Discovery of thermal springs in the Raudfjellet region, SW Spitsbergen
Abstract
Two thermal springs were discovered in the Raudfjellet region in Spitsbergen. They had a total discharge of about 0.1 m3/sec and were found in metamorphic carbonate rocks on bare ground under the eastern part of Torellbreen. Water with temperatures between 12.3 and 6.5°C caused thermoerosive phenomena to take place at the end of the eastern Torellbreen snout and formed an ice sheet covering the ground after cooling and freezing.Downloads
Authors contributing to Polar Research retain copyright of their work, with first publication rights granted to the Norwegian Polar Institute. Read the journal's full Copyright- and Licensing Policy.