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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 ...
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List of counties in Oklahoma; National Register of Historic Places listings in Garfield County, Oklahoma; North Enid, Oklahoma; R. E. Hoy No. 1 Oil Well; Waukomis, Oklahoma; Waverley Historic District (Enid, Oklahoma) User:Nyttend/County templates/OK; Template:Garfield County, Oklahoma; Template:NRHP in Garfield County, Oklahoma; Category ...
Aquifers of the United States Withdrawal rates from the Ogallala Aquifer.. This is a list of some aquifers in the United States.. Map of major US aquifers by rock type. An aquifer is a geologic formation, a group of formations, or a part of a formation that contains sufficient saturated permeable material to yield significant quantities of water to groundwater wells and springs.
English: The maps use data from nationalatlas.gov, specifically countyp020.tar.gz on the Raw Data Download page. The maps also use state outline data from statesp020.tar.gz . The Florida maps use hydrogm020.tar.gz to display Lake Okeechobee.
The Wellington Formation is an Early Permian geologic formation in Kansas and Oklahoma. [2] The formation's Hutchinson Salt Member is more recognized by the community than the formation itself, and the salt is still mined in central Kansas. [ 3 ]
The Hoy sand was the first successful sand of the Garber-Covington oil field, and the first well to be drilled with the advice of a geologist. [ 2 ] [ 3 ] From 1916 to 1940 the well utilized primary production, adding secondary methods of gas injection (1941 to 1948) and waterflooding (since 1948). [ 2 ]
The Texas and Oklahoma red beds are sedimentary rocks, mostly consisting of sandstone and red mudstone. [8] The red color of the rocks is due to the presence of ferric oxide . [ 9 ] The rocks were deposited during the early Permian in a warm, moist climate, [ 10 ] with seasonal periods of dry conditions.