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Landslides from Massive Rock Slope Failure pp 573–590Cite as

LANDSLIDE-DRIVEN EROSION AND TOPOGRAPHIC EVOLUTION OF ACTIVE MOUNTAIN BELTS

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Part of the book series: NATO Science Series ((NAIV,volume 49))

Abstract

Landslides play a crucial role in the erosion and topographic evolution of active mountain belts. They drive the expansion of drainage networks in uplifting rock mass, and counter the tectonic mass flux into orogenic systems. Moreover, landslides are the source of most sediment eroded from the continents, and the probability distributions of landslides and their triggers are a first-order control on the variability of the sediment flux from active mountain belts. Here, we illustrate these points with observations from he Southern Alps and other regions of New Zealand, the Central Taiwan Mountains, the Finisterre Mountains of Papua New Guinea and the eastern Greater Caucasus of Azerbaijan.

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Author information

Authors and Affiliations

  1. Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK

    N. HOVIUS

  2. Lamont-Doherty Earth Observatory of Columbia University Route 9W, Palisades, NY, 10964, USA

    C.P. STARK

Authors
  1. N. HOVIUS
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  2. C.P. STARK
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Editor information

Editors and Affiliations

  1. Department of Earth Sciences, University of Waterloo, ON, Canada

    Stephen G. Evans

  2. Department of Earth Sciences, Università degli Studi di Roma, ȘLa Sapienza’, Rome, Italy

    Gabriele Scarascia Mugnozza

  3. Institute of the Geospheres Dynamics, Russian Academy of Sciences, Moscow, Russia

    Alexander Strom

  4. Geological Survey of Canada, Vancouver, BC, Canada

    Reginald L. Hermanns

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HOVIUS, N., STARK, C. (2006). LANDSLIDE-DRIVEN EROSION AND TOPOGRAPHIC EVOLUTION OF ACTIVE MOUNTAIN BELTS. In: Evans, S.G., Mugnozza, G.S., Strom, A., Hermanns, R.L. (eds) Landslides from Massive Rock Slope Failure. NATO Science Series, vol 49. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-4037-5_30

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