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National Geologic Map Database
Geologic Unit: Pariott
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Map showing publication footprint
  • Usage in publication:
    • Pariott member*
  • Modifications:
    • Original reference
  • Dominant lithology:
    • Sandstone
    • Mudstone
    • Siltstone
    • Shale
  • AAPG geologic province:
    • Paradox basin
Publication:

Shoemaker, E.M., and Newman, W.L., 1959, Moenkopi formation (Triassic? and Triassic) in Salt anticline region, Colorado and Utah: American Association of Petroleum Geologists Bulletin, v. 43, no. 8, p. 1835-1851. [Available online, with subscription, from AAPG archives: http://www.aapg.org/datasystems or http://search.datapages.com]


Summary:

Pg. 1838-1839, 1842, 1847-1848. Pariott member of Moenkopi formation. Consists of red-brown to purplish-brown sandstone and chocolate-brown, orange, and red mudstone, siltstone, and shale. Thickness at type section 134 feet; 252 feet in Sinbad Valley, southwestern Colorado; thickens abruptly toward the west and is several hundred feet thick where it dips beneath the surface beyond northwest end of Castle Valley, southwestern Utah, where it is overlain by a lens of gray silty conglomeratic sandstone assigned by Baker (1933, USGS Bull. 841) to Shinarump conglomerate and by Dane (1935, USGS Bull. 863) to Chinle formation. Overlies Sewemup member (new); unconformably underlies Chinle formation and in some areas truncated by it. [Age is Middle(?) Triassic.]
Type section: south side Pariott Mesa, in sec. 5, T. 25 N., R. 23 E., Grand Co., southwestern UT.

Source: US geologic names lexicon (USGS Bull. 1200, p. 2924).


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

Asterisk (*) indicates usage by the U.S. Geological Survey. Other usages by state geological surveys.

"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 does not conform with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005). This may be explained within brackets ([ ]).