Details, Fiction and clear glass plates

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The Ninnescah consists chiefly of reddish-brown silty shale that contains many beds of slender calcareous siltstone and blocky reddish-brown shale possessing scattered greenish-grey places, and, within the higher part, skinny beds of quite good grained sandstone. Regionally there are numerous modest veinlets of gypsum or gypsiferous siltstone. Just a A part of the Ninnescah Shale, about 250 feet, is current in Sumner County.

A significant upland area in the northwest corner of Sumner County is mantled with sand and gravel of Nebraskan age. These deposits address an area of about thirty sq. miles and appear to fill a broad, shallow channel or bedrock sag, which aligns close to with the current study course of Slate Creek.

Much of Sumner County is mantled by an accumulation of colluvium. These deposits, of Illinoisan to The latest age, had been formed partly by weathering of Permian shales set up and partly by deposition of silt, clay, and sand by sheet clean or unconcentrated wash.

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The salt beds are overlain by about 300 toes of shale constituting the higher Section of the Wellington Formation. Purple and purplish-red shale is considerably more popular in the upper Component of the development than while in the lower element. The Milan Dolostone member, which crops out inside the lender of Chikaskia River south of Milan, types the very best in the Wellington Formation.

In Sumner County the Wisconsinan terrace deposits alongside Arkansas River produce significant portions of h2o of high quality except in community places polluted by oil-discipline brine or sewage. Wisconsinan terrace deposits alongside Ninnescah River yield average to huge quantities of h2o. In almost all of the valley, the standard of h2o from these deposits is sweet except for regionally troublesome quantities of iron.

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The Wellington Formation yields only little portions of drinking water to wells in Sumner County. Most of the material composing the development is almost impermeable, plus the drinking water arises from tiny fracture zones or from thin limestone lenses. Because of this the Wellington is extremely unpredictable as an aquifer.

A lot of dune tracts border Chikaskia and Arkansas Rivers. Many of these tracts lie over the north aspect of your rivers or north of specific big loops or bends from the rivers. The dunes are composed mainly of great- to medium-grained nicely-rounded quartz sand, which has been blown from your flood plains on the rivers from the prevailing south winds.

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They seldom exceed 20 ft in thickness but in areas of low topographic reduction They might completely conceal the underlying product around several square miles. On Plate 1 the colluvial deposits that overlie Permian shale are differentiated from those who overlie discontinuous Kansan or Illinoisan terrace deposits.

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