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dc.contributor.author Bryn en_US
dc.contributor.author Neil F. en_US
dc.contributor.author Michael J. en_US
dc.contributor.author James L. en_US
dc.date.accessioned 2008-12-11T16:14:41Z
dc.date.available 2008-12-11T16:14:41Z
dc.date.issued 2004-03-01 en_US
dc.identifier http://dx.doi.org/10.3189/172756504781830114 en_US
dc.identifier.citation Hubbard , B , Glasser , N F , Hambrey , M J & Etienne , J L 2004 , ' A sedimentological and isotopic study of the origin of supraglacial debris bands: Kongsfjorden, Svalbard ' Journal of Glaciology , vol 50 , no. 169 , pp. 157-170 . , 10.3189/172756504781830114 en_US
dc.identifier.other PURE: 94535 en_US
dc.identifier.other dspace: 2160/1557 en_US
dc.identifier.uri http://hdl.handle.net/2160/1557
dc.description.abstract Debris bands associated with supraglacial moraines and associated basal deposits have been logged and sampled for their ice and debris at three glaciers in north-west Spitsbergen, Svalbard. Physical properties, including sediment concentrations, sediment particle-size distributions, clast macro-fabrics, and oxygen isotope compositions, indicate that all transverse and some longitudinal debris bands originate from the basal zone of these glaciers. Transverse supraglacial bands are composed of extensive stratified-facies basal ice that is enriched in 18O and which contains polymodal debris with spatially consistent clast fabrics. These properties suggest initial formation as basal ice and subsequent elevation into an englacial position by thrusting rather than formation as crevasse fills. The formation of longitudinal debris bands results from laterally compressive folding in response to the convergence of multiple flow units into a narrow glacier tongue. In common with transverse debris bands, longitudinal bands appear to be composed of stratified basal ice. The bands exposed at the surface of austre Brøggerbreen comprise two subfacies, strongly suggesting that the glacier was at least partially warm-based in the past, when the basal ice formed. en_US
dc.format.extent 14 en_US
dc.relation.ispartof Journal of Glaciology en_US
dc.title A sedimentological and isotopic study of the origin of supraglacial debris bands: Kongsfjorden, Svalbard en_US
dc.contributor.pbl Institute of Geography & Earth Sciences en_US
dc.contributor.pbl Centre for Glaciology en_US


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