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Home > Explore! > Surficial Geology > Surficial Geologic History > Figure 13
Figure 13. Sand dune in Wayne. This and other "deserts" in Maine formed as windstorms in late-glacial time blew sand out of valleys, often depositing it as dune fields on hillsides downwind. Some dunes were reactivated in historical time when grazing animals stripped the vegetation cover. Last updated on October 6, 2005 |
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