Tensleep Sandstone

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

Tensleep Formation
Stratigraphic range: Late Pennsylvanian-very Early Permian
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TypeGeological formation
UnderliesPhosphoria & Chugwater Formations
OverliesSacajewea & Amsden Formations
Thicknessup to 535 feet (160 m)
Lithology
PrimarySandstone
OtherLimestone
Location
Coordinates42.6°N 108.2°W / 42.6; -108.2
Approximate paleocoordinates4.3°N 35.2°W / 4.3; -35.2
Region Wyoming
Country USA
Type section
Named forTen Sleep, Wyoming
Named byN.H. Darton
Year defined1904
Tensleep Sandstone (the United States)
Tensleep Sandstone (Wyoming)

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.

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