Description
Earth's topographic surface forms an interface across which the geodynamic and geomorphic engines interact. This interaction is best observed along crustal margins where topography is created by active faulting and sculpted by geomorphic processes. Crustal deformation manifests as earthquakes at centennial to millennial timescales.
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Contributors
- Haddad, David Elias (Author)
- Arrowsmith, Ramon (Thesis advisor)
- Reynolds, Stephen (Committee member)
- Semken, Steven (Committee member)
- Shirzaei, Manoochehr (Committee member)
- Whipple, Kelin (Committee member)
- Zielke, Olaf (Committee member)
- Arizona State University (Publisher)
Date Created
The date the item was original created (prior to any relationship with the ASU Digital Repositories.)
2014
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Note
- Partial requirement for: Ph.D., Arizona State University, 2014Note typethesis
- Includes bibliographical referencesNote typebibliography
- Field of study: Geological sciences
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by David Elias Haddad