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  2. Geology of Kansas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Kansas

    Humboldt Fault (red) and Midcontinent Rift (green) in Kansas and Nebraska. The Nemaha uplift is a deep fault zone which runs diagonally across east Kansas and extends from just south of Omaha, Nebraska to Oklahoma City. This fault zone directly overlies a granite "high" in the Precambrian basement and is structurally active as the Humboldt Fault.

  3. Nemaha Ridge - Wikipedia

    en.wikipedia.org/wiki/Nemaha_Ridge

    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.

  4. Monument Rocks (Kansas) - Wikipedia

    en.wikipedia.org/wiki/Monument_Rocks_(Kansas)

    Designated. 1968. 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 ...

  5. SubTropolis - Wikipedia

    en.wikipedia.org/wiki/SubTropolis

    SubTropolis. Location. Kansas City, Missouri, United States. Coordinates. 39°09′40″N 94°28′34″W  /  39.161213°N 94.476242°W  / 39.161213; -94.476242. The interior of SubTropolis. SubTropolis is a business complex located inside of a 55,000,000-square-foot (5,100,000 m 2), 1,100-acre (4.5 km 2) mine in the bluffs north of ...

  6. Wichita Mountains - Wikipedia

    en.wikipedia.org/wiki/Wichita_Mountains

    The Wichita Mountains are located in the southwestern portion of the U.S. state of Oklahoma. [1] It is the principal relief system in the Southern Oklahoma Aulacogen, being the result of a failed continental rift. The mountains are a northwest-southeast trending series of rocky promontories, many capped by 500 million-year old granite.

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