Slushflows were first recorded in the Iberian Peninsula on 18 December 1997
Three slushflows were released at the ski resort of Fl Port del Comte, in
the Catalan Pyrenees, northeast Spain, during intense rainfall. Two of the
slushflows originated on the pistes, and the third affected another piste.
Three ski lifts were damaged. This paper analyzes the hydrogeological chara
cteristics of the massif, the geomorphic features of the terrain and the me
teorological and snowpack conditions that caused the release of the slushfl
ows. Man's role in triggering the slushflows by compacting snow on the pist
es is also considered. Drainage control for reducing the hazard is outlined
, taking into consideration the low frequency of the phenomenon.