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 Garber-Wellington Aquifer, Association of Central Oklahoma Governments

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

See also

List of fossiliferous stratigraphic units in Oklahoma

References