMATION FROM THE AREA
- 50m0 S L, 113,PI IS AVAILABLE.

5MT )P15Y 1



MOR;ZP2Y2

Y15015
540 P ulltn
A25312
Yonn

560
ys8e ARCA
Y203, T





r):


COMMENT KEY

': P2 A= CALCAREOUS
5 20 ) B= CHERT
-- -C= CLAY
PIOR-P"Y2 D= DOLOMITE
G= GYPSUM
YV5015 11= HEAVY MINERALS
-540 M-Ylini 1= IRON STAIN
A5s31' J= MICA
L= LIMESTONE
Y8010 M= CALCAREOUS MUD
E MY50 P= PYRITE
560 Y50 ARCA 0: QUARTZ SAND
R= CALCITE SPAR
Y203,T T= SILT
Y" 50T X= PHOSPHATE GRAVEL
Y= PHOSPHATE SAND
- 580 M- MY 10( Z= SHELLS
SCY15015 BIOT= BIOTURBATED
CU= CUTTINGS
D30Y200 M= MOLDIC POROSITY
SM5Y2 VU= VUGULAR POROSITY
- 600 |- M Y3P2 V= VERY. e.g. VMO= VERY MOLDIC
Y2,'IO 00= TRACE
MOY305 7= QUESTIONABLE
VA= VARIABLE
MIOYIP HI= HIGHLY RECRYSTALLIZED
- 620 '- LOV= LOV RECRYSTALLIZATION
i REXT= RECRYSTALLIZED
yP3n C-G- COARSE TO GRANULE SIZE RANGE
M-C= MEDIUM TO COARSE SIZE RANGE
SY3ISP2 V-0= VERY FINE TO MICROCRYSrALLINE
- 640 PERM= POSSIBLY HIGH PERMEABILITY
MUD= MUDSTONE
M0Y7I AC= VACKESTONE
PAC= PACKSTONE

-- 660

YVi5nsvA NDTEI
."iyi3T iX' -
S y3010 ALL NUMBERS IN COMMENTS
--680 .-" M140Y5 REFER TO PERCENTAGES
Yo.. Tc
YooI?. TC
YIOO NGVD= NATIONAL GEODETIC VERTICAL DATUM
- 700 v vISZoxi
FOR MORE DETAILED INFORMATION
CONSULT CORE DESCRIPTION.





FIGURE 7


W-16523


KRESHAN CORE.
KORESHAN #1 CORE


FEET


COMMENTS


t.1.1 1
VI: c

L.4", lbHU
HI :', r
MISPI.B

nf30'l, H?


PCRV


HATCHING PATTERN KEY


AUAI.rr.a


nI'S-.I w-
VIO,?W... .. .. ..- -


;lasz,.+
- 0=X3l vt.I
bOCIa*Y2
YIN: t *.*t


- 180


n.~CI,: V







cr, ., .".*


CLATEV, SMELLY S1"



PNMSPWMTIC SA



I v *


LOCATIONs
COUNTY: LEE
T 46S R 25E S 33 A
LAT= N 26D 25M 58S
LONG= V 81D 49M 08S
T.D. 822'
ELEVATIONi 11'


-NGVD

- 20


UDSC


-- 40




-- 60




--80


NOY IC III
Y3M'~CI H
YmOf5IIa',~


M; A.3Y I

mIiov.ItU


- 120




--340


NO S.IPLES



FINE SL



SHELLY SMB


* ^1


-- 160


;~.:ri~;'~~'~':4
Ic ~rr I

-


















240




260




- 280




300




- 320




- 340




- 360




-- 380




- 400




- 420


EiI


f -Ilis 20ik:


S Y5,MI







AtADLUVL

6- YSHIMnI)




IJJvtICPaI.

Cii.Y III




3C I30 1




Y112-5/11 0
al i *:1 .1











YGX', IA
Y3CI'I'D

' Y70S5,10




Y3P1


F:. Y2Q3Rs5n

03Y2RSMO
YB P1

i Y?3RPHl^'
YtPlI'tI


::;:~
':::.:


PHOSPHATIC, SANDY LIMESTONE.



MOLDIC LIMESTONE



DILOCMITIC LIMESTONE



i M HUDSTONE



PACKSTONE/VACKESTONE



C.R.INSTONE



INTERBEDDED LS. AND DOLOMITE


t ". N5. '44


03T111
OI, J il'


CLAYEY SAND



DCLOMITIC SAND



LIMY SAND



LIMY. SHELLY SAND



PHOSPHATIC SANDY CLAY



DOLOMITIC CLAY



SANDY LIMESTONE










YIVGTlOrl



Y503TI I


-420




-440









-- 480


Y 15015C1
S020V20X
QISYISX3
Q5Y5X1
aSYSDX
TloalUcx
YVClXLll .






YlzU I'pj

ZV'>tlir.DT



MAC/PAL
- CcltWlp


Y3C2X1IHI
V Yt, 1H
YMPV4D
YIP11411O
Van 1Pgyg

YIPAC-MA






R30Y30PIO

Y3.2aullg
.t: PR
"l' -N Pil
ii:


I- ylPp, I


s INTEP.BEDDED LS. AND DOLOMITE



CLAYEY DOLOMITE



SANDY DOLOMITE



PHOSPHATIC SANDY DOLOITE



PHOSPHATIC, SANDY, CLAYEY DOLI



S OLOSILT/ FINE CRYSTALLINE IX






FORMATION ABBREVIATIC


UNFFERENTIATED SANK CLAY AND l
TAHMn FORMATION
PEACE RIVER FORMATION
ARCADA FORMATION
SUWANNEE LIMESTONE


ARCA


--500




- 5WO


- 540


UDSC *


PCRV a
ARCA a
SVNN -


-- 560


0- bO




,,ii ,iiiiii iiii i i 1 Y3. i, Mu
"- COMMENT KEIY Y

640 ''Y35.''Mo A= CALCAREOUS
8= CIdERT
C= CLA,
SlOH3IwavMO D= DOLC'IITE
0'o ,MO G= GYPSUM
S660 faia 3Y1 H= HEAVY MINERALS
05 aY111 1= IRON STAIN
1J= MICA '
( 07oY,Mu I.= LIMESTONE
M= CAL.CAREOJS MUD
-- 680 Ii P= PYRITE
gu QUARTZ SAND
vi i
SR CALCITE SPAR
YIaIMnLI T= SILT
u- Ub u X= PHOSPHATE GRAVEL
700 05, PER Y= PHOSPHATE SAND
a'H1l Z= SHELLS
Vu YUuIL BIOT= BIOTURBATED .I
CU; CUTTINGS
Y2a4R5nMn MHO MOLDIC POROSITY
720 VU= VUGULAR POROSITY
S030YIII V= VERY. e.g. VMO= VERY MOLDIC
05' 0 S ?= QUESTIONABLE
VA= VARIABLE
740 81 HI= HIGHLY RECRYSTALLIZED
020Y7rPO LOV= LOV RECRYSTALLIZATION ..i
1 QSS5'id REXT= RECRYSTALLIZED
C-G, COARSE TO GRANULE SIZE RANGE
02050YI M-Cm MEDIUM TO COARSE SIZE RANGE ,
760- V-0= VERY FINE TO MICROCRYSTALLINE
( rIY PERM= POSSIBLY HIGH PERMEABILITY
MUD= MUDSTONE
VAC= VACKESTONE
S 18540011 PAC= PACKSTONE ':
- 780 .

,--
-" 09, NOTE! :i

800 CM1 ALL NUMBERS IN COMMENTS
-Sao 02PI,nM SVNN LLi
REFER TO PERCENTAGES

H1IGH PERh NGVD= ;ATION4L GEODETIC VERTICAL DATUM

FOR MOPE DETAILED INFORMATION
CONSULT CORE DESCRIPTION.


- 840




"1






FMT TIme
fCMAiIMMT


SI


V-4157


Utn







-m3


-mJ





-.3O


-2W

-2W0






-430

-2W

-2W0


WBIN



































TU
LD
TN


0 2 4
NILES
VERTICAL SCALE 41 TIMES HORIZONTAL SCALE
FIGURE 8 CROSS SECTION A A'


V-I556


UDSC a


TD


TD

THE SEDIMENTS IN THIS INTERVAL
ARE CHARACTERISTICALLY COARSE
FOR THE PEACE RIVER FORNATML.
FOR THIS REASON THEY HAVE BEEN
DESIGNATED AS UDIFFERENTIATED
SAIDS, CLAYS, AND SHELLS UNTIL
HORE INFORMATION FROM THE AREA
IS AVAILABLE.


MM? 50

NVaI O




-UO
1: -59



-LM
-150

-20




-300




-400

-450

-500
I
-550

-600

-650
TD
-700

-750

-800


FEET


]


WVNNEE ?


PEACE IIVER
FIgT~aI


-~U -


FI T


-4- T









FEET B UDSC B' FEET
S50 W-15286 50
= W-16523 W -16146
S 0 tGVD liNGVD 0
TAMIAMI FORMATION
-50 T AMIAMI FORMATION -50 -

-100 -100 -
PEACE RIVER FORMATION PEACE RIVER FORMATION -

--150 -150

--800 TD -200 -

-850 -250 -

-300 -300

-350 -350 -

--400 -400

--450 -450 -
ARCADIA FORMATION ARCADIA FORMATION

-500 -500

--550 -550

-600 -600

-650 -650 -

--700 -700

-730 -750 -


S SUVANNEE LIMESTONE -
TD

I !
MILES

VERTICAL SCALE 416 TIMES HORIZONTAL SCALE

FIGURE 9 CROSS SECTION B '


43.




- -... :.. ~. .-.,-l....- ...* Y- ;:il.


C

V-16329

mNGV


Iz~


FEET
-50



-50

-100

--150

-300




-300




--400

-450




-550O

-.-00




-700

-750

00


FORT THOMPSON/
SC CALOOSAHATCHEE C'
UDSC FORMATIONS

W1643 V-16505
^^^.,. ,LJMfvn


TAMIANI FORMATION















PEACE RIVER FORMATION


p~,r I


50

0


UDSCb














ARCAA FORATION


'ET


Y I
-700
TD TD -700
THE SOCNTS IN THIS INTRVAL -750
A CHARACTERISTICALLY COARSE
OR THE PEACE RIVER FtRMATION
FOR THS REASON THEY HAVE IEN -800 -
SdGlNATEO AS UNWFERENTIATE
SANDS. CLAY& AND SHELLS UNTIL
M INFORMATION M THE AREA 0 2 4
IS AVAILABLE. I I
MILES
VERTICAL SCALE 416 TIMES HORIZONTAL SCALE

FIGURE 10 ROSS SECTION C C'


t


' 1


NG~V


-50

-100

-150

-200

-250

-300

-350

-400

-450

-S00

-550

-600

-650


"'''










FLRD GEOLOSk ( IC SUfRiW


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