Penters Chert

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Penters Chert
Stratigraphic range: Devonian
Type Formation
Unit ofnone
Sub-unitsnone
Underlies Clifty Limestone
Overlies Lafferty Limestone
Thicknessup to 90 feet [1]
Lithology
Primary Chert
Location
Region Arkansas
Country United States
Type section
Named forPenters Bluff railroad station, Izard County, Arkansas
Named byHugh 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

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References

  1. 1 2 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.
  2. 1 2 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.