COOKIES: By using this website you agree that we can place Google Analytics Cookies on your device for performance monitoring. |
University of Cambridge > Talks.cam > Scott Polar Research Institute - Polar Physical Sciences Seminar > CANCELLED DUE TO STRIKE ACTION Concentrated, “pulsed” axial glacier flow: structural glaciological evidence from Kvíárjökull in SE Iceland
CANCELLED DUE TO STRIKE ACTION Concentrated, “pulsed” axial glacier flow: structural glaciological evidence from Kvíárjökull in SE IcelandAdd to your list(s) Download to your calendar using vCal
If you have a question about this talk, please contact Ian Willis. THIS TALK HAS BEEN CANCELLED DUE TO STRIKE ACTION A detailed structural glaciological study carried out on Kvíárjökull in SE Iceland reveals that recent flow within this maritime glacier is concentrated within a narrow corridor located along its central axis. This active corridor is responsible for feeding ice from the accumulation zone on the south-eastern side of Öræfajökull to the lower reaches of the glacier and resulted in a c. 200 m advance during the winter of 2013-14 and the formation of a push-moraine. The corridor comprises a series of lobes linked by a laterally continuous zone of highly fractured ice characterised by prominent flow-parallel crevasses, separated by shear zones. The lobes form highly crevassed topographic highs on the glacier surface and occur immediately down-ice of marked constrictions caused by prominent bedrock outcrops located on the northern side of the glacier. Close to the frontal margin of Kvíárjökull, the southern side of the glacier is relatively smooth and pock-marked by a number of large moulins. The boundary between this slow moving ice and the active corridor is marked by a number of ice flow-parallel strike-slip faults and a prominent dextral shear zone which resulted in the clockwise rotation and dissection of an ice-cored esker exposed on the glacier surface. It is suggested that this concentrated style of glacier flow identified within Kvíárjökull has affinities with the individual flow units which operate within pulsing or surging glaciers. This talk is part of the Scott Polar Research Institute - Polar Physical Sciences Seminar series. This talk is included in these lists:
Note that ex-directory lists are not shown. |
Other listsType the title of a new list here Plant Sciences Departmental Seminars Lady Margaret LecturesOther talksCohomology of the moduli space of curves Elizabeth Bowen's Writings of the Second World War Oncological imaging: introduction and non-radionuclide techniques The Anne McLaren Lecture: CRISPR-Cas Gene Editing: Biology, Technology and Ethics The world is not flat: towards 3D cell biology and 3D devices |