Quaternary environmental change in the Stikine Plateau region, northwestern British Columbia, Canada ...
Bibliography: p. 289-313. ... : Records of Quaternary environmental change have been resolved on the Stikine Plateau of northwestern British Columbia. Glacial sediment has been preserved between Early Pleistocene basalt flows on Mt. Edziza and underneath Middle Pleistocene basalt flows in the Stikin...
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ftdatacite:10.11575/prism/15661 2023-11-05T03:45:16+01:00 Quaternary environmental change in the Stikine Plateau region, northwestern British Columbia, Canada ... Spooner, Ian Stewart 1994 https://dx.doi.org/10.11575/prism/15661 https://prism.ucalgary.ca/handle/1880/30361 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. QE 696 S726 1994a Additional Copy QE 696 S726 1994 Geology, Stratigraphic - Quaternary Geology - British Columbia - Stikine River region article doctoral thesis CreativeWork Other 1994 ftdatacite https://doi.org/10.11575/prism/15661 2023-10-09T10:53:43Z Bibliography: p. 289-313. ... : Records of Quaternary environmental change have been resolved on the Stikine Plateau of northwestern British Columbia. Glacial sediment has been preserved between Early Pleistocene basalt flows on Mt. Edziza and underneath Middle Pleistocene basalt flows in the Stikine River valley. The Mt. Edziza record indicates that regional ice advanced from the southwest and west of Mt. Edziza and inundated the plateau. Radiometric and paleomagnetic dating indicates sediment deposition occurred during isotope stages 24 to 26. Paleomagnetic sampling resulted in the resolution of the Jaramillo normal polarity event within the section. The Stikine River valley section indicates that river blockage and glaciolacustrine sediment deposition occurred at about 330 ± 30 ka (isotope stage 10). The blockage was a result of early ice advance in the Coast Mountains and eventual regional ice cover is indicated by till overlying the glaciolacustrine sediment. Advance-phase glaciolacustrine sediment deposited in the Stikine River ... Article in Journal/Newspaper Stikine River DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
QE 696 S726 1994a Additional Copy QE 696 S726 1994 Geology, Stratigraphic - Quaternary Geology - British Columbia - Stikine River region |
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QE 696 S726 1994a Additional Copy QE 696 S726 1994 Geology, Stratigraphic - Quaternary Geology - British Columbia - Stikine River region Spooner, Ian Stewart Quaternary environmental change in the Stikine Plateau region, northwestern British Columbia, Canada ... |
topic_facet |
QE 696 S726 1994a Additional Copy QE 696 S726 1994 Geology, Stratigraphic - Quaternary Geology - British Columbia - Stikine River region |
description |
Bibliography: p. 289-313. ... : Records of Quaternary environmental change have been resolved on the Stikine Plateau of northwestern British Columbia. Glacial sediment has been preserved between Early Pleistocene basalt flows on Mt. Edziza and underneath Middle Pleistocene basalt flows in the Stikine River valley. The Mt. Edziza record indicates that regional ice advanced from the southwest and west of Mt. Edziza and inundated the plateau. Radiometric and paleomagnetic dating indicates sediment deposition occurred during isotope stages 24 to 26. Paleomagnetic sampling resulted in the resolution of the Jaramillo normal polarity event within the section. The Stikine River valley section indicates that river blockage and glaciolacustrine sediment deposition occurred at about 330 ± 30 ka (isotope stage 10). The blockage was a result of early ice advance in the Coast Mountains and eventual regional ice cover is indicated by till overlying the glaciolacustrine sediment. Advance-phase glaciolacustrine sediment deposited in the Stikine River ... |
format |
Article in Journal/Newspaper |
author |
Spooner, Ian Stewart |
author_facet |
Spooner, Ian Stewart |
author_sort |
Spooner, Ian Stewart |
title |
Quaternary environmental change in the Stikine Plateau region, northwestern British Columbia, Canada ... |
title_short |
Quaternary environmental change in the Stikine Plateau region, northwestern British Columbia, Canada ... |
title_full |
Quaternary environmental change in the Stikine Plateau region, northwestern British Columbia, Canada ... |
title_fullStr |
Quaternary environmental change in the Stikine Plateau region, northwestern British Columbia, Canada ... |
title_full_unstemmed |
Quaternary environmental change in the Stikine Plateau region, northwestern British Columbia, Canada ... |
title_sort |
quaternary environmental change in the stikine plateau region, northwestern british columbia, canada ... |
publisher |
University of Calgary |
publishDate |
1994 |
url |
https://dx.doi.org/10.11575/prism/15661 https://prism.ucalgary.ca/handle/1880/30361 |
genre |
Stikine River |
genre_facet |
Stikine 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/15661 |
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1781707078913490944 |