Penters Chert
| Penters Chert Stratigraphic range: Devonian | |
|---|---|
| Type | Formation |
| Unit of | none |
| Sub-units | none |
| Underlies | Clifty Limestone |
| Overlies | Lafferty Limestone |
| Thickness | up to 90 feet[1] |
| Lithology | |
| Primary | Chert |
| Location | |
| Region | Arkansas |
| Country | United States |
| Type section | |
| Named for | Penters Bluff railroad station, Izard County, Arkansas |
| Named by | Hugh Dinsmore Miser[2] |
The Penters Chert is a Devonian geologic formation in the Ozark Plateaus of Arkansas.[1] The name was introduced in 1921 by Hugh Dinsmore Miser in his study of Arkansas.[2] Miser designated a type locality near the old Penters Bluff railroad station in Izard County, Arkansas, however, he did not assign a stratotype. As of 2017, a reference section has not been designated for this unit.
See also[]
References[]
- ^ a b McFarland, John David (2004) [1998]. "Stratigraphic summary of Arkansas" (PDF). Arkansas Geological Commission Information Circular. 36: 9. Archived from the original (PDF) on 2016-12-21. Retrieved 2018-01-11.
- ^ a b Miser, Hugh D. (1921). "Preliminary report on the deposits of manganese ore in the Batesville district, Arkansas" (PDF). U.S. Geological Survey Bulletin. 715-G: 98, pls. 6, 7.
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