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The debris flow in Log pod Mangartom, NW Slovenia
2008
WIT Transactions on Engineering Sciences
unpublished
In November 2000, heavy rains in Slovenia triggered numerous slope processes. Among the largest were the landslide and debris flow in Log pod Mangartom in western Slovenia. This paper describes the main geographical, geological, and geomechanical features of the debris flow, detailing its causes and describing the consequences. The facts presented in the article demonstrate that intensive geomorphic processes are relatively frequent phenomena and are an important factor in the transformation of the surface in alpine regions.
doi:10.2495/deb080131
fatcat:t6zx2mjsenenlfz4ka5aemrnce