Evidence of intrapermafrost groundwater flow beneath an active rock glacier in the Swiss Alps
Temperature measurements in borehole 2/1987 through rock glacier Murtèl Corvatsch revealed a very high mean heat flow of 150 mW/m2. 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 addition,...
| Published in: | Permafrost and Periglacial Processes |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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| Online Access: | https://doi.org/10.1002/ppp.3430030216 |