Pg. 217. Altuda member of Vidrio formation. Middle member of Vidrio formation. Thin-bedded dolomites, characterized by considerable amounts of sandy and shaly material. Thickness 0 to 400 feet. Is separated from underlying Word formation by several hundred feet of very massive cliff-forming dolomites, making up lower part of Vidrio formation. To west these thin and gradually merge with Altuda member. Overlain by 1,000+/- feet of massive dolomites, which represent upper part of Vidrio formation and interfinger with lower part of overlying Gilliam formation. Age is Permian.
Named from exposures in vicinity of Altuda section house, Glass Mountains, Brewster Co., western TX.
Source: US geologic names lexicon (USGS Bull. 896, p. 41-42).
Pg. 75, 131, 134, 136, quarto. Treated Altuda member as a member of Capitan formation, and gave several detailed sections, in some of which he descirbed it as chiefly limestone with considerable siliceous shale, and in others as almost wholly dolomite, and gave thicknesses of 347, 477, and 734 feet. [See also 1930 (1931) entry under Capitan.]
Source: US geologic names lexicon (USGS Bull. 896, p. 41-42).
Pg. 737. Changed name to Altuda shaly member of Capitan limestone, and also treated the Vidrio, Gilliam, and Tessey as members of Capitan limestone. Age is Permian.
Source: US geologic names lexicon (USGS Bull. 896, p. 41-42).
Pg. 655. Altuda formation. Rank raised to formation. Recognized in western Texas. Age is Permian (Guadalupe).
Source: US geologic names lexicon (USGS Bull. 1200, p. 68).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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