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Tensleep Sandstone information


Tensleep Formation
Stratigraphic range: Late Pennsylvanian-very Early Permian
~308–298 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
TypeGeological formation
UnderliesPhosphoria & Chugwater Formations
OverliesSacajewea & Amsden Formations
Thicknessup to 535 feet (160 m)
Lithology
PrimarySandstone
OtherLimestone
Location
Coordinates42°36′N 108°12′W / 42.6°N 108.2°W / 42.6; -108.2
Approximate paleocoordinates4°18′N 35°12′W / 4.3°N 35.2°W / 4.3; -35.2
RegionTensleep Sandstone Wyoming
CountryTensleep Sandstone USA
Type section
Named forTen Sleep, Wyoming
Named byN.H. Darton[1]
Year defined1904
Tensleep Sandstone is located in the United States
Tensleep Sandstone
Tensleep Sandstone (the United States)
Tensleep Sandstone is located in Wyoming
Tensleep Sandstone
Tensleep Sandstone (Wyoming)

The Tensleep Sandstone is a geological formation of Pennsylvanian to very early Permian age in Wyoming.[2]

The formation is composed of fine- to medium-grained sandstone, light gray and yellowish gray; generally slightly to moderately calcareous; some dolomite and sandy dolomite beds; mostly thick to massive sets of low-angle, wedge-planar crossbeds of dunes. Forms cliffs 61-91m (200-300 feet) thick.[3]

  1. ^ Darton, N.H., 1904, Comparison of the stratigraphy of the Black Hills, Bighorn Mountains, and Rocky Mountain Front Range: Geological Society of America Bulletin, v. 15, p. 379-448
  2. ^ U.S. Geological Survey. "Geologic Unit: Tensleep". Retrieved 2014-12-23.
  3. ^ Maughan, E.K. 1972. Geologic map of the Wedding of the Waters Quadrangle, Hot Springs County, Wyoming. US Geological Survey Map GQ-1042

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