Garber Sandstone
Geologic formation in Oklahoma
From Wikipedia, the free encyclopedia
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]
| Garber Sandstone | |
|---|---|
| Stratigraphic range: Permian | |
| Type | Formation |
| Unit of | Wichita 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 upper portion of the Garber is associated with extensive baryte mineralization associated with desert rose occurrences in the outcrop area.[3]
