Haskell Limestone
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Haskell Limestone
Haskell limestone is a geological unit name originating in Kansas and used in adjoining states. The unit was named in 1931 by R.C. Moore for the then Haskell Indian Nations University, Haskell Institute in the southeast of Lawrence, Kansas. The name has been applied to various beds within this range, and assigned as a member variously to the Lawrence Formation, Cass Formation, and Stranger Formation, and significant legacy literature exists for each classification. These three formations now comprise the Douglas Group. In 2002, within the effort to improve the correlation of Kasimovian, Missourian stage geology between the states of Missouri and Kansas, as well as Nebraska and Iowa, the Haskell was assigned in Kansas to the Cass Formation as its lowest member (on the basis of Principle of faunal succession, distinct changes in fossil species). Distribution and outcrop The Haskell Limestone is recognized in deep hydrocarbon well logs throughout most of the state of Kansas; the " ...
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Wakarusa River
The Wakarusa River is a tributary of the Kansas River, approximately long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed March 30, 2011 in eastern Kansas in the United States. It drains an agricultural area of rolling limestone hills south of Topeka and Lawrence. Description It rises in several branches located southwest of Topeka. The main branch rises on the Wabaunsee-Shawnee county line, approximately southwest of Topeka and flows east. The South Branch rises in eastern Wabaunsee County, approximately southwest of Topeka and flows east-northeast, joining the main branch south of Topeka. The main branch flows generally east, flowing south of Lawrence. It joins the Kansas River in Douglas County at Eudora, approximately east of Lawrence. It is impounded by Clinton Dam approximately southwest of Lawrence to form Clinton Lake. The river is known for its gentle current that winds through river-level outcroppi ...
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