
Tafoni in shales at 2700 m. Muttenbergen in Brigels, eastern Switzerland. Photo by PS
To my knowledge, tafoni weathering has hardly been described in rocks at high altitudes in the Swiss Alps. But last summer I came across fine examples in a series of young, slightly metamorphic shales and marlstones of Tertiary age at altitudes of about 2700 m in Brigels, which is in the eastern canton of Graubünden. This summer I set out to investigate more closely. To my joy, tafoni could be observed “everywhere” connected to very exposed peaks and promontories, constituting a significant part of the breaking-up of the rocks. Importantly, in the dry summer, salt efflorescence could also be observed “everywhere” related to tafoni formation. Here’s a brief report. Continue reading














