PHYSIOGRAPHIC NOTES ON FEATURES IN THE MACKENZIE DELTA AREA
ABSTRACT Evidence is presented to show that a group of knobby hills on coalescing alluvial fans along the Richardson Mountains is landslide debris rather than glacial deposit, Associated with the debris are pingo‐like features and lenses of ground ice. A heavy layer of silt over remnant snowbanks is...
Published in: | The Canadian Geographer/Le Géographe canadien |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
1956
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Online Access: | http://dx.doi.org/10.1111/j.1541-0064.1956.tb01851.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1956.tb01851.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1956.tb01851.x |
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crwiley:10.1111/j.1541-0064.1956.tb01851.x 2024-06-02T08:10:13+00:00 PHYSIOGRAPHIC NOTES ON FEATURES IN THE MACKENZIE DELTA AREA Fraser, J.K. 1956 http://dx.doi.org/10.1111/j.1541-0064.1956.tb01851.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1956.tb01851.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1956.tb01851.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Canadian Geographies / Géographies canadiennes volume 2, issue 7, page 20-20 ISSN 0008-3658 1541-0064 journal-article 1956 crwiley https://doi.org/10.1111/j.1541-0064.1956.tb01851.x 2024-05-03T11:21:46Z ABSTRACT Evidence is presented to show that a group of knobby hills on coalescing alluvial fans along the Richardson Mountains is landslide debris rather than glacial deposit, Associated with the debris are pingo‐like features and lenses of ground ice. A heavy layer of silt over remnant snowbanks is attributed to wind deposition. Article in Journal/Newspaper Mackenzie Delta Wiley Online Library Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) Richardson Mountains ENVELOPE(-136.171,-136.171,67.000,67.000) The Canadian Geographer/Le Géographe canadien 2 7 20 20 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
ABSTRACT Evidence is presented to show that a group of knobby hills on coalescing alluvial fans along the Richardson Mountains is landslide debris rather than glacial deposit, Associated with the debris are pingo‐like features and lenses of ground ice. A heavy layer of silt over remnant snowbanks is attributed to wind deposition. |
format |
Article in Journal/Newspaper |
author |
Fraser, J.K. |
spellingShingle |
Fraser, J.K. PHYSIOGRAPHIC NOTES ON FEATURES IN THE MACKENZIE DELTA AREA |
author_facet |
Fraser, J.K. |
author_sort |
Fraser, J.K. |
title |
PHYSIOGRAPHIC NOTES ON FEATURES IN THE MACKENZIE DELTA AREA |
title_short |
PHYSIOGRAPHIC NOTES ON FEATURES IN THE MACKENZIE DELTA AREA |
title_full |
PHYSIOGRAPHIC NOTES ON FEATURES IN THE MACKENZIE DELTA AREA |
title_fullStr |
PHYSIOGRAPHIC NOTES ON FEATURES IN THE MACKENZIE DELTA AREA |
title_full_unstemmed |
PHYSIOGRAPHIC NOTES ON FEATURES IN THE MACKENZIE DELTA AREA |
title_sort |
physiographic notes on features in the mackenzie delta area |
publisher |
Wiley |
publishDate |
1956 |
url |
http://dx.doi.org/10.1111/j.1541-0064.1956.tb01851.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1956.tb01851.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1956.tb01851.x |
long_lat |
ENVELOPE(-136.672,-136.672,68.833,68.833) ENVELOPE(-136.171,-136.171,67.000,67.000) |
geographic |
Mackenzie Delta Richardson Mountains |
geographic_facet |
Mackenzie Delta Richardson Mountains |
genre |
Mackenzie Delta |
genre_facet |
Mackenzie Delta |
op_source |
Canadian Geographies / Géographies canadiennes volume 2, issue 7, page 20-20 ISSN 0008-3658 1541-0064 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1541-0064.1956.tb01851.x |
container_title |
The Canadian Geographer/Le Géographe canadien |
container_volume |
2 |
container_issue |
7 |
container_start_page |
20 |
op_container_end_page |
20 |
_version_ |
1800756051377651712 |