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Landslides as Important Disturbance Regimes — Causes and Regeneration.

Authors :
Caldwell, M. M.
Heldmaier, G.
Jackson, R. B.
Lange, O. L.
Mooney, H. A.
Schulze, E. -D.
Sommer, U.
Beck, Erwin
Bendix, Jörg
Kottke, Ingrid
Makeschin, Franz
Mosandl, Reinhard
Bussmann, R. W.
Wilcke, W.
Richter, M.
Source :
Gradients in a Tropical Mountain Ecosystem of Ecuador; 2008, p319-330, 12p
Publication Year :
2008

Abstract

Landslides are part of rapid mass movement events, and considered processes of denudation. The classification scheme in Fig. 24.1 identifies different processes with regard to the type of movement in relation to the type of material (Varnes 1978). Other classification systems (e.g. Ahnert 1996; Crozier 1986a; Dikau et al. 1996; Hutchinson 1988) consider the medium of transport (gravitation, pore water, snow, soil ice, etc.) or the velocity of the phenomenon (rapid, intermediate, slow). [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISBNs :
9783540735250
Database :
Complementary Index
Journal :
Gradients in a Tropical Mountain Ecosystem of Ecuador
Publication Type :
Book
Accession number :
33673611
Full Text :
https://doi.org/10.1007/978-3-540-73526-7_31