| Tensleep Formation | |
|---|---|
|
Stratigraphic range:
Late Pennsylvanian-very
Early Permian ~ | |
 | |
| Type | Geological formation |
| Underlies | Phosphoria & Chugwater Formations |
| Overlies | Sacajewea & Amsden Formations |
| Thickness | up to 535 feet (160 m) |
| Lithology | |
| Primary | Sandstone |
| Other | Limestone |
| Location | |
| Coordinates | 42°36′N 108°12′W / 42.6°N 108.2°W |
| Approximate paleocoordinates | 4°18′N 35°12′W / 4.3°N 35.2°W |
| Region | 
Wyoming |
| Country | 
USA |
| Type section | |
| Named for | Ten Sleep, Wyoming |
| Named by | N.H. Darton [1] |
| Year defined | 1904 |
  Tensleep Sandstone (the United States)  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]
Trace fossils
In 1932 Edward Branson and Maurice Mehl reported the discovery of a fossil trackway in the formation. [4] A new ichnospecies, Steganoposaurus belli, was erected for these footprints. [4] The tracks were probably made by a web-footed animal slightly less than three feet long. [4] This creature was originally presumed to be an amphibian, but the toe prints it left behind were pointed like a reptile's rather than round like an amphibians. The actual trackmaker may have been similar to the genus Hylonomus. [5] The ichnogenus Tridentichnus are similar footprints preserved in the Supai Formation of Arizona. [6]
References
- ^ 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
- ^ U.S. Geological Survey. "Geologic Unit: Tensleep". Retrieved 2014-12-23.
- ^ Maughan, E.K. 1972. Geologic map of the Wedding of the Waters Quadrangle, Hot Springs County, Wyoming. US Geological Survey Map GQ-1042
- ^ a b c "Western Traces in the 'Age of Amphibians'," Lockley and Hunt (1995); page 34.
- ^ "Western Traces in the 'Age of Amphibians'," Lockley and Hunt (1995); page 35.
- ^ "Western Traces in the 'Age of Amphibians'," Lockley and Hunt (1995); pages 34-35.
Bibliography
- Lockley, Martin and Hunt, Adrian. Dinosaur Tracks of Western North America. Columbia University Press. 1999.
| Tensleep Formation | |
|---|---|
|
Stratigraphic range:
Late Pennsylvanian-very
Early Permian ~ | |
|
| |
| Type | Geological formation |
| Underlies | Phosphoria & Chugwater Formations |
| Overlies | Sacajewea & Amsden Formations |
| Thickness | up to 535 feet (160 m) |
| Lithology | |
| Primary | Sandstone |
| Other | Limestone |
| Location | |
| Coordinates | 42°36′N 108°12′W / 42.6°N 108.2°W |
| Approximate paleocoordinates | 4°18′N 35°12′W / 4.3°N 35.2°W |
| Region |
Wyoming |
| Country |
USA |
| Type section | |
| Named for | Ten Sleep, Wyoming |
| Named by | N.H. Darton [1] |
| Year defined | 1904 |
Tensleep Sandstone (the United States) 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]
Trace fossils
In 1932 Edward Branson and Maurice Mehl reported the discovery of a fossil trackway in the formation. [4] A new ichnospecies, Steganoposaurus belli, was erected for these footprints. [4] The tracks were probably made by a web-footed animal slightly less than three feet long. [4] This creature was originally presumed to be an amphibian, but the toe prints it left behind were pointed like a reptile's rather than round like an amphibians. The actual trackmaker may have been similar to the genus Hylonomus. [5] The ichnogenus Tridentichnus are similar footprints preserved in the Supai Formation of Arizona. [6]
References
- ^ 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
- ^ U.S. Geological Survey. "Geologic Unit: Tensleep". Retrieved 2014-12-23.
- ^ Maughan, E.K. 1972. Geologic map of the Wedding of the Waters Quadrangle, Hot Springs County, Wyoming. US Geological Survey Map GQ-1042
- ^ a b c "Western Traces in the 'Age of Amphibians'," Lockley and Hunt (1995); page 34.
- ^ "Western Traces in the 'Age of Amphibians'," Lockley and Hunt (1995); page 35.
- ^ "Western Traces in the 'Age of Amphibians'," Lockley and Hunt (1995); pages 34-35.
Bibliography
- Lockley, Martin and Hunt, Adrian. Dinosaur Tracks of Western North America. Columbia University Press. 1999.