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The Central Kansas Uplift is a broad arch in the rocks of west-central Kansas. The rock units within this arch have been major oil producers. The Anadarko Basin of southwest Kansas contains significant natural gas. The Sedgwick Basin, the Cherokee Basin and the Forest City Basin of south and east Kansas also produce petroleum and natural gas. [22]
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 ...
In eastern Kansas, abundant, large, flinty stones could be collected from the hills and fields to build long stone walls. However, in several counties in central Kansas, where most of the rock was soft shale or chalk, a practical alternative was available; one particular bed of stone had ideal properties to substitute for wood fenceposts.
Leaders of states in the U.S. which have significant mineral deposits often create a state mineral, rock, stone or gemstone to promote interest in their natural resources, history, tourism, etc. Not every state has an official state mineral, rock, stone and/or gemstone, however.
Similarly, "Manhattan stone" was the commercial name used for the same limestone when quarried in the vicinity of Manhattan, Kansas. [4] It was also called "Alma Limestone" when first quarried at Alma, Kansas. [6] [7] The Cottonwood Limestone is one of the most persistent and easily recognizable horizons in Kansas.
This limestone outcrops in east-central Kansas, extending into northeast-central Oklahoma and southeastern Nebraska, in the Midwestern United States. Its conspicuous "rim rock" marker horizon outcrop caps the bluffs overlooking the original buildings of Fort Riley, as well as the Marshall Army Airfield opposite the Kansas River. [5] [6] [7]
Defining the southeast border of the High Plains, the towering stone-capped bluffs of the Fort Hays Escarpment are "perhaps the most conspicuous physiographic boundary in Kansas." [3] The iconic stone blockhouse of Fort Hays is built from the namesake limestone. The Fort Hays Limestone was a generally practical building stone.
The iconic stone posts of Kansas were cut from a layer in the Greenhorn.. The formation was named for the Greenhorn Station on Greenhorn Creek in Colorado in 1896 by Grove Karl Gilbert; [2] and it is the namesake of the Greenhorn Marine Cycle of the Cretaceous Western Interior Seaway.