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Geologic units in Chesterfield county, South Carolina

Peedee Formation /Black Creek Group, undivided (Cretaceous) at surface, covers 62 % of this area
Peedee Formation /Black Creek Group, undivided
Lithology: clay or mud; sand; limestone
Cid Formation, Mudstone Member (Ordovician to Late Cambrian) at surface, covers 4 % of this area
Cid Formation, Mudstone Member: thin bedded tuffaceous metasiltstone
Lithology: metasedimentary rock
Cape Fear/Eutaw Formations (Cretaceous) at surface, covers 10 % of this area
Cape Fear/Eutaw Formations Kcfe: Poorly sorted clayey sand and gravel deposited in delta-dominated fluvial- and restricted marine environments. Unit is characterized by an abundance of smoky quartz gravel, feldspar, monazite, and garnet typically concentrated in placer deposits. Generally non-marine from North Carolina to central Georgia but contains shallow-water delta-front deposits in western Georgia.
Lithology: sand; gravel
Middendorf Formation (Cretaceous) at surface, covers < 0.1 % of this area
Middendorf Formation - sand, sandstone, and mudstone, gray to pale gray with an orange cast, mottled; clay balls and iron-cemented concretions common, beds laterally discontinuous, cross-bedding common.
Lithology: sand; sandstone; mudstone; clay or mud
Brandywine Formation (Miocene) at surface, covers 1.0 % of this area
Brandywine Formation: Upland gravel similar to Columbia group mapped in the uplands of southern Maryland southeast of DC. 10-40 ft thick. Extensive sand and gravel resources.
Lithology: gravel; sand
Granite (Carboniferous to Permian) at surface, covers < 0.1 % of this area
Granite
Lithology: granite
Persimmon Fork Formation (Cambrian to Neoproterozoic) at surface, covers 8 % of this area
Persimmon Fork Formation: predominately metatuff
Lithology: metavolcanic rock
Chatham Group, undivided (Triassic) at surface, covers 1.0 % of this area
Chatham Group, undivided: conglomerate, sandstone and mudstone
Lithology: conglomerate; sandstone; mudstone
Penholoway Formation (Pleistocene) at surface, covers 0.9 % of this area
Penholoway Formation: Similar to Cape May, broad lateral extent underlying terraces in the Carolinas; swamps and ridges on terrace surface were originally barrier islands and back bays. Superimposed on these landforms are swarms of Carolina bays.
Lithology: sand; clay or mud
Socastee Formation (Pleistocene) at surface, covers 0.5 % of this area
Socastee Formation: Low coastal formation in Carolinas like Penholoway but younger and lower in altitude.
Lithology: sand; clay or mud
Alluvial Valley Swamp (Quaternary) at surface, covers 5 % of this area
Alluvial Valley Swamp: Unconformable on all underlying units, fluvial sand and gravel at base, grading upwards into fine sands and silts, local peat. May be overrun with recent sediments from forest cutting and agriculture.
Lithology: sand; gravel; silt; peat
Duplin Formation (Pliocene) at surface, covers 2 % of this area
Duplin Formation: Coastal terrace of Carolinas. Pliocene equivalent to Yorktown. Deeply weathered.
Lithology: sand; clay or mud; conglomerate
Metamudstone and Meta-Argillite (Cambrian/Late Proterozoic) at surface, covers < 0.1 % of this area
Metamudstone and Meta-Argillite - bedding plane and axial-planar cleavage common; interbedded with metasandstone, meta-conglomerate, and metavolcanic rock.
Lithology: metasedimentary rock; meta-argillite; meta-conglomerate; metavolcanic rock
Granite- Pageland pluton (Carboniferous to Permian) at surface, covers 0.9 % of this area
Granite- Pageland pluton
Lithology: granite
Richtex Formation (Ordovician to Middle Cambrian) at surface, covers 4 % of this area
Richtex Formation: laminated metamudstone; contains Middle Cambrian or younger sponge spicules
Lithology: metasedimentary rock
Flat Swamp Formation (AKA Flat Swamp Member of Cid Formation) (Ordovician to Neoproterozoic) at surface, covers 0.9 % of this area
Flat Swamp Formation (AKA Flat Swamp Member of Cid Formation): crystal and lithic metatuff of rhyolite to rhyodacite composition
Lithology: felsic metavolcanic rock

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Page Last modified: 10:03 on 08-May-2012