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Map showing publication footprint
  • Usage in publication:
    • Thompson Canyon sandstone bed*
  • Modifications:
    • Named
  • Dominant lithology:
    • Sandstone
  • AAPG geologic province:
    • Paradox basin
Publication:

Fisher, D.J., 1936, The Book Cliffs coal field in Emery and Grand Counties, Utah: U.S. Geological Survey Bulletin, 852, 104 p.


Summary:

Named as a bed in middle part of Neslen member (new) of Price River formation of the Mesaverde group. Source of name and type locality not stated. Thompson Wash is in Ts21 and 22S, Rs19 and 20E, Grand Co, UT in the Paradox basin. Mapped from Saleratus Canyon to Cottonwood Canyon and east to Garfield Co, CO [extent into CO not discussed]. Consists of 10-15 ft of massive, faintly cross-bedded, straw-colored sandstone. Weathers to rounded surfaces. Overlain and underlain by unnamed parts of Neslen. Is 20 ft thick in a section measured in NW1/4 sec 32, T20S, R21E where it varies from buff-brown to buff-yellow. Thought to occupy same stratigraphic position as Rollins sandstone [member of Mesaverde formation] of CO. Of Late Cretaceous age. Geologic maps.

Source: GNU records (USGS DDS-6; Denver GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Thompson Canyon sandstone member*
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Paradox basin
Publication:

Cobban, W.A., and Reeside, J.B., Jr., 1952, Correlation of the Cretaceous formations of the Western Interior of the United States: Geological Society of America Bulletin, v. 63, no. 10, p. 1011-1044.


Summary:

Recognized in the central Book Cliffs, UT in the Paradox basin. Raised in stratigraphic rank from Thompson Canyon sandstone bed to Thompson Canyon sandstone member of Neslen formation of Mesaverde group. Of late Campanian, Late Cretaceous age. Correlation chart.

Source: GNU records (USGS DDS-6; Denver GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Thompson Canyon Sandstone Bed*
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Paradox basin
Publication:

Franczyk, K.J., 1989, Depositional controls on the late Campanian Sego Sandstone and implications for associated coal-forming environments in the Uinta and Piceance basins, IN Evolution of sedimentary basins; Uinta and Piceance basins: U.S. Geological Survey Bulletin, 1787-F, p. F1-F17.


Summary:

Is a member of Neslen Formation of Late Cretaceous age. Identified only at Sego Canyon, Ts19 and 20S, R20E, Grand Co, UT in the Paradox basin. Is extensively burrowed and bioturbated. Contains low-angle trough cross-stratification and ripple laminations near top. Its geometry, lateral extent, and sedimentary structures indicate brackish-water deposition, probably a bay fill. Cross sections. Correlation chart. Measured sections. Of Late Cretaceous age.

Source: GNU records (USGS DDS-6; Denver GNULEX).


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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 ( ).

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