Pl. 10, p. 953. Eskota dolomite gypsum. Massive gypsum beds, 10 to 20 feet thick, underlain by thin dolomite. Has not been followed farthern than central Fisher County, central northern Texas. Lies 120 feet above Childress dolomite and gypsum, and is older than Croton gypsum. Age is Permian.
Probably named from Eskota, Fisher Co., central northern TX.
Source: US geologic names lexicon (USGS Bull. 896, p. 699).
Pg. 180. Eskota gypsum is a member in Whitehorse-Cloud Chief interval. Age is Permian.
Source: US geologic names lexicon (USGS Bull. 896, p. 699).
Area of report is central Texas; in this area the Whitehorse Sandstone and Cloud Chief Gypsum are mapped undivided. Separately mapped units of Whitehorse and Cloud Chief include (ascending): Childress Dolomite, Eskota Gypsum, and Claytonville Dolomite. Eskota Gypsum is present in various localities in Fisher County, Texas. Whitehorse, Cloud Chief, and Blaine (undivided) overlie Permian San Angelo Formation and underlie Permian Quartermaster Formation. Assigned to the Permian. Geologic map.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Eskota Gypsum [unranked] in middle part of Cloud Chief Gypsum and Whitehorse Sandstone, undivided (Permian). Separately mapped in parts of Cottle, Kent, King, and Stonewall Counties, Texas. Not described. [See also entry under Cloud Chief or Whitehorse.]
Source: Modified from GNU records (USGS DDS-6; Denver GNULEX).
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