The siliciclastics are
quartz and vary in color from white to light olive gray. They are unconsolidated to poorly indurated (hard), slightly clayey sands with minor phosphate to light gray to bluish gray, poorly consolidated, variably silty clay (Dogtown Member). The siliciclastics are sporadically
fossiliferous and often contain
oyster shells as found in the
Seaboard Air Line Railroad site. The carbonate sediments contain
phosphate and are white to light olive gray. They are generally not hard but variably sandy with clay. This unit is also fossiliferous with both molds and casts and includes limestone (
mudstone and
wackestone). The limestones often grade into
calcareous-cemented sands. The Dogtown Member is time transgressive with older aged material at ~15.9–15.3 Ma. and found in the south while the younger material is in the north. ==Overlay==