| Garber Sandstone | |
| Type: | Formation |
| Age: | Permian |
| Prilithology: | Sandstone |
| Otherlithology: | conglomerate, shale, siltstone, chert |
| Region: | Oklahoma |
| Country: | United States |
| Unitof: | Wichita Formation |
| Underlies: | Hennessey Formation |
| Overlies: | Chase Group |
| Thickness: | 100 to 400 ft[1] |
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]