2012
DOI: 10.1007/s11069-012-0381-4
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Landslide susceptibility zonation in Greece

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Cited by 103 publications
(85 citation statements)
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“…Class scores are based on the standardization of the Landslide Relative Frequency proposed by Sabatakakis et al [2013].…”
Section: Landslide Susceptibility Indicator (Lssi) Factorsmentioning
confidence: 99%
“…Class scores are based on the standardization of the Landslide Relative Frequency proposed by Sabatakakis et al [2013].…”
Section: Landslide Susceptibility Indicator (Lssi) Factorsmentioning
confidence: 99%
“…For the aims of this study the highest class includes slopes and escarpments susceptible to both landslides and rock falls. Class scores are based on the standardization of the Landslide Relative Frequency proposed by Sabatakakis et al (2013).…”
Section: Lssi = W1sa + W2sf + W3e+w4l+w5tlpmentioning
confidence: 99%
“…The occasional planar slip surfaces are located in the weathered zone of marls or flysch while ground water level reaches the surface of the slope during heavy rainfall. The most critical landslide-prone formations regarding lithology, and structure are flysch and neogene sediments, while schist and cherts significantly contribute in landslide phenomena [55]. Slides which usually take place in the gentle slope of flysch mantle are typically quite shallow and take form of a sheet of weathered zone sliding on a slip surface parallel to the ground [56].…”
Section: Datamentioning
confidence: 99%
“…In line with [57,58], in this paper the term landslide is used for translational and rotational earth slides, which were recorded in the validation dataset. These events vary consistently in volume, from some thousands of m 3 to several million m 3 [55], and depicting small to extremely large magnitude, according to [59] classification.…”
Section: Datamentioning
confidence: 99%