Named for Tomahawk Creek, south of Orange, Orange Co., central VA. Occurs in a small fault block immediately south of Orange. Was informally used by Pavlides (1990; USGS Open-File Report 90-548). Consists of green graywacke and phyllite. Thickness ranges from 0 to 300 m. Upper and lower contacts not exposed; may rest unconformably on Late Proterozoic Catoctin Formation and may be unconformably overlain by Cambrian(?) Nasons Formation (new). Only know correlative along strike to the southwest is, in part, BRA unit of Rossman (1991). Age is therefore assigned as Late Proterozoic(?) or Cambrian(?). Report includes geologic map and correlation chart.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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