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The Aspen Grove Landslide, Ephraim Canyon, Central Utah. Open Access Deposited
The Aspen Grove landslide, central Utah, occurred in older landslide debris. The debris is about 6-15 meters thick, and consists of medium- to high-plasticity clays and silty clays. Persistent landslide structures, including toes, hollows, and flank ridges, outline dimly preserved landslide masses in the older debris.
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Permanent link to this page: https://scholar.uc.edu/show/2514nk53w