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Filtering by: Creator/Author Baum, Rex Lee. Department Other

Type:: Etd
Description/Abstract:: 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.
Creator/Author:: Baum, Rex Lee.
Submitter:: UC Libraries
Date Uploaded:: 03/26/2018
Date Modified:: 03/26/2018
Date Created:: 1988

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