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Tectonic Geomorphology, Quaternary Chronology, and Paleoseismicity

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Developments and Applications of Geomorphology

Abstract

Tectonic geomorphology, defined as the application of geomorphology to tectonic problems, includes the study of landform assemblages and landscape evolution as well as development of process-response models for areas and regions affected by recent tectonic activity. Of particular interest in the study of the earthquake hazard for a particular area are problems associated with deriving rates of faulting and determination of paleoseismicity (study of prehistoric earthquakes) for the late Pleistocene and Holocene. Tectonic geomorphology is a relatively new branch of applied geomorphology, the study of which requires understanding of a number of disciplines other than geomorphology including structural geology, Quaternary stratigraphy, pedology and geochemistry as it relates to weathering-soils and absolute dating techniques.

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Authors and Affiliations

  1. Department of Geological Sciences, University of California, Santa Barbara, CA, 93106, USA

    E. A. Keller

  2. Department of Geological Sciences, California State University, San Diego, CA, 92182, USA

    T. K. Rockwell

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  1. E. A. Keller
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  2. T. K. Rockwell
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Editors and Affiliations

  1. Denver Federal Center, U. S. Geological Survey, Mail Stop 413, 80225, Lakewood, CO, USA

    John E. Costa

  2. Earth Science Department, State University College, 13820, Oneonta, NY, USA

    P. Jay Fleisher

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© 1984 Springer-Verlag Berlin Heidelberg

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Keller, E.A., Rockwell, T.K. (1984). Tectonic Geomorphology, Quaternary Chronology, and Paleoseismicity. In: Costa, J.E., Fleisher, P.J. (eds) Developments and Applications of Geomorphology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-69759-3_7

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  • DOI: https://doi.org/10.1007/978-3-642-69759-3_7

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