Catoctin Formation

Catoctin Formation
Stratigraphic range: Ediacaran
TypeFormation
UnderliesChilhowee Group
OverliesBasement Rock
Thickness100-400 Feet
Location
RegionVirginia, Maryland, and Pennsylvania
CountryUnited States
Type section
Named forIts exposure on Catoctin Mountain
Named byArthur Keith

Geological Map of the Catoctin Formation shown in blue and other formations associated with it.

The Catoctin Formation is a geologic formation that expands through Virginia, Maryland, and Pennsylvania.[1] It dates back to the Precambrian and is closely associated with the Harpers Formation, Weverton Formation, and the Loudoun Formation.[1] The Catoctin Formation lies over a granitic basement rock and below the Chilhowee Group[1] making it only exposed on the outer parts of the Blue Ridge.[2] The Catoctin Formation contains metabasalt, metarhyolite,[3] and porphyritic rocks, columnar jointing, low-dipping primary joints, amygdules, sedimentary dikes, and flow breccias.[4] Evidence for past volcanic activity includes columnar basalts and greenstone dikes.

  1. ^ a b c Reed, John C. (1955-07-01). "Catoctin Formation Near Luray, Virginia". GSA Bulletin. 66 (7): 871–896. doi:10.1130/0016-7606(1955)66[871:CFNLV]2.0.CO;2. ISSN 0016-7606 – via GeoScienceWorld.
  2. ^ Bloomer, Robert O.; Bloomer, Richard R. (1947-03-01). "The Catoctin Formation in Central Virginia". The Journal of Geology. 55 (2): 94–106. doi:10.1086/625404. ISSN 0022-1376. S2CID 129699878.
  3. ^ Thurmont, Mailing Address: 6602 Foxville Road; Us, MD 21788 Phone:663-9388 Contact. "Geology - Catoctin Mountain Park (U.S. National Park Service)". www.nps.gov. Retrieved 2021-04-13.{{cite web}}: CS1 maint: numeric names: authors list (link)
  4. ^ "USGS: Geological Survey Bulletin 1265 (Catoctin Formation)". www.nps.gov. Retrieved 2021-04-13.