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The sand thickness contour map was well prepared by contouring points of equivalent sand thickness acquired from logs of wells and examination holes and doesn't consist of silt and clay beds which were current with the effectively website. The transmissibility map was prepared by implementing permeability values received from chosen pumping tests in the region on the sand and gravel thickness as recorded inside the logs of wells and check holes for those formations for which samples were being readily available. In Substantially of Arkansas Valley, notably in which the entire sand and gravel thickness is finest, the permeability of those sediments decreases with depth. The permeability value placed on someone sand and gravel mattress at a well or exam-hole site was dependant on a comparison with the lithology on the bed with that of similar sediments from wells exactly where permeability data derived from pumping assessments had been out there.
The surface area of a lot of the Ninnescah-Wellington Upland is underlain by loess, which overlies sand and gravel in part of the region. The bedrock area would be the Wellington Formation in with regards to the japanese a single-third and also the Ninnescah Shale in the western two-thirds.
Inside Subarea C1, drilled wells less than 150 feet deep acquire h2o from Answer openings in gypsum and anhydrite beds within the reduced A part of the Wellington Formation. The water is usually less than artesian pressure but flows at the area in only a few locations. A number of creeks within the subarea have Lower into or near the water-bearing, zone, and large springs and seeps provide a perennial flow within the creeks.