Wildhorse Branch Formation named in the Carolina Slate belt of central SC. Consists of greenish-gray greenstone, felsic tuffaceous phyllite, and graphitic phyllite. Thickness greater than 3000 m. Underlies Persimmon Fork Formation (new). Age is Precambrian or Cambrian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Wildhorse Branch Formation greater than 2400 m thick in mapped area. Consists of 50 percent felsic tuff, 40 percent mafic tuffs and flows, and 10 percent pelitic sediments, mostly metamorphosed to schist. Underlies Persimmon Fork Formation and overlies unnamed quartz-microcline gneiss. No age given.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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