Open Session - SWISS GEOSCIENCE MEETINGs

REFERENCES
Delaloye, R., & Lambiel C. 2007: Drilling in a low elevation cold talus slope (Dreveneuse, Swiss Prealps). Geophysical
Research Abstracts 9: 10907.
Morard, S., Delaloye, R. & Dorthe J. 2008: Seasonal thermal regime of a mid-latitude ventilated debris accumulation.
Proceedings of the Ninth International Conference on Permafrost, July 2008, Fairbanks, Alaska, 1233-1238.
Ohata, T., Furukawa, T. & Higuchi K. 1994: Glacioclimatological study of perennial ice in the Fuji ice cave, Japan, Part 1,
Seasonal variation and mechanism of maintenance. Arctic and Alpine Research, vol. 26, 3. 227-237.
6.1
Inventory of geomorphosites of Bavona and Rovana valleys (Ticino)
Pagano Luca
6670 Avegno, luca.pagano@gmail.com
During the last decade, research on geomorphological heritage has improved due to the development of geotourism and
geoparks and to the activity of the Working group on Geomorphosites of the International Association of Geomorphologists.
Several methods (see Reynard and Coratza, 2007) were developed for assessing the quality of geomorphosites – that is landforms
to which a value can be given due to human perception and/or utilization (Panizza, 2001). The aim is to reduce subjectivity
and to facilitate the selection of the most representative sites, worth to be protected and/or promoted.
Inspired by several approaches developed during the last decade, Reynard et al. (2007) developed at the Institute of Geography
of Lausanne University an assessment method of geomorphosites. The method allows assessing the scientific, ecological,
aesthetic, cultural and economic values of geomorphosites and to note more descriptive data in order to set up a site inventory.
The assessment is divided in two categories of criteria: the central (scientific value) and additional (ecological, economic,
aesthetic and cultural) values.
The assessment method was applied on two alpine valleys in the Southern Swiss Alps. More precisely, we focused on the selection
and the assessment of Bavona and Rovana valleys’ geomorphosites (Maggia Valley, Ticino). 28 landforms with a scientific
central value were identified and studied. Results show that Calnegia hanging valley obtains the most important score
and is just followed by the Basòdino Glacier, a small ice cap glacier. One site, the fossil proglacial margin of the Basòdino
Glacier W, represents an incredible geodiversity due to the glacio-karstic origin of Pian del Ghiacciaios polje.
After the inventory stage, we noted that, on the ground, geomorphology is not much known in comparison with the high
value of some geomorphosites. Thus, in order to acknowledge them by the general public, we offered some perspectives with
the intention of promoting the geomorphological heritage of the region. Firstly, the definition of categories of protection
would contribute to preserve the vulnerable geomorphosites towards human impacts. Secondly, we underline the value of
some interesting sites of the inventory with the idea of promoting a sustainable tourist development. Geodiversity is indeed
poorly taken into account for the (geo)tourist development of the region.
REFERENCES:
Pagano, L. 2008: Inventaire des géotopes géomorphologiques du Val Bavona et du Val Rovana. Sélection, evaluation et
perspectives. Mémoire de Licence. Université de Lausanne.
Panizza, M. 2001: Geomorphosites, concepts, methods and examples of geomorphological survey. Chinese science bulletin
46, Suppl. Vol., 4-6.
Reynard, E. & Coratza, P. 2007: Geomorphosites and geodiversity: a new domain of research. Geographica Helvetica 62, 3:
138-139.
Reynard, E. Fontana, G. Kozlic, L. Scapozza, C 2007: A method for assessing « scientific » and « additional values » of
geomorphosites. Geographica Helvetica, 62, 3: 148-158.
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Symposium 6: Apply! Snow, ice and Permafrost Science + Geomorphology