Elements and Their Compounds in the Environment 2004
DOI: 10.1002/9783527619634.ch23j
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Cited by 3 publications
(2 citation statements)
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“…Removal of material (in red), no change (in yellow) and deposition of material (in green). The resulting patterns reflect the landslide dynamics: red colours dominate in the upper scarp section, and alternate with distinct zones of deposition and no change, which suggests slide-like movement, which is in accordance with observations by Jaritz and Marte (2008). Deposition predominates in the toe area of the slide, without interruptions of vast removal and no change areas, suggesting flow-type accumulations to prevail in the lower section of the landslide.…”
Section: Topographical Changesupporting
confidence: 73%
See 1 more Smart Citation
“…Removal of material (in red), no change (in yellow) and deposition of material (in green). The resulting patterns reflect the landslide dynamics: red colours dominate in the upper scarp section, and alternate with distinct zones of deposition and no change, which suggests slide-like movement, which is in accordance with observations by Jaritz and Marte (2008). Deposition predominates in the toe area of the slide, without interruptions of vast removal and no change areas, suggesting flow-type accumulations to prevail in the lower section of the landslide.…”
Section: Topographical Changesupporting
confidence: 73%
“…Major events occurred in the early 1927, 1935 and 1988, during which 2-3x10 6 m 3 was mobilized as rock-and soil slides, and debris flows (Jaritz and Marte, 2008). The geology is formed by a tilted sedimentary sequence of alternating Molasse marls, sandstone and conglomerates (Friebe, 2007), that, in combination with a highly fractured rock mass, promotes groundwater flow to potential failure planes, thus reactivating the landslide.…”
Section: Study Areamentioning
confidence: 99%