Smoky Hill Chalk

geological formation in the United States of America From Wikipedia, the free encyclopedia

Smoky Hill Chalk
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The Smoky Hill Chalk is an Upper Cretaceous conservation Lagerstätte, or fossil-rich geological formation. It is known for its exceptionally well-preserved marine reptiles from the Western Inland Sea.[1]

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This fossil of Toxochelys, an extinct marine turtle, from the Smithsonian's National Museum of Natural History.
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Skull of a female Pteranodon, found in the Smoky Hills Chalk in 1876.

The Smoky Hill Chalk outcrops in parts of northwest Kansas, its most famous localities for fossils, and in southeastern Nebraska. Large well-known fossils excavated from the Smoky Hill Chalk include marine reptiles such as plesiosaurs, large bony fish such as Xiphactinus, mosasaurs, pterosaurs (namely Pteranodon), flightless marine birds such as Hesperornis, and turtles. Many of the most well-known specimens of the marine reptiles were collected by dinosaur hunter Charles H. Sternberg and his son George. The son collected a unique fossil of the giant bony fish Xiphactinus audax with the skeleton of another bony fish, Gillicus arcuatus inside the larger one. Another excellent skeleton of Xiphactinus audax was collected by Edward Drinker Cope during the late nineteenth century heyday of American paleontology.[2]

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