Garber Sandstone

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]

See also

• Oklahoma portal
• Paleontology portal

• List of fossiliferous stratigraphic units in Oklahoma