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Publications by [Sartori M.]

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<p>About 22 mio m<sup>3</sup> of rock fell from a cliff near the village of Randa (10 km north of Zermatt, Switzerland) on 18 April 1991. A second retrogressive rockslide of about 7 miom<sup>3</sup> followed on 9 May 1991. At present, a rock mass situated ...
Reference: Natural Hazards and Earth System Sciences (2003) 3: 423–433
A posteriori studies of rock slope instabilities generally show that rockfalls do not occur at random locations: the failure zone can be classified as sensitive from geomorphological evidence. Zones susceptible to failure can therefore be detected. Effects ...
Filed under: Rock Mechanics -  Rock Falls
Reference: Natural Hazards and Earth System Sciences (2003) 3: 431–438