∕ Interbedded silty claystones and minor conglomerates occur, particularly within the basal portions of the sequence, indicating variable energy conditions during early stages of deposition; and ∕ The Razorback Beds form a distinctive topographic unit, preserved mainly along ridge crests and elevated landforms, where sandstones contrast with surrounding eroded Paleozoic bedrock.
Figure 39. Geological Map (WSP)
Project number: 25B061
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