Garber Sandstone
In today's world, Garber Sandstone is a topic that has become increasingly relevant. Whether due to its impact on society, the economy or culture, Garber Sandstone has captured the attention of millions of people around the world. From its origins to the present, Garber Sandstone has generated debates, controversies and significant advances that have marked the history of humanity. In this article we will explore various aspects of Garber Sandstone, analyzing its importance, its implications and its evolution over time. Without a doubt, Garber Sandstone is a topic that leaves no one indifferent and that deserves to be studied and understood in its entirety.
| Garber Sandstone | |
|---|---|
| Stratigraphic range: Permian | |
| Type | Formation |
| Unit of | Wichita 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.
See also
References
- ^ a b Garber Sandstone, USGS: Mineral Resources > Online Spatial Data
- ^ The Garber-Wellington Aquifer, Association of Central Oklahoma Governments
- ^ 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
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