Description
The morphology of mountainous areas is strongly influenced by stream bed incision rates, but most studies of landscape evolution consider erosion at basin scales or larger. The research here attempts to understand the smaller-scale mechanics of erosion on exposed bedrock channels in the conceptual framework of an established saltation-abrasion model by Sklar and Dietrich [2004].
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Contributors
- Adams, Mark (Author)
- Whipple, Kelin (Thesis advisor)
- Heimsath, Arjun (Committee member)
- Schmeeckle, Mark (Committee member)
- Arizona State University (Publisher)
Date Created
The date the item was original created (prior to any relationship with the ASU Digital Repositories.)
2016
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Note
- Partial requirement for: M.S., Arizona State University, 2016Note typethesis
- Includes bibliographical references (pages 84-85)Note typebibliography
- Field of study: Geological sciences
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by Mark Adams