Garber Sandstone
Garber Sandstone Stratigraphic range: Permian | |
---|---|
Type | Formation |
Underlies | Hennessey Formation |
Overlies | Chase Group |
Thickness | 100 to 400 ft[1] |
Lithology | |
Primary | Sandstone |
Other | conglomerate, shale, siltstone, chert[1] |
Location | |
Region | Oklahoma |
Country | United States |
The Garber Sandstone is a geologic formation from the Permian Period in Oklahoma. It serves as an important aquifer, the Garber-Wellington Aquifer, in Logan, Oklahoma, and Cleveland counties of central Oklahoma.[2]
The upper portion of the Garber is associated with extensive baryte mineralization associated with desert rose occurrences in the outcrop area.[3]
See also
References
- 1 2 Garber Sandstone, USGS: Mineral Resources > Online Spatial Data
- ↑ The Garber-Wellington Aquifer, Association of Central Oklahoma Governments
- ↑ Review of the General Geology and Solid-Phase Geochemical Studies in the Vicinity of the Central Oklahoma Aquifer, US Geological Survey Circular 1019, 1986, p. 6
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