Garber Sandstone

Garber Sandstone Stratigraphic range: Permian
Type	Formation
Underlies	Hennessey Formation
Overlies	Chase Group
Thickness	100 to 400 ft
Lithology
Primary	Sandstone
Other	conglomerate, shale, siltstone, chert
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.

The upper portion of the Garber is associated with extensive baryte mineralization associated with desert rose occurrences in the outcrop area.