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Slope-Channel Coupling as a Factor in the Evolution of Mountains by Malgorzata Wistuba
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Slope-Channel Coupling as a Factor in the Evolution of Mountains

The Western Carpathians and Sudetes
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Description

In this thesis, coupling between the delivery of slope material into valley floors and river erosion is considered to be a factor in the evolution of mid-altitude, forested mountains. Analyses of slope-channel interactions were made in ten small catchments with particular emphasis on landsliding-erosion feedback. An original, new dendrogeomorphic approach was applied to determine the cyclic occurrence of landsliding and erosion during recent decades. The results of dendrochronological studies show that the processes studied are strongly interdependent. Fluvial erosion can trigger landsliding by undermining slope bases. Landsliding can intensify erosion by delivering slope material into valley floors. The results of dendrochronological studies have permitted a better understanding of the relief observed in areas where landslides and erosion are coupled. A scheme was established which describes the importance of coupling in the evolution of mid-mountain landscape.
Release date Australia
September 24th, 2016
Audience
  • Professional & Vocational
Edition
Softcover reprint of the original 1st ed. 2014
Illustrations
39 Illustrations, color; 70 Illustrations, black and white; XIII, 224 p. 109 illus., 39 illus. in color.
Pages
224
Dimensions
155x235x13
ISBN-13
9783319382968
Product ID
26165094

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Slope-Channel Coupling as a Factor in the Evolution of Mountains on Hardback by Malgorzata Wistuba Save $74
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