The late Cenozoic stratigraphy of part of central Florida immediately south of the land-pebble phosphate district was studies in detail to determine the southern limit of the economically important Bone Valley formation and its relations with marine rocks of late Miocene and Pliocene age in south-central Florida. In addition a reconnaissance
type appraisal of the phosphate and uranium resources of this area was
desired. The upper Tertiary and Quaternary rocks were mapped, and the
economic geology was studied in a general manner.
The Hawthorn formation of middle Miocene age, is the oldest rock
Exposed. Undifferentiated phosphatic sand and clay may be composed of
the Bone Valley formation, of late Miocene to Pliocene age; a combination
of Bone Valley formation and residuum of weathered Hawthorn formation;
or Hawthorn residuum alone. The Bone Valley formation and residuum of
Hawthorn formation appear almost identical in cuttings from auger drilling
in this area. It was not feasible nor practical to map these two
units separately. The undifferentiated phosphatic sand and clay interfingers with a marine sand of late Miocene age, The Caloosahatchee marl of Pliocene age, is present in the southeast corner of the area
investigated. It is apparent that the undifferentiated phosphatic sand
and clay was undergoing subaerial erosion and reworking during deposition
or the Caloosahatchee marl. Stratified sand and clayey sand containing
scattered thin lenses of fresh-water limestone and marl of Pleistocene age are either floodplain deposits or subaerial topset beds of a delta
made by the Pleistocene Peace River. Sediments of Recent age are local
stream deposits.
Bars and shoals in the Peace River south of Brownville, De Soto
County, contain appreciable tonnages of low grade "river-pebble" phosphate.
The phosphate and uranium content of the undifferentiated phosphatic
sand and clay in Hardee County is too low to be of economic significance.
