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In Slate Creek valley no Get in touch with between alluvium and Wisconsinan terrace deposits is discernible; as a result Modern alluvium On this valley is presumed to get current only in the bottom in the creek channel. Due to the fact alluvium and Wisconsinan terrace deposits can't be differentiated during the subsurface, your complete thickness of unconsolidated sediments fundamental the flood plains on the streams is treated as Latest alluvium in logs and sections.
The sand dunes are over the h2o table and don't generate drinking water to wells, but due to their higher porosity and permeability and incomplete drainage, they serve as significant recharge locations.
The reduce Portion of the Nebraskan deposits is made up chiefly of great to medium sand but includes minor quantities of coarse sand and arkosic gravel. The upper component is made of silt and tan or pink sandy clay. The best identified thickness of those deposits in Sumner County is about 90 feet.
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The Modern alluvium in Sumner County resembles lithologically the Wisconsinan terrace deposits from which almost all of it absolutely was derived. While in the Arkansas, Ninnescah, and Chikaskia River clear glass plates valleys the basal Portion of the alluvial deposits includes coarse sand and gravel, which grades upward into finer sand and silt. The alluvium of Bluff Creek is composed mainly of fine sand, silt, and clay.
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The Wellington Formation underlies all of Sumner County other than perhaps compact locations from the valley of Arkansas River. During the jap two-thirds of your county the development crops out or is covered by Pleistocene deposits; inside the western third with the county it is actually overlain by the Ninnescah Shale.
The Wellington Formation yields only compact quantities of h2o to wells in Sumner County. Almost all of the material composing the development is almost impermeable, and also the drinking water arises from small fracture zones or from slender limestone lenses. Because of this the Wellington is amazingly unpredictable as an aquifer.
Quite a few dune tracts border Chikaskia and Arkansas Rivers. These types of tracts lie to the north facet on the rivers or north of particular massive loops or bends inside the rivers. The dunes are composed generally of fantastic- to medium-grained well-rounded quartz sand, which has been blown within the flood plains of your rivers through the prevailing south winds.
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Most of the dunes are only sparsely vegetated and therefore are subject to blowouts in the course of intervals of potent wind and drought.