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Geologic Unit: Garceno
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Map showing publication footprint
  • Usage in publication:
    • Garceno sandstone member
  • Modifications:
    • Original reference
  • Dominant lithology:
    • Sandstone
  • AAPG geologic province:
    • Gulf Coast basin
Publication:

Patterson, J.M., 1942, Stratigraphy of Eocene between Laredo and Rio Grande City, Texas: American Association of Petroleum Geologists Bulletin, v. 26, no. 2, p. 256-274. [Available online, with subscription, from AAPG archives: http://www.aapg.org/datasystems or http://search.datapages.com]


Summary:

Pg. 259 (fig. 2), 261-262. Garceno sandstone member of Cook Mountain formation. Name applied to basal sandstone member of formation. With exception of a 50-foot dark-colored marine shale about 150 feet above the base, member is composed of glauconitic marine sandstone beds that are highly fossiliferous. Thickness approximately 500 feet. Underlies Veleno member (new); overlies Mount Selman formaiton. Age is Eocene (Claiborne).
Named from Garceno ranch house, located on outcrop of the sandstone, 9 mi northwest of Zapata, Mexico. Ranch house is on American side of Rio Grande, western TX.

Source: US geologic names lexicon (USGS Bull. 1200, p. 1465).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).