'Toadstool Park, Nebraska'

'Toadstool Park, Nebraska'

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Credit: JIM STEINBERG/SCIENCE PHOTO LIBRARY

Caption: Toadstool Park in Oglala National Grassland, Nebraska. Toadstools form because hard layers of rocks embedded within the softer layers erode more slowly, leaving ''caps'' resembling toadstools.

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Keywords: badlands, bedded, bedding, differential erosion, eroded, erosion, erosive feature, geology, geomorphology, nebraska, nebraska badlands, oglala national grassland, rock formations, rock layers, sedimentary rock, sideways, toadstool geologic park, toadstool park, weathered, weathering

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