|UFDC Home||myUFDC Home | Help ||
CITATION SEARCH THUMBNAILS MAP IT! MAP IMAGE ZOOMABLE
STANDARD VIEW MARC VIEW
Map Series No. 137
MINERAL RESOURCES OF SUWANNEE
Ronald W. Hoenstine, P.G. #57, Steven M. Spencer,
and Ed Lane
FLORIDA GEOLOGICAL SURVEY
WALTER SCHMIDT, STATE GEOLOGIST AND CHIEF
DIVISION OF RESOURCE MANAGEMENT
DEPARTMENT OF NATURAL RESOURCES
In recent years, considerable attention has been focused on Florida's rapid
development, the accompanying population increase, and their effect on the state's
important mineral resources. Frequently, this development occurred in areas underlain
by known mineral deposits, precluding extraction of the minerals. The economics
associated with these mineral resources represent substantial employment and income
to the private sector as well as taxes to county and state governments. One response
to this conflict between rapid population and urban growth, and Florida's mineral
resource development was in the form of legislation enacted by the Florida Legislature
in 1985 requiring each county to establish a comprehensive land use plan. Additional
guidelines and due dates were established by the 1986 Florida Legislature.
In response to this legislation, and at the request of the North Central Florida
Regional Planning Council, the Florida Geological Survey initiated this investigation of
Suwannee County's mineral resources. The objectives were to identify potential mineral
resource areas and to present the results in a format appropriate for use by city and
county planners. This mineral resource assessment is general and is intended as a
land-use planning tool. A site-specific evaluation would require detailed research
beyond the scope of this investigation.
A knowledge of Suwannee County's mineral resources is basic and integral to
the process of initiating, developing, and implementing an effective comprehensive land
use plan. This information is essential to planners and officials in their analyses of
urban and rural development in such areas as zoning, road construction and the
establishment of waste disposal sites.
Resource evaluation for this report is based on a number of sources including
Florida Geological Survey reports and unpublished data, core and well cutting
descriptions, geological logs, field reconnaissance, state and federal statistical data,
company reports, questionnaires, and discussions with mining company personnel and
state and federal officials. Although detailed information on company statistics is
confidential, information of a more general nature is readily available or can be
reasonably extrapolated from existing data. The diversity of sources as well as their
close association with the various aspects of resource evaluation lends substantial
confidence to the general assessments and inferences of this report.
Metric Conversion Factors
For readers who prefer metric units to the U. S. units used in this report, the
following conversion factors are provided.
Suwannee County lies entirely within the Northern (Proximal) Geomorphic
Zone, which encompasses much of northern Florida (White, 1970). Two major
geomorphic divisions occur in this zone within Suwannee County. These include the
Northern Highlands and the Gulf Coastal Lowlands (Figure 1).
The Northern Highlands occupies the east-central and northeastern portions
of the county. Here, various weathering processes (i.e., stream erosion and subsurface
dissolution) have played a key role in shaping the area's distinctive topography forming
undulating hills and ridges. Topographic highs in this area reach maximum elevations
of 185 feet above mean sea level (MSL).
This region has numerous small lakes and ponds. Most are karst features,
having formed due to the dissolution of the underlying limestone and the subsequent
collapse of overlying sediments.
The Northern Highlands is bounded to the west by the Cody Scarp, a
prominent escarpment named and described by Puri and Vernon (1964) as the most
persistent topographic break in Florida. In Suwannee County, the toe of the Cody
Scarp occurs at an elevation of approximately 100 feet above MSL.
Bordering the Northern Highlands to the west is the Gulf Coastal Lowlands.
Occupying approximately 60 percent of the county, the Gulf Coastal Lowlands lie in an
area bounded to the east and northeast by the Cody Scarp, to the southwest by the
Suwannee River and to the south by the Santa Fe River. Elevations here range from
approximately 100 feet above MSL along the Cody Scarp to less than 30 feet above
MSL along the Suwannee River at the Lafayette-Suwannee County boundary.
A number of terraces representing relict depositional features formed by ancient
seas are present in Suwannee County. Healy (1975) recognized three marine terraces,
based on elevation, in Suwannee County. These terraces are from highest to lowest:
the Coharie Terrace (170 to 215 feet above MSL), the Sunderland/Okefenokee Terrace
(100 to 170 feet above MSL) and the Wicomico Terrace (70 to 100 feet above MSL).
Figure 2 depicts the approximate location and areal extent of these terraces.
V.*.,.*.*.*.*.*.:-.*-.*... ..-...:.:.:... ...-...-.- .- ._
.....:.:......-.:... .. .
... ... ..
STAL LOWLANDS** ***
..... ....... ......
RP ". ................ ..... ...'o ... .. ...........
.. ...'; .. ." ...'.'.*.; .'.'.;; '.'.'.. '... ,.'.'.'.'.
................................ ....::::::::::::::::: :::::::::::
.. .. .. .. .. .. .. .. .. .. .
.. .. .. .. .. .. .. .. .. .
Suwannee County is part of a transitional geologic area that lies between the
thick, lower Tertiary (Paleogene) and Cretaceous carbonate sediments characteristic
of the Florida peninsula and the age-equivalent, predominantly siliciclastic sediments
of western Florida. The area is underlain by thick carbonate deposits of Eocene and
Oligocene age which are in turn covered by younger limestones and dolomites, sands,
silts and clays.
To date, the deepest penetration of subsurface sediments in the county is to
a depth of 4,424 feet below MSL in Hunter Petroleum No. 1 oil test well (Permit 724, W-
12246, section 16, Township 2S, Range 12E). Here, basement sediments consisting
of Paleozoic black shales are present at a depth of 3,630 feet below MSL (Applin, 1951;
Lloyd, 1985). These basement rocks are overlain by Mesozoic and lower to middle
Cenozoic Erathem carbonates (limestone and dolomite) measuring thousands of feet
in thickness. These carbonates are overlain in the near-surface by Neogene deposits
of fine- to medium-grained quartz sand, clayey sand, sandy clay, silt, limestone,
dolomite, and organic-rich (peat) sediments.
The oldest rock cropping out in Suwannee County is the Ocala Limestone.
This unit is exposed in pits, quarries and bottom sediments of the Suwannee River in
southern Suwannee County. The lithology is variable, ranging from a pale orange to
white, poorly to moderately indurated, moderately to highly porous, microfossiliferous,
partially dolomitized, partially recrystallized limestone. The Ocala Limestone, which was
deposited during the Late Eocene Epoch (41 to 38 million years before present, BP),
has an average thickness of 150 feet in Suwannee County (Florida Geological Survey
well data). The Ocala Limestone is an important potable water-bearing unit and
comprises an integral part of the Floridan aquifer system.
The Suwannee Limestone overlies the Ocala Limestone in much of the northern
two-thirds of the county, extending as far south as the area immediately south of the
town of McAlpin. Deposited during the Oligocene Epoch (38 to 33 million years BP),
these sediments have a lithology that ranges from an indurated, cream to yellow,
chalky, fossiliferous limestone over much of its area of occurrence to silicified boulders
in an area bordering the Suwannee River at the Suwannee River State Park.
Although extremely variable, the Suwannee Limestone averages 90 feet thick.
A maximum observed thickness of 115 feet occurred in Florida Geological Survey well
W-8780 (section 14, Township 2S, Range 13E). Where present, these sediments
comprise the top of the Floridan aquifer system in Suwannee County.
The Hawthorn Group unconformably overlies the Suwannee Limestone except
in areas where the Suwannee Limestone is missing, in which case it unconformably
overlies the Ocala Limestone. The Hawthorn Group, which primarily occurs in
northeastern Suwannee County, was observed in well cuttings to extend as far west as
an area approximately four miles south of the town of Falmouth (W-3846; section 15dc,
Township 2S, Range 12E). These Miocene age sediments were deposited
approximately 23 to 15 million years ago during the Early and Middle Miocene. The
Hawthorn Group contains a diverse lithology, consisting of phosphatic interbedded
sand, clayey sand, sandy clay, limestone and dolomite. These sediments are referred
to in the cross sections as Hawthorn Group Undifferentiated.
The majority of Suwannee County is covered by a veneer of Pleistocene anu
Holocene sands and clays referred to as "Undifferentiated Sand and Clay." Associated
with ancient sea level stands and lacustrine deposits, these sediments consist of fine-
to medium-grained sand, silt and clay. They overlie the Hawthorn Group in north-
central and northeastern Suwannee County. In the other areas of the county they
overlie the Suwannee Limestone or the Ocala Limestone. These sediments vary in
thickness from less than a foot in areas such as western Suwannee County along the
Suwannee River, to more than 50 feet in karst depressions developed in the Suwannee
Limestone or Ocala Limestone.
The purpose of the following discussion is to provide information on the
occurrence of certain economic mineral commodities in Suwannee County. The
information presented is not intended to be an exhaustive investigation leading to
immediate industrial development. However, where the information is favorable, it may
show that certain areas warrant further investigation. The Mineral Resources Map is
designed to present a geographic overview of the major economic mineral commodities
identified in Suwannee County. Factors such as thickness of overburden, quality, and
volume of the deposit could affect the mining of the mineral commodity at any specific
site. In contrast,' geologic cross sections were extrapolated from cores and well
cuttings to show the distribution and thickness of surface and near-surface stratigraphic
units (Figures 3b and 3c). As a result, occasional variations between the geologic
cross sections and the Mineral Resources Map may occur. The principal mineral
commodities discussed here include clay, limestone, peat, hard rock phosphate, and
Clayey sand deposits are scattered throughout Suwannee County. These
sediments are used as road construction material and, locally, as fill. Alluvial clay
deposits are present along portions of the Suwannee, Santa Fe, and Ichetucknee Rivers
(David Howell, United States Department of Agriculture Soil Conservation Service, SCS,
personal communication, 1991). These deposits are typically stratified with sands and
clayey sands. Extensive testing would be required to determine their full potential as
an economic commodity. There is currently little potential for a clay products industry
using local materials from Suwannee County.
Operators quarried the Oligocene age Suwannee Limestone in the vicinity of
Live Oak for use as coarse and fine aggregate, and base material until about 1975.
Miners in this region had problems with the rock being soft, and having numerous
pockets and seams of clay. Overburden of as much as 50 feet covers the limestone
in the area. Table 1 lists ranges and value.j used to determine suitability of limestone
as an aggregate source.
Table 1. Aggregate Ranges/Values-Live Oak Region
(Source: Florida Department of Transportation, unpublished data)
Los Angeles abrasion
percent soft particles
sodium sulfate soundness
bulk specific gravity
apparent specific gravity
-7 -7 -7 -- 7 7
IARIE TERRACE ----:- ---7-~-:
-DERLAND TERRACE (COOKE, 1939)...-
FENOKEE TERRACE (MACNEIL 1950) -
OMICO TERRACE -O 1
In southern Suwannee County near Branford, the Eocene age Ocala Limestone
is mined and used as base material when used in state road contracts. Mining in this
region is to depths approaching 40 feet below water level. An additional 20 feet of dry
rock is mined for a total depth of about 60 feet below land surface. The Ocala
Limestone is not suitable for the manufacture of aggregate due to its softness and
friable nature. Currently, there are four limestone quarrying operations in Suwannee
County (Mineral Resources Map). They include Hatch Enterprises, Incorporated
(section 16, Township 6S, Range 14E); Anderson Mining Corporation (section 19,
Township 6S, Range 15E); Tim-Prep, Incorporated (section 14, Township 6S, Range
14E); and the county road department (section 14, Township 6S, Range 14E) which
operates a quarry for road base material. Hatch Enterprises, Inc., mines a dolomitic
limestone to depths of 30 feet below water level. The occurrence of dolomitic limestone
at this site does not extend eastward to nearby mines. Tim-Prep, Inc., the county road
department pit, and Anderson Mining Corp. all extract limestone belonging to the Ocala
The quarrying of limestone is accomplished with the use of draglines and, when
needed, explosives are used to facilitate the mining by fracturing and loosening
indurated rock. The rock is stockpiled and allowed to dry before it is run through a
portable crusher. It is then put into trucks for shipping. The primary uses for limestone
mined in Suwannee County are roadbase, agricultural soil conditioners, and asphalt
Suwannee County has ample reserves of near-surface limestone. The reserves
are sufficient to supply the region with limestone for years to come.
Peat is a product of partially decomposed organic materials which accumulate
when the depositional rate exceeds decomposition (Davis, 1946; Bond et al., 1986).
In perennially wet areas organisms which normally metabolize plant matter are inhibited,
thereby allowing peat to form.
The United States Department of Agriculture Soil Conservation Service (SCS)
(1965) found a few small areas of peat in Suwannee County (Mineral Resources Map).
The SCS mapped approximately 90 acres of this material in the county. The peat
varies in thickness from 30 to 60 inches and is usually underlain by sand. The organic
material comprising the peat consists of the remains of sweetbay, ash, cypress, pine,
moss, ferns, maidencane, and other water-tolerant plants (SCS, 1965).
Hard Rock Phosphate
Hard rock phosphate, once mined in southeastern Suwannee County, has not
been quarried in Florida since 1966. The Suwannee County deposits represent this
commodity's northernmost occurrence. These hard rock deposits occur as far south
as Pasco County. The width along this trend does not exceed 16 miles (Vernon, 1943).
The demise of hard rock phosphate mining began with the mining of pebble
phosphate. The costs associated with mining pebble phosphate are much lower than
that of hard rock. The probability of hard rock phosphate once again becoming
economically competitive is low.
Quartz sand is common in the near-surface and surface sediments of
Suwannee County. However, its occurrence with clays, along with the presence of
other impurities, diminish its value as an economic commodity. Surficial sediment
samples from southern Suwannee County, which were examined for this study, were
typically unconsolidated quartz sands, pale yellowish-brown to very pale-orange in
color, fine grained, fine to medium range, and angular to subrounded (section 19,
Township 5S, Range 15E). Accessory constituents included traces of heavy minerals
and minor amounts of organic.
Much of Suwannee County has surface and near-surface sediments made up
of clayey sand, and organic muck. Although the potential for large scale mining is
minimal due to the heterogeneous nature of these sediments, they are valuable locally
as fill material.
Applin, P. L, 1951, Preliminary report on buried pre-Mesozoic rocks in Florida and
adjacent states: U.S. Geological Survey Circular 91, 28 p.
Bond, P.A., Campbell, K.M., and Scott, T.M., 1986, An overview of peat in Florida and
related issues, report to the Florida Legislature: Florida Geological Survey
Special Publication 27, 151 p.
Cooke, C. W., 1939, Scenery in Florida as interpreted by a geologist: Florida Geological
Survey Bulletin 17, 120 p.
Davis, J.H., 1946, The peat deposits of Florida, their occurrence, development and
uses: Florida Geological Survey Bulletin 30, 250 p.
Healy, H. G., 1975, Terraces and shorelines of Florida: Florida Bureau of Geology Map
Series 71, scale 1:2,000,000.
Knapp, M. S., 1978, Environmental geology series-Gainesville sheet: Florida Bureau of
Geology Map Series 79, scale 1:250,000.
1978, Environmental geology series-Valdosta Sheet: Florida Bureau of
Geology Map Series 88, scale 1:250,000.
Lloyd, J. M., 1985, Annotated bibliography of Florida basement geology and related
tectonic studies: Florida Geological Survey Information Circular 98, 72 p.
MacNeil, F. S., 1950, Pleistocene shorelines in Florida and Georgia: U. S. Geological
Survey Professional Paper 221-F, p. 95-107.
Puri, H. S., and Vernon, R. 0., 1964, Summary of the geology of Florida and a
guidebook to the classic exposures: Florida Geological Survey Special
Publication 5 (revised), 312 p.
United States Department of Agriculture Soil Conservation Service, 1965, Soil survey
report for Suwannee County, Florida: U.S.Department of Agriculture Soil
Conservation Service in cooperation with the University of Florida, Institute of
Food and Agricultural Services, 101 p.
Vernon R. 0., 1943, Florida mineral industry, with summaries of production for 1940 and
1941: Florida Geological Survey Bulletin 24, 207 p.
White, W. A., 1970, The geomorphology of the Florida peninsula: Florida Bureau of
Geology Bulletin 51, 164 p.
Two well systems are used in this report. One uses the rectangular
system of section, township and range for identification. The well
number consists of six parts: W for well, county abbreviations, the
Township, Range, and Section, and the quarter/quarter location
within the section. The other system uses the Florida Geological
Survey sample repository accession number.
0 4 MILES
0 6 KILOMETERS
SCALE FOR -15958
FIGURES 1,2, AND 3a
Figure 1. Geomorphology
(modified from White, 1970)
FIGURE 2. TERRACES AND SHORELINES
(modified from Healy, 1975)
FIGURE 3a. GEOLOGIC CROSS SECTION LOCATIONS
WSu-l S-1 2E--32bb W-145
OCALA I UMESTONE
FIGURE 3b. GEOLOGIC CROSS SECTION A-A'
20 ANDTD 85AY
TD 85 OCALA
0 2 4 MILES
0 3 6 KILOMETERS
SCALE FOR FIGURES 3b AND 3c
- TD 157
FIGURE 3c. GEOLOGIC CROSS SECTION B-B'
VERTICAL EXAGGERATION FOR FIGURES 3b AND 3c IS APPROXIMATELY 175 TIMES HORIZONTAL
r CODY SCAR
-0 MSL ----- --
|0||sobekcm_page_globals.constructor||Application State validated or built|
|0||sobekcm_page_globals.constructor||Navigation Object created from URI query string|
|0||sobekcm_page_globals.display_item||Retrieving item or group information|
|0||sobekcm_page_globals.get_entire_collection_hierarchy||Retrieving hierarchy information|
|0||cached_data_manager.retrieve_item_aggregation||Found item aggregation on local cache|
|0||item_aggregation_builder.get_item_aggregation||Found 'all' item aggregation in cache|
|0||html_echo_mainwriter.add_style_references||Adding style references to HTML|
|0||html_echo_mainwriter.add_text_to_page||Reading the text from the file and echoing back to the output stream|
|21||html_echo_mainwriter.add_text_to_page||Finished reading and writing the file|