The Quaternary History of the Northern Cumberland Peninsula, Baffin Island, N.W.T. Part III: The Late Glacial Deposits of Sulung and Itidlirn Valleys and Adjacent Parts of the Maktak-Narpaing Trough
Four moraine systems are recognized within the area. The oldest was deposited at the margin of a major outlet glacier about 600 m a.s.1 Local corrie glaciers in the Sulung and Itidlirn Valleys show three and two moraine systems respectively, which in part have over-ridden the lateral moraine. Studie...
Published in: | Canadian Journal of Earth Sciences |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1972
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e72-030 http://www.nrcresearchpress.com/doi/pdf/10.1139/e72-030 |
_version_ | 1821860710155550720 |
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author | Dugdale, R. E. |
author_facet | Dugdale, R. E. |
author_sort | Dugdale, R. E. |
collection | Canadian Science Publishing |
container_issue | 4 |
container_start_page | 366 |
container_title | Canadian Journal of Earth Sciences |
container_volume | 9 |
description | Four moraine systems are recognized within the area. The oldest was deposited at the margin of a major outlet glacier about 600 m a.s.1 Local corrie glaciers in the Sulung and Itidlirn Valleys show three and two moraine systems respectively, which in part have over-ridden the lateral moraine. Studies of the degree of boulder weathering and the rounding of pebble edges on the four units allows cross-correlation between Itidlirn and Sulung Valleys. Weathering ratios are used to tentatively date the moraines as follows: lateral moraine of the outlet valley glacier, 43 000± years old; Phase 1 corrie moraine in Sulung Valley 35 000± years old; Phase 2 corrie moraines 23 000± years old and the youngest corrie moraines (Phase 3) 12 500± years old, as determined from weathering studies in adjacent valleys. |
format | Article in Journal/Newspaper |
genre | Baffin Island Baffin Cumberland Peninsula |
genre_facet | Baffin Island Baffin Cumberland Peninsula |
geographic | Baffin Island Cumberland Peninsula |
geographic_facet | Baffin Island Cumberland Peninsula |
id | crcansciencepubl:10.1139/e72-030 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-64.497,-64.497,66.501,66.501) |
op_collection_id | crcansciencepubl |
op_container_end_page | 374 |
op_doi | https://doi.org/10.1139/e72-030 |
op_rights | http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_source | Canadian Journal of Earth Sciences volume 9, issue 4, page 366-374 ISSN 0008-4077 1480-3313 |
publishDate | 1972 |
publisher | Canadian Science Publishing |
record_format | openpolar |
spelling | crcansciencepubl:10.1139/e72-030 2025-01-16T21:07:35+00:00 The Quaternary History of the Northern Cumberland Peninsula, Baffin Island, N.W.T. Part III: The Late Glacial Deposits of Sulung and Itidlirn Valleys and Adjacent Parts of the Maktak-Narpaing Trough Dugdale, R. E. 1972 http://dx.doi.org/10.1139/e72-030 http://www.nrcresearchpress.com/doi/pdf/10.1139/e72-030 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 9, issue 4, page 366-374 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1972 crcansciencepubl https://doi.org/10.1139/e72-030 2023-11-19T13:39:22Z Four moraine systems are recognized within the area. The oldest was deposited at the margin of a major outlet glacier about 600 m a.s.1 Local corrie glaciers in the Sulung and Itidlirn Valleys show three and two moraine systems respectively, which in part have over-ridden the lateral moraine. Studies of the degree of boulder weathering and the rounding of pebble edges on the four units allows cross-correlation between Itidlirn and Sulung Valleys. Weathering ratios are used to tentatively date the moraines as follows: lateral moraine of the outlet valley glacier, 43 000± years old; Phase 1 corrie moraine in Sulung Valley 35 000± years old; Phase 2 corrie moraines 23 000± years old and the youngest corrie moraines (Phase 3) 12 500± years old, as determined from weathering studies in adjacent valleys. Article in Journal/Newspaper Baffin Island Baffin Cumberland Peninsula Canadian Science Publishing Baffin Island Cumberland Peninsula ENVELOPE(-64.497,-64.497,66.501,66.501) Canadian Journal of Earth Sciences 9 4 366 374 |
spellingShingle | General Earth and Planetary Sciences Dugdale, R. E. The Quaternary History of the Northern Cumberland Peninsula, Baffin Island, N.W.T. Part III: The Late Glacial Deposits of Sulung and Itidlirn Valleys and Adjacent Parts of the Maktak-Narpaing Trough |
title | The Quaternary History of the Northern Cumberland Peninsula, Baffin Island, N.W.T. Part III: The Late Glacial Deposits of Sulung and Itidlirn Valleys and Adjacent Parts of the Maktak-Narpaing Trough |
title_full | The Quaternary History of the Northern Cumberland Peninsula, Baffin Island, N.W.T. Part III: The Late Glacial Deposits of Sulung and Itidlirn Valleys and Adjacent Parts of the Maktak-Narpaing Trough |
title_fullStr | The Quaternary History of the Northern Cumberland Peninsula, Baffin Island, N.W.T. Part III: The Late Glacial Deposits of Sulung and Itidlirn Valleys and Adjacent Parts of the Maktak-Narpaing Trough |
title_full_unstemmed | The Quaternary History of the Northern Cumberland Peninsula, Baffin Island, N.W.T. Part III: The Late Glacial Deposits of Sulung and Itidlirn Valleys and Adjacent Parts of the Maktak-Narpaing Trough |
title_short | The Quaternary History of the Northern Cumberland Peninsula, Baffin Island, N.W.T. Part III: The Late Glacial Deposits of Sulung and Itidlirn Valleys and Adjacent Parts of the Maktak-Narpaing Trough |
title_sort | quaternary history of the northern cumberland peninsula, baffin island, n.w.t. part iii: the late glacial deposits of sulung and itidlirn valleys and adjacent parts of the maktak-narpaing trough |
topic | General Earth and Planetary Sciences |
topic_facet | General Earth and Planetary Sciences |
url | http://dx.doi.org/10.1139/e72-030 http://www.nrcresearchpress.com/doi/pdf/10.1139/e72-030 |