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...

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Published in:The Canadian Geographer/Le Géographe canadien
Main Author: Fraser, J.K.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1956
Subjects:
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
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spelling 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
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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
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container_issue 7
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