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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Bibliographic Details
Main Authors: Bradwell, T., Stoker, M.S.
Other Authors: Dowdeswell, J.A.
Format: Book Part
Language:unknown
Published: Geological Society of London 2016
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/515812/
http://mem.lyellcollection.org/content/46/1/421