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The sand thickness click here contour map was prepared by contouring details of equivalent sand thickness acquired from logs of wells and check holes and doesn't include silt and clay beds which were current on the effectively website. The transmissibility map was prepared by implementing permeability values received from picked pumping assessments in the area on the sand and gravel thickness as recorded inside the logs of wells and check holes for those formations for which samples have been readily available. In much of Arkansas Valley, significantly the place the entire sand and gravel thickness is greatest, the permeability of these sediments decreases with depth. The permeability benefit applied to an individual sand and gravel bed in a effectively or examination-hole web-site was determined by a comparison with the lithology on the bed with that of comparable sediments from wells in which permeability knowledge derived from pumping tests were being offered.
The surface area of the majority of the Ninnescah-Wellington Upland is underlain by loess, which overlies sand and gravel in part of the region. The bedrock floor may be the Wellington Development in in regards to the jap just one-third and the Ninnescah Shale during the western two-thirds.
In Subarea C1, drilled wells fewer than 150 feet deep get water from Resolution openings in gypsum and anhydrite beds during the decreased Section of the Wellington Development. The drinking water is often underneath artesian tension but flows in the surface area in only a few areas. Numerous creeks while in the subarea have Minimize into or close to the drinking water-bearing, zone, and huge springs and seeps supply a perennial circulation inside the creeks.