Flow mud
The flow mud is fastest (up to 80 km/h) and more fluid of the various types of movements of ground. It is made up from at least 30% of Eau and 50% of silts, Vase S and other materials Argile ux.
The mud flows are often formed on Versant S and are constituted in River with mode Torrent iel. The destroying power of some of enters allows a comparison with the Avalanche S.
This hydrological phenomenon appears in particular in the arid areas and semi-arid where one can observe long periods of followed Sécheresse unexpected Averse S and ielles Torrent. These last so brutally hydrate the ground S, strongly desiccated, which they exhaust and enlarge these temporary rivers. It is then about a phenomenon of Solifluxion.
See too
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