View Original Image at Full SizeDepiction of the Channeled Scabland and Palouse region during the last glacial maximum. Old loess was scoured by floods to leave a braided network of loess islands. Floods sediments deposited in basins were reworked by the wind to form sand dunes (black) and loess (yellow). EF is the location of Eureka Flat.
Image 12534 is a 1729 by 2264 pixel WebP
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Jul24 08
Permanent URL: https://serc.carleton.edu/download/images/12534/pacific_northwest_region_lgm.webp
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Mark Sweeney, University of South Dakota
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