Ice-Marginal and Proglacial Fluvial Characteristics of A High-Arctic Glacier, Linnébreen, Svalbard, 2013
Linnébreen, a 2 km2 high-arctic primarily cold-based polythermal glacier in a valley of Carboniferous sedimentary rocks and Proterozoic phyllite and schist in southwest Spitsbergen, has retreated approximately 208 m since 2004, and 1.5 km from its Little Ice Age maximum (LIAM) at around 1936. Drift...
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Format: | Dataset |
Language: | unknown |
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Arctic Data Center
2013
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Online Access: | https://doi.org/10.18739/A24B2X431 |