Evidence of intrapermafrost groundwater flow beneath an active rock glacier in the Swiss Alps
Abstract Temperature measurements in borehole 2/1987 through rock glacier Murtèl Corvatsch revealed a very high mean heat flow of 150 mW/m 2 . Between 52 m and 56 m depth, seasonal variations are observed; above and underneath this zone temperatures have remained negative during the last 4 years. In...
Published in: | Permafrost and Periglacial Processes |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
1992
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Online Access: | http://dx.doi.org/10.1002/ppp.3430030216 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030216 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030216 |