Polk Creek Shale
The Polk Creek Shale is a Late Ordovician geologic formation in the Ouachita Mountains of Arkansas and Oklahoma. First described in 1892,[3] this unit was not named until 1909 by Albert Homer Purdue in his study of the Ouachita Mountains of Arkansas.[2] Purdue assigned Polk Creek in Montgomery County, Arkansas as the type locality, but did not designate a stratotype. As of 2017, a reference section for this unit has yet to be designated.
Polk Creek Shale Stratigraphic range: Ordovician | |
---|---|
Type | Formation |
Unit of | none |
Sub-units | none |
Underlies | Blaylock Sandstone |
Overlies | Bigfork Chert |
Thickness | 50 to 225 feet[1] |
Lithology | |
Primary | Shale |
Location | |
Region | Arkansas, Oklahoma |
Country | United States |
Type section | |
Named for | Polk Creek, Montgomery County, Arkansas |
Named by | Albert Homer Purdue[2] |
Paleofauna
Graptolites
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References
- McFarland, John David (2004) [1998]. "Stratigraphic summary of Arkansas" (PDF). Arkansas Geological Commission Information Circular. 36: 19. Archived from the original (PDF) on 2016-12-21. Retrieved 2018-01-09.
- Purdue, A.H. (1909). Slates of Arkansas. Geological Survey of Arkansas. pp. 30, 35.
- Griswold, L.S. (1892). "Whetstones and the novaculites". Annual Report of the Geological Survey of Arkansas for 1890. 3.
- Miser, Hugh D.; Purdue, A.H. (1929). "Geology of the De Queen and Caddo Gap quadrangles, Arkansas". U.S. Geological Survey Bulletin. 808: 40–42.
- Decker, Charles E. (1935). "Graptolites of the Sylvan Shale of Oklahoma and Polk Creek Shale of Arkansas". Journal of Paleontology. 9 (8).
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