http://www.cnr.it/ontology/cnr/individuo/prodotto/ID66777
A surge-type movement et Ghiacciaio del Belvedere and a developing slope instability in the east face of Monte Rosa, Macugnaga, Italian Alps (Articolo in rivista)
- Type
- Label
- A surge-type movement et Ghiacciaio del Belvedere and a developing slope instability in the east face of Monte Rosa, Macugnaga, Italian Alps (Articolo in rivista) (literal)
- Anno
- 2002-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1080/002919502760056422 (literal)
- Alternative label
Haeberli W. (a), Kaeaeb A. (a), Paul F. (a), Chiarle M. (b), Mortara G. (b), Mazza A. (c), Deline P. (d), Richardson S. (e) (2002)
A surge-type movement et Ghiacciaio del Belvedere and a developing slope instability in the east face of Monte Rosa, Macugnaga, Italian Alps
in Norsk geografisk tidsskrift (Online)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Haeberli W. (a), Kaeaeb A. (a), Paul F. (a), Chiarle M. (b), Mortara G. (b), Mazza A. (c), Deline P. (d), Richardson S. (e) (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- (a) Glaciology and Geomorphodynamics Group, Geography Department, University of
Zurich, (b) CNR-IRPI, (c) Comitato Glaciologico Italiano, (d) Edytem, Universitè de Savoie, (e) Reynolds Geo-Sciences Ltd (literal)
- Titolo
- A surge-type movement et Ghiacciaio del Belvedere and a developing slope instability in the east face of Monte Rosa, Macugnaga, Italian Alps (literal)
- Abstract
- Extraordinary development s are taking place at Ghiacciaio del Belvedere near Macugnaga, Valle Anzasca, in the Italian Alps. A
surge-type ow acceleration started in the lower parts of the Monte-Rosa east face, leading to strong crevassing and deformation of
Ghiacciaio del Belvedere, with extreme bulging of its orographic right margin. High water pressure and accelerated movement
lasted into winter 2001/2002: in places, the ice is now starting to override moraines from the Little Ice Age. In addition, but fairly
independently , a most active detachment zone for rock falls and debris ows has been developing for several years now in the east
face of Monte Rosa. Besides the scienti c interest in these separate phenomena, both events affect the growing hazard potentia l to
the local infrastructure and must be considered seriously. (literal)
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