Note: This data set was first published on the 1998 CAPS CD.
The text for this document was taken unchanged from that CD.

See also Description of Data Files.


Investigator: Markus Imhof


Institute of Geography / Group for Applied Geomorphology,
University of Bern,
Hallerstrasse 12,
CH-3012 Bern (Switzerland)
Phone: ++41 31 631 85 67
Fax: ++41 31 631 85 11

Description of the study area:

The area investigated covers the entire Bernese Alps (western Switzerland), about 4200 km2 and is situated between 46o 10' - 46o 50' N and 7o 10' - 8o 30' E. The Bernese Alps are one of the main European watersheds, separating the catchment area of the Aare (draining into the North Sea via the Rhine) from that of the Rhone (which flows into the Mediterranean Sea). The lowest points of the the study area are situated in the valley floors of the two rivers at about 500 m ASL, whereas several summits exceed 4000 m ASL (highest point: Finsteraarhorn, 4273 m ASL). The main structure of the Bernese Alps is the crystalline Aar massif striking WSW-ENE and culminating in the western part of the study area. To the north and the west, the massif is covered by thrust nappes consisting of sedimentary rocks mainly of Mesozoic and early Tertiary age (chiefly marine limestones, shales, and sandstones). Their summits are considerably lower (mostly between 2000 and 3500 m ASL).

According to their geographic situation between 46o and 47o N, the climate of the Bernese Alps is of temperate character typical for the zone of the westerlies. Because of the their horizontal and vertical extension, the Alps themselves have considerable influence on the climate. Based on climatic criteria, two main realms can be distinguished: the moist and quite oceanic part in the north of the main watershed and the slightly more continental part sloping south to the Rhone. The northern part, exposed to the westerlies, shows maximum precipitation during summer, with quite low variabilities, whereas the south is somewhat dryer, showing no distinct maximum but higher variabilities. Accordingly, mean cloudiness is higher in the north. This results in an increase in the height of the mean glacier elevation from about 2500 m ASL in the northern part of the Bernese Alps to 2900 m ASL in the south. Because of the high precipitation (locally exceeding 4000 mm per year) and their external situation, the Bernese Alps show a lower equilibrium line of the glaciers and are the mountain group showing the heaviest glacierization of the Alps, which leaves little space for periglacial phenomena (both the glacier showing the lowermost front and the largest glacier of the Alps are situated within the study site). However, this does not mean that permafrost is rare in the Bernese Alps: above 3300 m ASL, permafrost can be considered as continuous. In fact, the bedrock of many of the higher mountains in the Bernese Alps is perennially frozen.

The number of rock glaciers found in the Bernese Alps is relatively small compared with other Alpine regions. Furthermore, the objects are quite small. This can be explained with the stronger glacierization. Modelling shows that permafrost ground amounts to roughly half as much as the glacierized area (subglacial permafrost not included).

(Imhof, 1996)

The inventory has been established from the results of the interpretation of aerial photographs and field work between 1992 and 1994.

Current storage of data:

The data are not at risk of getting lost.


Imhof, M. 1994. Die Verbreitung von Permafrost in den Berner Alpen. Unpublished diploma work, 212p. (in German)

Imhof, M. 1996. Modelling and verification of the Permafrost Distribution in the Bernese Alps (Western Switzerland). Permafrost and Periglacial Processes, 7, 267-280.

King, L. 1974. Studien zur postglazialen Gletscher- und Vegetationsgeschichte des Sustenpassgebietes, Basler Beiträge zur Geografie, Heft 18, 125p. (in German)

Krummenacher, B. 1998. Periglaziale Prozesse und Formen im Furggentälti, Gemmipass. Geographica Bernensia, Bern, 245 S., sFr. 40. (in German)

Krummenacher, B., and Budmiger, K. 1992. Monitoring of periglacial phenomena in the Furggentälti (Swiss Alps). Permafrost and Periglacial Processes, 3, 149-155.

Krummenacher, B., Budmiger, K., Mihajlovic, D., and Blank, B. 1997. 8 Jahre Periglazialforschung im Furggentälti: aktuelle Werkstattberichte. Arbeitsheft Nr. 19 der VAW / ETH ZÆrich, 8-24.

Messerli, B., and Zurbuchen, M. 1968. Blockgletscher im Weissmies und Aletsch und ihre photogrammetrische Kartierung, Die Alpen, Quartalsheft 3, 1-13. (in German)

Mihajlovic, D. 1997. Ausaperungsmonitoring im Furggentälti. Unpublished diploma work. (in German)


Please cite these data as follows:

Imhof, M. 1998. Rock glaciers, Bernese Alps, western Switzerland. In: International Permafrost Association, Data and Information Working Group, comp. Circumpolar Active-Layer Permafrost System (CAPS), version 1.0. CD-ROM available from National Snow and Ice Data Center, Boulder, Colorado: NSIDC, University of Colorado at Boulder.