small shell fossils on a brown cave wall
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Brachiopods in Wind Cave
small shell fossils on a brown cave wall
Brachiopods are shellfish that were extremely common when the Pahasapa Limestone was formed. The calcium from the shells and bones of dead sea creatures were crushed by pressure to create the limestone that Wind Cave sits in. These are the most common fossils seen in the cave and are one to two inches wide on average. Most species of brachiopods are extinct.
U.S. National Park Service
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Wind Cave National Park, Code: WICA
Wind Cave National Park, Custer County, South Dakota
Latitude: 43.5802993774414, Longitude: -103.439002990723

7/16/2010 1:22:36 AM
Friday, July 3, 2020 11:07:47 AM
Friday, July 3, 2020 11:07:47 AM
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