In: Journal of Glaciology, 2016, vol. 62, no. 233, p. 535–551
Glacier response to climate forcing can be heterogeneous and complex, depending on glacier system characteristics. This article presents the decadal evolution of the Tsarmine Glacier (Swiss Alps), a very small and heavily debris-covered cirque glacier located in the Alpine periglacial belt. Archival aerial photogrammetry and autocorrelation of orthophotos were used to compute surface...
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In: Journal of Maps, 2016, vol. 12, no. 1, p. 160–172
This paper presents a geomorphological map of the Hérens valley in the Western Swiss Alps. With an area of 270 km2 and altitudes ranging from 470 to 4357 m a.s.l., this valley is one of the main secondary catchments of the Upper Rhône valley. The high differences in altitudes, combined with a varied geology, create an important geomorphic diversity. The main processes active in mountain...
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Lausanne : Université de Lausanne - Faculté des lettres, 2006
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In: Geomorphology, 2011, vol. 132, no. 3-4, p. 208-221
In order to determine the spatial extension and the characteristics of permafrost within alpine talus slopes, two sites located in the western part of the Swiss Alps were studied using borehole drilling and electrical resistivity tomography (ERT) profiles. Three boreholes were drilled along an upslope–downslope transect in both talus slopes. In both sites, frozen sediments are present only in...
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In: Bulletin de la Murithienne, 2004, no. 122, p. 89-102
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In: Bulletin de la Murithienne, 2003, no. 121, p. 83-97
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In: Bulletin de la Murithienne, 2003, no. 121, p. 7-20
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In: Bulletin de la Murithienne, 2002, no. 120, p. 19-24
Concerne: le Mont Dolin (Arolla) et Wisse Schijen (Randa).
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In: Bulletin de la Murithienne, 1999, no. 117, p. 89-104
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In: Bulletin de la Murithienne, 1996, no. 114, p. 135-150
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