On June 3,1995, during a field campaign in the Kärkevagge, a drainage basin in Swedish Lapland, a slush torrent could be observed and documented by a time series of photographs and by video recordings. Thus, information on dynamical features of slush torrents are rather limited, and most results are based on qualitative observations. This particularly holds for slush torrents which are major slushflow events reaching supercritical flow velocities. Most of the observed events occurred in mountainous drainage basins at high latitudes, so relatively few observations and measurements are presented in the scientific literature. Slushflows have been investigated in various regions of the Earth for more than forty years.
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