Antietam Formation
Antietam Formation Stratigraphic range: Cambrian | |
---|---|
Type | Formation |
Unit of | Chilhowee Group |
Underlies | Tomstown Dolomite |
Overlies | Harpers Formation |
Thickness | 550 ft |
Lithology | |
Primary | Sandstone, quartzite |
Other | Schist |
Location | |
Region | Appalachia, Eastern United States, and Southeastern United States |
Country | United States |
Extent | Maryland, Pennsylvania, Virginia,[1] and West Virginia |
Type section | |
Named for | Antietam Creek |
The Antietam Formation or Antietam Sandstone is a geologic formation in Pennsylvania, Maryland and West Virginia.[2][3][4] It is largely quartz sandstone with some quartzite and quartz schist. It preserves Skolithos trace fossils dating back to the Cambrian Period.[5]
Tight folds in the schist of Antietam Formation
Thin section of schist. Porphyroblastic biotite, a, in a dolomitic matrix. The tourmaline, t, is epigenetic.
References[]
- ^ Paleozoic Sedimentary Successions of the Virginia Valley & Ridge and Plateau
- ^ Antietam Formation in West Virginia, USGS
- ^ Antietam Formation in Pennsylvania, USGS
- ^ Maryland Geological Survey, Volume 10, Johns Hopkins Press, 1918 p. 200
- ^ "Geology of West Virginia's Blue Ridge". Archived from the original on 2016-03-04. Retrieved 2015-03-25.
Categories:
- Cambrian Maryland
- Cambrian geology of Pennsylvania
- Cambrian West Virginia
- Cambrian south paleopolar deposits
- Southern United States geologic formation stubs
- West Virginia geography stubs
- Northeastern United States geologic formation stubs
- Pennsylvania geography stubs
- Maryland geography stubs