White Bluff Formation
The White Bluff Formation is a marl, sand, and clay geologic formation in Arkansas that is part of the Jackson Group. It preserves fossils dating back to the Paleogene period, specifically the Eocene.
White Bluff Formation Stratigraphic range: Paleogene | |
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Type | Formation |
Unit of | Jackson Group |
Sub-units | Pastoria Sand Member, Caney Point Marl Member, Rison Clay Member |
Lithology | |
Primary | marl, sand, clay |
Location | |
Region | |
Country | |
Type section | |
Named for | White Bluff, along the Arkansas River |
Description
The White Bluff Formation is composed of three members: the Pastoria Sand Member, the Caney Point Marl Member, and the Rison Clay Member.[1] The Pastoria Sand is a clayey sand containing glauconite and mollusca fossils. The Caney Point Marl is a chalky clay with glauconite and various invertebrate fossils. The Rison Clay is a clay with interbedded silts containing foraminifera fossils and scattered mollusca molds.[1] The entire formation was deposited as a marine sequence.[1][2]
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References
- Wilbert, Jr., Louis J. (1953). "The Jacksonian Stage in southeastern Arkansas" (PDF). Arkansas Division of Geology Bulletin. 19: 37–56. Retrieved 29 June 2018.
- McFarland, John D. (rev. 2004). "Stratigraphic summary of Arkansas" (PDF). Arkansas Geological Commission Information Circular. 36. Retrieved 29 June 2018. Check date values in:
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- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 8 July 2014.
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