Casselman Formation

Casselman Formation
Stratigraphic range: Pennsylvanian

Outcrop of Casselman Formation at Mile Marker 84.2, Pennsylvania Turnpike
Type sedimentary
Unit of Conemaugh Group
Underlies Monongahela Group
Overlies Glenshaw Formation
Lithology
Primary shale, siltstone, sandstone, red beds, coal
Other limestone
Location
Region Appalachian Plateau
Country United States
Extent Pennsylvania, Maryland, West Virginia
Type section
Named for Casselman River
Named by N. K. Flint, 1965[1]

The Casselman Formation mapped sedimentary bedrock unit in Pennsylvania, Maryland, and West Virginia, of Pennsylvanian age. It is the uppermost of two formations in the Conemaugh Group, the lower being the Glenshaw Formation. The boundary between these two units is the top of the marine Ames Limestone.[2] The Conemaugh Group overlies the Upper Freeport coal bed of the Allegheny Formation and underlies the Pittsburgh coal seam of the Monongahela Group.

The Conemaugh Group consists of cyclic sequences of shale, siltstone, sandstone, red beds, thin impure limestone, and thin nonpersistent coal. Red beds are associated with landslides.[3]

The thickness of the Conemaugh Group averages about 400 feet in Ohio, and it ranges from 450 feet on the Ohio River in West Virginia to 520 feet in Washington County, Pennsylvania, and then to 890 feet in Somerset County, Pennsylvania.[4]

Fedexia remains are among the fossils that have been recovered from the formation.

Footnotes

  1. ↑ Flint, N.K., 1965, Geology and mineral resources of southern Somerset County, Pennsylvania: Pennsylvania Geological Survey County Report, 4th series, no. 56A, 267 p.
  2. ↑ Assessment of Appalachian Basin Oil and Gas Resources: Carboniferous Coal-bed Gas Total Petroleum System http://pubs.usgs.gov/of/2004/1272/2004-1272.pdf
  3. ↑ Casselman Formation http://tin.er.usgs.gov/geology/state/sgmc-unit.php?unit=PAPAcc;6
  4. ↑ Assessment of Appalachian Basin Oil and Gas Resources: Carboniferous Coal-bed Gas Total Petroleum System http://pubs.usgs.gov/of/2004/1272/2004-1272.pdf Citing Arkle and others, 1979; Collins; 1979; Edmunds and others, 1999


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