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The geology of Kansas encompasses the geologic history and the presently exposed rock and soil. Rock that crops out in the US state of Kansas was formed during the Phanerozoic eon , which consists of three geologic eras : the Paleozoic , Mesozoic and Cenozoic .
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Spring River, Kansas. Nearly 75 mi (121 km) of the state's northeastern boundary is defined by the Missouri River.The Kansas River (locally known as the Kaw), formed by the junction of the Smoky Hill and Republican rivers at appropriately-named Junction City, joins the Missouri River at Kansas City, after a course of 170 mi (270 km) across the northeastern part of the state.
New geologic maps are now available for Saline County in central Kansas and Kearny County in the southwest. A detailed KGS study underway of the stratigraphic architecture of the High Plains aquifer is being funded by a grant from the National Science Foundation (NSF).
Monument Rocks (also Chalk Pyramids) are a series of large chalk formations in Gove County, Kansas, rich in fossils. The formations were the first landmark in Kansas chosen by the U.S. Department of the Interior as a National Natural Landmark. The chalk formations reach a height of up to 70 ft (21 m) and include formations such as buttes and ...
Print/export Download as PDF; Printable version; In other projects ... Pages in category "Geology of Kansas" The following 18 pages are in this category, out of 18 ...
Structures of Kansas showing the Nemaha Uplift/Ridge. The Nemaha Ridge (also called the Nemaha Uplift and the Nemaha Anticline [1]) is located in the Central United States.It is a buried structural zone associated with a granite high in the Pre-Cambrian basement that extends from approximately Omaha, Nebraska to Oklahoma City, Oklahoma.
Excellent examples of collapse features formed by groundwater geological processes. Monument Rocks: 1968: Gove: Private Pinnacles, small buttes, and spires of Niobrara formation chalk. Rock City: 1976