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  • © 1998

Geomorphological Hazards in High Mountain Areas

Part of the book series: GeoJournal Library (GEJL, volume 46)

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Table of contents (16 chapters)

  1. Front Matter

    Pages i-xi
  2. Catastrophic Flood Flushing of Sediment, Western Himalaya, Pakistan

    • J F. Shroder Jr., M. P. Bishop, R. Scheppy
    Pages 27-48
  3. Landslides and Deserted Places in the Semi-Arid Environment of the Inner Himalaya

    • Jussi Baade, Roland Mäusbacher, Günther A. Wagner, Erwin Heine, Robert Kostka
    Pages 49-62
  4. The Salt Weathering Hazard in Deserts

    • Andrew Goudie
    Pages 107-120
  5. Landslides in the Rocky Mountains of Canada

    • D. M. Cruden, X. Q. Hu
    Pages 133-148
  6. Late Holocene Sturzstroms in Glacier National Park, Montana, U.S.A.

    • David R. Butler, George P. Malanson, Forrest D. Wilkerson, Ginger L. Schmid
    Pages 149-166
  7. Andean Landslide Hazards

    • T. A. Blodgett, C. Blizard, B. L. Isacks
    Pages 211-227
  8. Fluvial Hazards in a Steepland Mountain Environment, Southern Bolivia

    • Jeff Warburton, Mark Macklin, David Preston
    Pages 229-243
  9. Back Matter

    Pages 309-316

About this book

On the basis of a total of thirteen case examples from the Tien Shan, Karakorum, Himalaya and Tangula Shan (central Tibet), the risk potential and hazards are inferred from the development of landscape during the Quaternary. The history of glaciers can be seen as of central importance for this. The Ice Age glacial erosion created V-shaped valleys, which with their steep flanks - as a consequence of the interglacial formation of V -valleys - have prepared and brought about landslides as well as rockslides and the hazards, combined with them. The same is true for the moraines, which the gla­ ciers have deposited high-up in the valley flanks and related loose stone deposits. Dry and wet mass movements follow after heavy precipitation, especially in the semi-arid investigation areas, and are catastrophes for the settlements and the communication routes in the valley floors. Their key-forms are debris cones and debris slopes, as well as mudflows and alluvial fans. In addition to the Ice Age glaciation history, as a preparatory, indirect factor, the Holocene to present glaciation history is, as a result of the danlming-up of glacier- and moraine lakes and their outbursts, a direct risk factor. The examples presented of acute and already occurred cases of damage were inves­ tigated in the years 1989-1994. Acknowledgements The authors wish to thank the Deutsche Forschungsgemeinschaft (DFG), the Max Planck-Gesellschaft (MPG), the Volkswagen-Stiftting (VW) and the Deutscher Aka­ demischer Austauschdienst (DAAD) for the financial support for the field-work.

Editors and Affiliations

  • Faculty of Science, Charles University, Prague, Czech Republic

    Jan Kalvoda

  • Oregon State University, Corvallis, USA

    Charles L. Rosenfeld

Bibliographic Information

  • Book Title: Geomorphological Hazards in High Mountain Areas

  • Editors: Jan Kalvoda, Charles L. Rosenfeld

  • Series Title: GeoJournal Library

  • DOI: https://doi.org/10.1007/978-94-011-5228-0

  • Publisher: Springer Dordrecht

  • eBook Packages: Springer Book Archive

  • Copyright Information: Springer Science+Business Media Dordrecht 1998

  • Hardcover ISBN: 978-0-7923-4961-7Due: 31 March 1998

  • Softcover ISBN: 978-94-010-6200-8Published: 14 October 2012

  • eBook ISBN: 978-94-011-5228-0Published: 06 December 2012

  • Series ISSN: 0924-5499

  • Series E-ISSN: 2215-0072

  • Edition Number: 1

  • Number of Pages: XI, 316

  • Topics: Hydrogeology, Physical Geography, Environmental Management

Buy it now

Buying options

eBook USD 39.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book USD 54.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Other ways to access