Great Plains Geology
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Normal fault in the Fort Hays member of the Cretaceous Niobrara Formation, south of Stockton, Kansas. These chalk beds were originally deposited in the shallow Western Interior Seaway about 80 million years ago. The thick beds of the Fort Hays member are extensively bioturbated. Faulting is post-Cretaceous and pre-Quat...
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Normal fault in the Fort Hays member of the Cretaceous Niobrara Formation, south of Stockton, Kansas. These chalk beds were originally deposited in the shallow Western Interior Seaway about 80 million years ago. The thick beds of the Fort Hays member are extensively bioturbated. Faulting is post-Cretaceous and pre-Q...
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- Roadcut Two Miles South of Codell, Kansas - Cretaceous Niobrara Formation, Fort Hays - Smoky Hill Members Contact by Ron Schott
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Just up the hill from www.gigapan.org/viewGigapan.php?id=1955 . It was a very cold morning. I was glad to get back in the car out out the wind while the robot did its thing. :-)
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- Roadcut Two Miles South of Codell, Kansas - Cretaceous Niobrara Formation, Fort Hays Member by Ron Schott
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Taken just after sunrise. The sun ducked behind a cloud for the right side of the panorama.
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Taken just before sunset. The shadows in the bottom right of this Giagpan weren't in view when I started shooting.
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Roadcut in Quaternary alluvium, south edge of Solomon River valley, west of Stockton, Kansas
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