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FLRD GEOLOSk ( IC SUfRiW
[year of publication as printed] Florida Geological Survey [source text]
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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 17
Geology of Bradford County, Florida
Frank R. Rupert
Florida Geological Survey
3 1262 04543 6275
L RAr Y
GEOLOGY OF BRADFORD COUNTY, FLORIDA
Florida Geological Survey
Bradford County lies in the Northern Highlands physiographic province
of White (1970). This province spans north Florida from the eastern edge
of Bradford County westward into Alabama. Characterized by a series of
topographically high and gently rolling clayey sand hills, this province is
thought to be a stream-dissected remnant of a once more extensive highland
plain covering much of the Gulf Coastal Plain (White, 1970).
Skirting the eastern edge of Bradford County is a topographic feature
named the Trail Ridge (see Figure 1). The Trail Ridge is an elongate,
north-south trending series of quartz sand hills rising abruptly above the
swampy plain of eastern Bradford County and reaching nearly 220 feet above
mean sea level (MSL). Its crest roughly parallels the Bradford-Clay county
line, and the ridge on average extends less than one mile into Bradford
County (Clark et al., 1964). The bulk of the Trail Ridge lies in neighbor-
ing Clay County, where it reaches 10 miles in width.
Elsewhere in Bradford County, land surface elevations vary from
approximately 60 feet MSL in the swampy Santa Fe River Valley in the
westernmost tip of the county, to 175 feet MSL in southeastern Bradford
County east of the town of Hampton. Over most of the county, the terrain
is generally flat, with large swampy areas and shallow lakes. Creeks and
streams are numerous but sluggish, and flow in poorly-defined channels.
The predominant surficial sediments are quartz sands and clayey sands.
Along the Santa Fe River at the southwestern edge of the county and along
the New River bordering the western edge, the tributary streams are more
deeply incised in the surrounding terrain. Here, tributary streams flowing
into the larger river valleys have cut ravines into the resistant clayey
sands. Steep-sloped bluffs also border the wide valley floors of both the
Santa Fe and New rivers in western Bradford County.
The Santa Fe River is the largest stream in the Bradford County area
and forms the Bradford-Alachua county boundary. The river begins in Santa
Fe Lake, a large shallow body in southeastern Bradford County and
northeastern Alachua County. Flow is westward, where it receives flow from
Hampton Lake, the Sampson River, draining Lake Sampson, and from the New
River which comprises the Bradford-Union county line. The New River forms
at the confluence of numerous small creeks in northern Bradford County, and
drains the highland areas in the northern and western portions of the
Bradford County is underlain by hundreds of feet of marine sands,
clays, limestones and dolomites (Clark et al., 1964). The oldest rock
penetrated by water wells is limestone of the Eocene age (37 to 54 million
years before present, B.P.) Avon Park Formation. Undifferentiated sur-
ficial sands and clays of Pliocene to Holocene Age (5 million years old and
younger) are the youngest sediments present. The Avon Park Formation and
the younger overlying limestone units are important freshwater aquifers,
and this discussion of the geology of Union County will be confined to
these Eocene age and younger sediments. Figure 1 shows the stratigraphic
cross section locations, and Figures 2 and 3 illustrate the underlying
stratigraphy of Bradford County.
AVON PARK FORMATION
The Avon Park Formation (Miller, 1986), as it occurs under Bradford
0 1 2 3 4 5
I ,, I I
0 2 4 6 8
-- CROSS SECTION LOCATION
*. SANTA FE
BRADFORD COUNTY GEOLOGICAL CROSS SECTION LOCATIONS
n > o 0
) 0. m
I I U
VERTICAL EXAGGERATION IS
210 WMES HORIZONTAL SCALE
AVON PARK FORMATION
0 1 2 3 4 5
0 2 4 6 8
T.D. 607 FEET
.ELL NUMBERS SHOWN ARE FLORIOA GEOLOGICAL SURVEY WELL ACCESSION NUMBERS
FIGURE 2: GEOLOGICAL CROSS SECTION A A'
L -50 T.D.-723 FEET
VERTICAL EXAGGERATION IS 210 TIMES HORIZONTAL SCALE
0 1 2 3 4 5
I p I I
0' 2 4 6 8
WELL NUMBERS ARE FLORIDA GEOLOGICAL SURVEY WELL ACCESSION NUMBERS
FIGURE 3: GEOLOGICAL CROSS SECTION B B'
County, is typically a dense, tan to dark brown, porous dolomite, frequently
interbedded with tan, gray, or cream-colored limestones and dolomitic lime-
stones of varying hardness (Clark et al., 1964). Foraminifera are the
dominant fossils present, although dolomitization has destroyed or altered
many of the contained fossils. The Avon Park Formation is a component of
the Floridan aquifer system, and the top of this unit underlies Bradford
County at depths ranging from 400 to 700 feet below land surface (Clark et
al., 1964; Florida Geological Survey in-house well data).
Marine limestones of the Ocala Group (Purl, 1957) unconformably
overlie the Avon Park Formation under all of Bradford County (Clark et al.,
1964). The Ocala Group is comprised of three formations; in ascending
order, these are the Inglis Formation, the Williston Formation, and the
Crystal 1iver Formation. These formations are differentiated on the basis
of lithology and fossil content. Typically, the lithology of the Ocala
Group grades upward from alternating hard and soft, white to tan, fossili-
ferous limestone and dolomitic limestone of the Inglis and lower Williston
Formations into white to pale orange, abundantly fossiliferous, chalky
limestones of the upper Williston and Crystal Formations. Foraminifera,
mollusks, bryozoans, and echinoids are the most abundant fossil types
occurring in the Ocala Group sediments. Thickness of the Ocala Group sedi-
ments under Bradford County average about 250 feet. The permeable and
cavernous nature of the Ocala Group limestones make them important fresh-
water-bearing units of the Floridan aquifer system. Many drinking water
wells in Bradford County withdraw water from the Crystal River Formation.
The Oligocene age (24 to 37 million years 1. P.) Suwannee Limestone
(Cooke and Mansfield, 1936) occurs as discontinuous erosional remnants over-
lying the Ocala Group sediments under the extreme western tip of Bradford
County from the town of Brooker westward (Clark et al., 1964; Florida
Bureau of Geology in-house data). In general, the Suwannee Limestone con-
sists of tan, white, or cream-colored marine limestone, frequently dolomi-
tic and coquinoid in portions and varying considerably in hardness. In
some wells, the Suwannee Limestone is lithologically similar to the Ocala
Group limestones, and is identified primarily on the last occurrence of the
foraminifera Dictyoconus. The thickness of the Suwannee Limestone ranges
between 20 and 40 feet, and the beds may be discontinuous in the subsurface;
this unit is not known in wells east of Brooker (Clark et al., 1964). In
north Florida, the Suwannee Limestone is a freshwater-bearing unit of the
Floridan aquifer system.
Phosphatic quartz sands, clays, limestones and dolomites of the Mio-
cene age (5 to 24 million years B. P.) Hawthorn Group (Scott, in prepara-
tion). unconformably overlie the Suwannee Limestone remnants or Ocala Group
in extreme western Bradford County; east of Brooker, the Hawthorn Group
sediments lie directly upon the Ocala Group limestones. The Hawthorn Grouo
is predominantly a series of marine deposits, consisting of variable and
interbedded lithologies, and characterized by phosphatic and quartz sands,
granules and pebbles. Three formations of the Hawthorn Group are distin-
guishable in Iradford County; in ascending order these are: the Penney
Farms Formation, interbedded phosphatic quartz sand, clay and carbonate;
the Marks Head Formation, thinly and complexly interbedded phosphatic
clays, sand, and carbonate; and the Coosawhatchie Formation, a green to
tan, phosphatic quartz sand with varying amounts of clay and dolomite. The
Hawthorn Group sediments have northeastward dip and range in thickness from
about 100 feet in western Bradford County to at least 300 feet in the
northeastern corner of the county near the state prison. The thick, rela-
tively impermeable clays within the Hawthorn Group are the primary con-
fining beds for the underlying Floridan aquifer system. Pliocene to
Holocene age undifferentiated sands form a veneer over the Hawthorn Group
sediments in most of Bradford County, although the larger river valleys in
the southern and western parts of the county may cut down into the Hawthorn
PLIOCENE TO HOLOCENE UNDIFFERENTIATED
Undifferentiated quartz sands and clays comprise the surficial sedi-
ments over nost of Bradford County. These unfossiliferous deposits are
virtually impossible to age-date, and include the unnamed reddish coarse
clastics, the relict Pleistocene (2.8 million to 0.1 million years 3. P.)
marine terrace sands, and Holocene age (0.1 million years to present)
aeolian, lacustrine and alluvial deposits.
Groundwater is water that fills the pore spaces in subsurface rocks
and sediments. This water is derived principally from precipitalon within
Union and nearby counties. The bulk of Bradford county's consumptive water
is withdrawn from ground-water aquifers. Three main aquifer systems are
present under Bradford County. In order of increasing depth; these are the
surficial aquifer system, the intermediate aquifer system, and the Floridan
aquifer system (Southeastern Geological Society Ad Hoc Committee on Florida
Hydrostratigraphic Unit Definition, 1986).
SURFICIAL AQUIFER SYSTEM
The surficial aquifer system is the uppermost freshwater aquifer in
Bradford County. Sediments comprising this aquifer are primarily the sands
and thin limestone layers in the uppermost part of the Hawthorn Group as
well as the overlying Pleistocene marine terrace sands. On average, the
surficial aquifer system is about 40-feet thick over most of Bradford
County (Clark et al., 1964). The surficial aquifer system is unconfined
and its upper surface is the water table. In general, the water table ele-
vation fluctuates with precipitation rate and conforms to the topography of
the land surface. Within Bradford County, the water table is normally 10
feet or less below land surface. Recharge to the surficial aquifer system
is largely through rainfall percolating downward through the surficial
sediments, and to a lesser extent by upward leakage from the deeper
aquifers. Water naturally discharges from the aquifer by evaporation,
transpiration, springflow,.and by downward seepage into the lower anuifers.
The surficial aquifer system yields water of suitable quality for consump-
tive use and is normally tapped by shallow dug or sand point wells. Due to
the relatively thin units comprising this aquifer, however, only limited
amounts of water are available before local water table lowering occurs.
INTERMEDIATE AQUIFER SYSTEM
The intermediate aquifer system is comprised of deeper water-bearing
sand and limestone layers within the Hawthorn Group. Low permeability
clays above the sand and limestone layers generally confine the intermediate
aquifer system under artesian conditions and separate It from the overlyino
surficial aquifer system. Water yield from this aquifer varies locally
with the quantity of sand and the porosity and permeability of the
limestone; in some areas, the Hawthorn Group limestones are very dense,
yielding little water. Recharge to the intermediate aquifer system con-
sists chiefly of downward seepage from the surficial aquifer system and
upward seepage from the Floridan aquifer system in areas where the poten-
tiometric surface of the Floridan aquifer system is higher than that of the
intermediate system. Numerous rural and domestic wells draw water from the
intermediate aquifer system, and as with the surficial aquifer system, the
volume of water available depends largely on local thickness of the aquifer
FLORIDAN AQUIFER SYSTEM
The Floridan aquifer system is comprised of several hundred feet of
Eocene to Oligocene age porous marine limestones, including the Avon Park
Formation, the Ocala Group, and the Suwannee Limestone. It is by far the
most productive aquifer in Bradford County. The Floridan aquifer system is
confined by low permeability clays of the overlying Hawthorn Group, and is
under artesian conditions. West of Brooker, discontinuous beds of Suwannee
Limestone comprise the upper unit of the Floridan aquifer system. East of
Brooker, the Crystal River Formation of the Ocala Group is the uppermost
unit. County-wide, depth to the Floridan varies, on average, between 75
and 300 feet (Florida Geological Survey in-house well data). The Floridan
aquifer system is an important freshwater source throughout Florida, and
many deep domestic wells and most municipal and industrial supply wells
draw from this aquifer.
Recharge to the Floridan aquifer in Bradford County occurs primarily
as downward leakage through the confining beds from the shallower aquifers
(Clark et al., 1964). Water leaves the Floridan aquifer system through
natural movement downgradient northwestwardd) and subsequent discharge
through springs, lakes, and along the Santa Fe River.
At present,;no mineral commodities are being mined on a commercial
basis in Bradford County. In general, the potential for commercially
feasible mineral production in this county is low. The following
discussion of the major mineral commodities is intended to provide an over-
view of the mining potential for each mineral.
A number of shallow private pits in Bradford County are worked for
fill sand. These sand deposits are concentrated in the unconsolidated
Pliocene to Holocene age surficial sediments covering most of the County.
The unnamed, variably-colored clayey coarse clastics, believed to be equi-
valent to the Miccosukee and Citronelle formations to the west, character-
istically contain fine to coarse grained quartz sand and gravelly sand.
Similar unnamed clayey sands are utilized as roadbase material in counties
to the south. Commercial production of these sands would require extensive
washing to remove the clay matrix; the economics of this procedure would
probably preclude commercial mining in Bradford County. White quartz sands
of the Trail Ridge fringe the eastern edge of Bradford County. These sands
are commercially mined in adjacent Clay County, and may offer industrial
Phosphatic sediments of the Hawthorn Group underlie most of Bradford
County. The phosphate occurs as tan to black sand, granule, and pebble
sized phosphorite (P205). Scott (1983) analyzed the P205 content of the
Hawthorn Group sediments in four Bradford County cores. The composite P205
percentages were found to range from a low of 0.1 percent to a maximum of
13.5 percent, with a county-wide average of only 3.5 percent (Scott, 1983).
Since the minimum economic concentration of P205 is approximately 28 per-
cent (Cathcart and Patterson, 1983), the phosphate mining potential is low
In 3radford County.
Economic deposits of heavy minerals, primarily ilmenite, rutile, leuco-
xene, staurolite, zircon, and monazite, are presently mined on the Trail
Ridge in nearby Clay County. Borehole sample data presented in Spencer
(1948) indicate that composite percentages of heavy minerals in the Trail
Ridge sands drop from approximately 4.0 percent in the currently-mined area
of Clay County, to between 1.0 and 1.5 percent on the western flank of the
ridge in Bradford County. These relatively low concentrations in Bradford
County preclude economical mining with existing technology.
LIMESTONE AND DOLOMITE
Bradford County is underlain by extensive deposits of Eocene to
Miocene age marine limestones. However, the excessive thickness of the
overlying Hawthorn Group siliciclastics and the Pliocene to Holocene undif-
ferentiated surficial sediments puts most limestone at too great a depth
for commercial mining.
Peat is an organic mineral commodity formed from rapid accumulation of
decaying vegetation. This commodity is currently being mined by two com-
panies near Keystone Heights in nearby Clay County (Campbell, 1986). To
date, no commercial mining of peat occurs in Bradford County. Although
unproven, the areas of highest peat potential are the shallow, swampy
regions in central Bradford County and in the Santa Fe Swamp in the south-
eastern corner of the county (Davis, 1946; Bond et al., 1986).
Clay and clayey sand deposits occur in the upper Hawthorn Group sedi-
ments as well as the undifferentiated Pliocene to Holocene surficial sedi-
ments over most of Bradford County. Except for private borrow pits, there
has been no commercial exploitation of these deposits. The suitability of
these clays for industrial and commercial use is, as yet, untested. To the
east in Putnam County, and in counties to the south, the red, clayey sands
and sandy clays formerly referred to as unnamed coarse clastics are used
extensively as road material.
Bond, P., Campbell, K. M., and Scott, T. M., 1986, An overview of peat in
Florida: Florida Geological Survey, Special Publication no. 27, 151 p.
Campbell, K. M., 1986, The industrial minerals of Florida: Florida Geolo-
gical Survey, Information Circular 102, 94 p.
Cathcart, J. B., and Patterson, S. H., 1983, Mineral resource potential of
the Farles Prairie and Buck Lake roadless areas, Marion County, Florida:
U. S. Geological Survey, Map Series MF-15918.
Clark, W. E., Musgrove, R. H., Menke, C. G. and Cagle, .1. W., 1964, Water
resources of Alachua, Bradford, Clay and Union Counties, Florida:
Florida Geological Survey, Report of Investigations no. 35, 170 p.
Cooke, C. W. and Mansfield, W. C., 1936, Suwannee Limestone of Florida
(abstract): Geological Society of America Proceedings, 1935, p.
Davis, J. H., 1946, The peat deposits of Florida: Florida Geological
Survey, Bulletin no. 30, 247 p.
Miller, J. A., 1986, Hydrogeologic framework of the Floridan aquifer system
in Florida and in parts of Georgia, Alabama, and South Carolina:
U. S. Geological Survey, Professional Paper 1403-8, p. 25-27.
Purl, H. S., 1957, Stratigraphy and zonation of the Ocala Group: Florida
Geological Survey Bulletin 38, 248 p.
Scott, T. M., 1983, The Hawthorn Formation of northeastern Florida, Part II,
Characterization and beneficiation of the northeastern Florida phos-
phate-bearing Hawthorn Formation: Florida Bureau of Geology, Report
of Investigation no. 94, p. 41-90.
(in preparation), The lithostratigraphy of the Hawthorn
Group (Miocene) of Florida: Florida Geological Survey, Bulletin no.
Southeastern Geological Society Ad Hoc Committee on Florida hydrostrati-
graphic unit definition, 1986, Hydrogeological units of Florida:
Florida Bureau of Geology, Special Publication no. 28, 9 p.
Spencer, R. V., 1948, Titanium minerals in Trail Ridge, Florida: U. S.
Bureau of Mines, Report of Investigations 4208, 21 p.
White, W. A., 1970, Geomorphology of the Florida peninsula: Florida
Geological Survey, Bulletin no. 51, 164 p.
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