Geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the Athabasca River Delta, N.E. Alberta ...

Bibliography: p. 182-195. ... : The Athabasca lower delta plain and subaqueous delta plain (lower Athabasca Delta) are mainly a product of fluvial influence and a shallow receiving basin. The geomorphology of the lower Athabasca Delta reflects these conditions, and is characterized by bifurcating, l...

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Bibliographic Details
Main Author: Gorecki, Richard C.
Format: Master Thesis
Language:English
Published: University of Calgary 1990
Subjects:
Online Access:https://dx.doi.org/10.11575/prism/409
https://prism.ucalgary.ca/handle/1880/101410
id ftdatacite:10.11575/prism/409
record_format openpolar
spelling ftdatacite:10.11575/prism/409 2023-11-05T03:40:20+01:00 Geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the Athabasca River Delta, N.E. Alberta ... Gorecki, Richard C. 1990 https://dx.doi.org/10.11575/prism/409 https://prism.ucalgary.ca/handle/1880/101410 en eng University of Calgary University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Geomorphology - Alberta - Athabasca River Sedimentation and deposition - Alberta - Athabasca River Deltas - Alberta - Athabasca River article master thesis CreativeWork Other 1990 ftdatacite https://doi.org/10.11575/prism/409 2023-10-09T10:52:22Z Bibliography: p. 182-195. ... : The Athabasca lower delta plain and subaqueous delta plain (lower Athabasca Delta) are mainly a product of fluvial influence and a shallow receiving basin. The geomorphology of the lower Athabasca Delta reflects these conditions, and is characterized by bifurcating, low-sinuosity distributary channels, muddy interdistributary basins, distributary mouth bars and a gently sloping offshore profile. The major sandy bodies within the lower Athabasca Delta are the product of deposition within the distributary mouth bar, the crevasse-splay and the infilling distributary channel. Distributary mouth bars form thin (less than 4 m), lenticular bodies which tend to coalesce and produce a semi-continuous sandy sheet along the delta front. Crevasse-splays similarly form lenticular bodies of coarse material, however, they are smaller in scale than distributary mouth bars and tend not to merge laterally with each other. Distributary channel-fills tend to consist of very clean sands, and may exceed 5.5 m in thickness. They ... Master Thesis Athabasca River DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Geomorphology - Alberta - Athabasca River
Sedimentation and deposition - Alberta - Athabasca River
Deltas - Alberta - Athabasca River
spellingShingle Geomorphology - Alberta - Athabasca River
Sedimentation and deposition - Alberta - Athabasca River
Deltas - Alberta - Athabasca River
Gorecki, Richard C.
Geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the Athabasca River Delta, N.E. Alberta ...
topic_facet Geomorphology - Alberta - Athabasca River
Sedimentation and deposition - Alberta - Athabasca River
Deltas - Alberta - Athabasca River
description Bibliography: p. 182-195. ... : The Athabasca lower delta plain and subaqueous delta plain (lower Athabasca Delta) are mainly a product of fluvial influence and a shallow receiving basin. The geomorphology of the lower Athabasca Delta reflects these conditions, and is characterized by bifurcating, low-sinuosity distributary channels, muddy interdistributary basins, distributary mouth bars and a gently sloping offshore profile. The major sandy bodies within the lower Athabasca Delta are the product of deposition within the distributary mouth bar, the crevasse-splay and the infilling distributary channel. Distributary mouth bars form thin (less than 4 m), lenticular bodies which tend to coalesce and produce a semi-continuous sandy sheet along the delta front. Crevasse-splays similarly form lenticular bodies of coarse material, however, they are smaller in scale than distributary mouth bars and tend not to merge laterally with each other. Distributary channel-fills tend to consist of very clean sands, and may exceed 5.5 m in thickness. They ...
format Master Thesis
author Gorecki, Richard C.
author_facet Gorecki, Richard C.
author_sort Gorecki, Richard C.
title Geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the Athabasca River Delta, N.E. Alberta ...
title_short Geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the Athabasca River Delta, N.E. Alberta ...
title_full Geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the Athabasca River Delta, N.E. Alberta ...
title_fullStr Geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the Athabasca River Delta, N.E. Alberta ...
title_full_unstemmed Geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the Athabasca River Delta, N.E. Alberta ...
title_sort geomorphology and sedimentology of the lower delta plain and subaqueous delta plain of the athabasca river delta, n.e. alberta ...
publisher University of Calgary
publishDate 1990
url https://dx.doi.org/10.11575/prism/409
https://prism.ucalgary.ca/handle/1880/101410
genre Athabasca River
genre_facet Athabasca River
op_rights University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
op_doi https://doi.org/10.11575/prism/409
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