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  • Usage in publication:
    • Stagg Creek Member*
  • Modifications:
    • Named
  • Dominant lithology:
    • Sandstone
    • Conglomerate
    • Siltstone
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
    • Taylorsville basin
Publication:

Weems, R.E., 1980, Geology of the Taylorsville basin, Hanover County, Virginia: Virginia Division of Mineral Resources Publication, no. 27, p. 23-38.


Summary:

The lower member of the Doswell Formation is here named the Stagg Creek Member, for Stagg Creek, a tributary of the South Anna River, Hanover Co., VA. It consists of massive sandstone and conglomerate with minor siltstone. It nonconformably overlies Mississippian Petersburg Granite and conformably underlies the Falling Creek Member of the Doswell. Thickness is 600 ft (180 m) at type section. Age is Late Triassic (middle Carnian) based on palynomorphs.

Source: GNU records (USGS DDS-6; Reston GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).