Weverton Formation | |
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Stratigraphic range: Cambrian | |
Type | Formation |
Unit of | Chilhowee Group[1] |
Sub-units | Buzzard Knob Member, Maryland Heights Member, and Owens Creek Member[2] |
Underlies | Harpers Formation |
Overlies | Catoctin Formation and London Conglomerate |
Lithology | |
Primary | sandstone, quartzite, |
Other | shale, siltstone |
Location | |
Region | Appalachia, Mid-Atlantic United States, and Southeastern United States |
Country | United States |
Extent | Maryland, Pennsylvania, Virginia, and West Virginia[3] |
Type section | |
Named for | Weverton, Maryland |
The Weverton Formation is a quartzite geologic formation in Maryland, Virginia, West Virginia, and Pennsylvania. It is considered the basal member of the Chilhowee Group.[1] The Weverton Formation dates back to the Cambrian period.