In September 2002, a part (>0,1 × 106 m3) of the Frébouge Glacier (Val Ferret) front avalanched onto the apex of the polygenic fan. The 0.1 × 106 m3 deposit was composed of poorly-sorted, subspherical, open- work ice particles and formed a lobate front; the lateral margins are steep metric ridges, along longitudinal shear zones. Some big ice boulders rolled 100-150 m ahead the front. Following Alean's (1985) ice avalanching typology, the Frébouge event is a type IA event: that is to say, avalanching of a low elevation temperate glacier front on a steep rock bed. Others type IA ice avalanches have probably occured in recent decades, but the rapid fusion of avalanche deposits makes their survey difficult. The ignorance of this process frequency explains its underestimation in alpine hazard analysis.
Il crollo frontale del Ghiacciaio di Frébouge (Massiccio del Monte Bianco, Valle d'Aosta) del 18 settembre 2002
Chiarle;Mortara;
2002
Abstract
In September 2002, a part (>0,1 × 106 m3) of the Frébouge Glacier (Val Ferret) front avalanched onto the apex of the polygenic fan. The 0.1 × 106 m3 deposit was composed of poorly-sorted, subspherical, open- work ice particles and formed a lobate front; the lateral margins are steep metric ridges, along longitudinal shear zones. Some big ice boulders rolled 100-150 m ahead the front. Following Alean's (1985) ice avalanching typology, the Frébouge event is a type IA event: that is to say, avalanching of a low elevation temperate glacier front on a steep rock bed. Others type IA ice avalanches have probably occured in recent decades, but the rapid fusion of avalanche deposits makes their survey difficult. The ignorance of this process frequency explains its underestimation in alpine hazard analysis.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
