| Rome Group | |
|---|---|
| Stratigraphic range: Cambrian | |
| Type | Group |
| Underlies | Conasauga Group |
| Overlies | Tomstown Dolomite |
| Location | |
| Region | West Virginia |
| Country | United States |
The Rome Group is a geologic group in West Virginia. It dates back to the Cambrian period.
| Rome Group | |
|---|---|
| Stratigraphic range: Cambrian | |
| Type | Group |
| Underlies | Conasauga Group |
| Overlies | Tomstown Dolomite |
| Location | |
| Region | West Virginia |
| Country | United States |
The Rome Group is a geologic group in West Virginia. It dates back to the Cambrian period.
These are tables of congressional delegations from West Virginia to the United States House of Representatives and the United States Senate.
Namibian cuisine is the cuisine of Namibia. It is influenced by two primary cultural strands:
The following is an alphabetical list of articles related to the U.S. state of West Virginia.
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. The Conemaugh Group overlies the Upper Freeport coal bed of the Allegheny Formation and underlies the Pittsburgh coal seam of the Monongahela Group.
Brook Glacier is a glacier that flows westward between Mount Strybing, Mount Allen and Krusha Peak on the west side of Owen Ridge in southern Sentinel Range, Ellsworth Mountains in Antarctica, and joins Bender Glacier east of Chaplin Peak. It was named by the Advisory Committee on Antarctic Names (2006) after Edward J. Brook, Professor of Geosciences, Oregon State University; U.S. Antarctic Project investigator of Antarctic paleoclimate in numerous field seasons from 1988; Chair, U.S. National Ice Core Working Group for use of Antarctic ice cores for research purposes, 2004–05.
The Glenshaw Formation is a mapped sedimentary bedrock unit in Pennsylvania, Maryland, West Virginia, and Ohio, of Pennsylvanian age. It is the lower of two formations in the Conemaugh Group, the upper being the Casselman Formation. The boundary between these two units is the top of the marine Ames Limestone. The Conemaugh Group overlies the Upper Freeport coal bed of the Allegheny Formation and underlies the Pittsburgh coal seam of the Monongahela Group.
Herron Airport is a privately owned airport in New Cumberland, West Virginia, United States, part of the Pittsburgh Combined Statistical Area. It was opened in November 1946, founded by William Earle “Earle” Herron.
The Coal and Coke Railway was a railway operated by the Coal and Coke Railway Company in central West Virginia between 1905 and 1916. The line was made up of branches acquired from other companies and new construction. It ran from Elkins, West Virginia, at its northeastern terminus, to Charleston, West Virginia, at its southwestern terminus. Gassaway, West Virginia, was roughly the halfway point in the railway's approximate length of 196 miles.
The Conemaugh Group is a geologic group in West Virginia, Pennsylvania, Ohio, and Maryland. It preserves fossils dating back to the Carboniferous period.
The Greenland Gap Group is a geologic group in West Virginia. It preserves fossils dating back to the Devonian period.
The Hinton Formation is a geologic formation in West Virginia. It preserves fossils dating back to the Carboniferous period. It is mainly made up of limestone, sandstone, and shale.
The Hampshire Formation is a geologic formation in West Virginia, USA. It preserves fossils dating back to the Devonian period.
The Oriskany Sandstone is a Middle Devonian age unit of sedimentary rock found in eastern North America. The type locality of the unit is located at Oriskany Falls in New York. The Oriskany Sandstone extends throughout much of the Appalachian Basin.
The Rochester Shale is a geologic formation exposed in New York and West Virginia. It preserves fossils dating back to the Silurian period.
The Harpers Formation is a geologic formation in Maryland, Pennsylvania, Virginia, and West Virginia, consisting of schist, phyllite, and shale. It dates back to the early Cambrian period. It is considered part of the Chilhowee Group.
The Swift Run Formation is a geologic formation in Virginia and West Virginia. It dates back to the Neoproterozoic.
The St. Paul Group is a geologic group in West Virginia. It dates back to the Ordovician period.
The Oswego Formation is a geologic formation in West Virginia. It dates back to the Ordovician period.
The Conasauga Group is a geologic group in West Virginia. It dates back to the Cambrian period.
The Wells Creek Formation is a geologic formation in West Virginia. It dates back to the Ordovician period.
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