Langston Formation
Langston Formation Stratigraphic range: Cambrian | |
---|---|
Type | Formation |
Underlies | Ute Formation |
Overlies | Brigham Formation |
Thickness | 30 - 498' |
Location | |
Region | Idaho, Utah |
Country | United States |
Type section | |
Named for | Langston Creek |
Named by | Charles Doolittle Walcott |
The Langston Formation is a geologic formation in Idaho and Utah. It preserves fossils dating back to the Cambrian period. The formation is composed of bluish-gray limestone,[1] weathering to a buff color, often with rounded edges.[2]
Blacksmith Fork is the type locality, and includes more fossils than the Idaho sections.
The Langton Formation includes the fossilerous Spence Shale.
See also
References
- ↑ Walcott, Charles. Nomenclature of Some Cambrian Cordilleran formations. Cambrian Geology and Paleontology, I. Smithsonian Miscellaneous Collections, 53:1–12, pg. 8
- ↑ Mansfield, George Rogers. Geography, Geology, and Mineral Resources of Part of Southeastern Idaho. U.S. Government Printing Office, 1927, pg. 53.
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 8 July 2014.
This article is issued from Wikipedia - version of the 1/12/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.