Search this site
-
Welcome!
I work with the geoarchaeology of old stone: quarries, monuments, rock art. And I try to figure out about their weathering, and conservation using traditional crafts. I also burn lime the traditional way. Many of my domestic services are managed through FABRICA, a registered Norwegian company established with good partners. On this website I publish articles on geology and cultural heritage. I don't use AI for text or images. For the joy of old stone! Per Storemyr
Visit FABRICA’s website!

-
Recent posts
- Tafoni in Tertiary shale at 2700 m in the Swiss Alps (Brigels, Graubünden)
- Kalkbrenning i Guédelon. Kalk til bygging av ny middelalderborg i Frankrike
- Tafoni-forvitring på holmer og skjær utenfor Tvedestrand
- Nye kalkovner i Tvedestrand. Tradisjonell kalkbrenning for kulturminnevernet
- The joy of well-preserved medieval soapstone sculpture
Popular right now
Find posts by Google Maps

Follow on:

SOAPSTONE! Book on its archaeology and history!

Book: The Stones of Nidaros Cathedral

Book: QuarryScapes

Tag Archives: shale
Tafoni in Tertiary shale at 2700 m in the Swiss Alps (Brigels, Graubünden)
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 an important 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
Posted in Geomorphology, Switzerland, tafoni, Weathering history
Tagged Alpine tafoni, Brigels, marlstone, salt analysis, salt weathering, shale, Swiss Alps, Switzerland, tafoni, tafoni weathering
Leave a comment
