Glacial sediment and landform record offshore NW Scotland: a fjord-shelf-slope transect through a Late Quaternary mid-latitude ice-stream system
Current estimates of ice-mass loss from ice sheets vary, but there is consensus that the rate of loss has increased over the last two decades from c. 100 to c. 400 Gt a−1 with the great majority occurring within ice-stream systems (e.g. Shepherd et al. 2012; Hanna et al. 2013). Where ice streams ter...
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Format: | Book Part |
Language: | unknown |
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Geological Society of London
2016
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Online Access: | http://nora.nerc.ac.uk/id/eprint/515812/ http://mem.lyellcollection.org/content/46/1/421 |