Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes

Title: Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes, Author: Tony J. Wilkinson, Location: Thode The transport of solid material in the form of movements of suspended and bed load in overland flow is examined. This movement achieves considerable magnitudes in many ri...

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Bibliographic Details
Main Author: Wilkinson, Tony J.
Other Authors: Bunting, B.T., Geography
Format: Thesis
Language:English
Published: 1972
Subjects:
Online Access:http://hdl.handle.net/11375/20919
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spelling ftmcmaster:oai:macsphere.mcmaster.ca:11375/20919 2023-05-15T14:47:02+02:00 Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes Wilkinson, Tony J. Bunting, B.T. Geography 1972-05 http://hdl.handle.net/11375/20919 en eng http://hdl.handle.net/11375/20919 Thesis 1972 ftmcmaster 2022-03-22T21:14:10Z Title: Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes, Author: Tony J. Wilkinson, Location: Thode The transport of solid material in the form of movements of suspended and bed load in overland flow is examined. This movement achieves considerable magnitudes in many rills flowing across low angle slopes during the Arctic spring and summer. The occurrence of suspended load is related to the intense runoff during the spring thaw and summer rainstorms and also to the washing of fine sediments trapped in the basal ice of transverse snowpatches. These sediments which are transported from the interflow zone upslope a from small but significant sedimentery deposits on backslopes and low angle slopes. The latter deposits are more extensive and appear to be incorporated in the regolith by processes of frost action and turbulation. Thesis Master of Science (MS) Thesis Arctic MacSphere (McMaster University) Arctic Wilkinson ENVELOPE(-66.200,-66.200,-66.817,-66.817)
institution Open Polar
collection MacSphere (McMaster University)
op_collection_id ftmcmaster
language English
description Title: Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes, Author: Tony J. Wilkinson, Location: Thode The transport of solid material in the form of movements of suspended and bed load in overland flow is examined. This movement achieves considerable magnitudes in many rills flowing across low angle slopes during the Arctic spring and summer. The occurrence of suspended load is related to the intense runoff during the spring thaw and summer rainstorms and also to the washing of fine sediments trapped in the basal ice of transverse snowpatches. These sediments which are transported from the interflow zone upslope a from small but significant sedimentery deposits on backslopes and low angle slopes. The latter deposits are more extensive and appear to be incorporated in the regolith by processes of frost action and turbulation. Thesis Master of Science (MS)
author2 Bunting, B.T.
Geography
format Thesis
author Wilkinson, Tony J.
spellingShingle Wilkinson, Tony J.
Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes
author_facet Wilkinson, Tony J.
author_sort Wilkinson, Tony J.
title Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes
title_short Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes
title_full Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes
title_fullStr Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes
title_full_unstemmed Downslope Sequences of Sediment Transport and Deposition on High Arctic Slopes
title_sort downslope sequences of sediment transport and deposition on high arctic slopes
publishDate 1972
url http://hdl.handle.net/11375/20919
long_lat ENVELOPE(-66.200,-66.200,-66.817,-66.817)
geographic Arctic
Wilkinson
geographic_facet Arctic
Wilkinson
genre Arctic
genre_facet Arctic
op_relation http://hdl.handle.net/11375/20919
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