Controls upon the location and size of glacial overdeepenings: PhD thesis
Controls upon the location and size of glacial overdeepenings: PhD thesis
Overdeepening is an important glaciological and geomorphological process that has the potential to influence the response of ice masses to climatic changes. We have examined several hundred glacial overdeepenings proximal to/ within Labrador, Canada, to investigate the controls upon overdeepening location and size. Our analyses show that overdeepening appears to correlate strongly with glacial confluence and, importantly, the correlation is strongest where confluence-geometry indicates the speed up of ice-flow. Further, we find that the magnitude of ice-flow speed up correlates with overdeepening depth only for confluences situated in or near major geological fault-zones. Our findings therefore support the hypothesis that overdeepening can be initiated by an increase in ice velocity. Further, we conclude that overdeepening is most efficacious where fractured bedrock enables efficient quarrying.
Lloyd, Christopher T.
de6d850d-fba9-4f7e-9340-8ba750bfd9a6
April 2015
Lloyd, Christopher T.
de6d850d-fba9-4f7e-9340-8ba750bfd9a6
Clark, Christopher
e3001c57-1ecc-4ff9-b144-55a785245303
Swift, Darrel
ac4590ea-3b0c-4265-a813-29f899899757
Lloyd, Christopher T.
(2015)
Controls upon the location and size of glacial overdeepenings: PhD thesis.
The University of Sheffield, Doctoral Thesis.
Record type:
Thesis
(Doctoral)
Abstract
Overdeepening is an important glaciological and geomorphological process that has the potential to influence the response of ice masses to climatic changes. We have examined several hundred glacial overdeepenings proximal to/ within Labrador, Canada, to investigate the controls upon overdeepening location and size. Our analyses show that overdeepening appears to correlate strongly with glacial confluence and, importantly, the correlation is strongest where confluence-geometry indicates the speed up of ice-flow. Further, we find that the magnitude of ice-flow speed up correlates with overdeepening depth only for confluences situated in or near major geological fault-zones. Our findings therefore support the hypothesis that overdeepening can be initiated by an increase in ice velocity. Further, we conclude that overdeepening is most efficacious where fractured bedrock enables efficient quarrying.
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Published date: April 2015
Identifiers
Local EPrints ID: 468415
URI: http://eprints.soton.ac.uk/id/eprint/468415
PURE UUID: 3ee75cb8-de37-4dee-a28b-2d8a885525d0
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Date deposited: 12 Aug 2022 21:39
Last modified: 17 Mar 2024 03:38
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Contributors
Thesis advisor:
Christopher Clark
Thesis advisor:
Darrel Swift
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