Using Geochemical Evidence to Determine Provenance in a High Arctic Glacier-Fed Lake, Linné Valley, Svalbard, Norway, 2005
In the Linné Valley of western Spitsbergen, the Linné glacier (Linnébreen) advanced and retreated throughout the Holocene. Sediment from Linnébreen is deposited into Lake Linné, located 5 km downvalley. Sediment provenance in Linnédalen is being studied as part of the NSF-funded Svalbard REU Project...
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Arctic Data Center
2013
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Online Access: | https://doi.org/10.18739/A2P843V60 |