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A Tapestry of Time and Terrain:
The Union of Two Maps - Geology and Topography
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The Great Plains

Select a new feature About the Cretaceous Period About the Lower Tertiary \About the Upper Tertiary
Great Plains
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The Great Plains Province, a broad yellowish band down the center of the map, is a vast east-tilted surface formed by deposition of sediment eroded from the uplifting Rocky Mountains in Early Tertiary time, beginning about 65 million years ago. This upraised region now is being eroded, especially on its eastern margin, by many east-flowing rivers that expose the older rocks beneath. To the west, these older, largely Cretaceous, sedimentary rocks contain some of the Nation's most spectacular dinosaur fossils.

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Last Modification: 18 Oct 2000 (ebj)
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