Les formes de glaces des grottes de la Nahanni, Territoires du Nord-Ouest, Canada
Exploration has been continuing on the karst system developed within the cliffs of the First Canyon (300–1050 m deep) of the South Nahanni River(61°18′ N, 124°10′ W). Probably the most northerly on the North American continent, this karst region is within the discontinuous permafrost zone, at the so...
| Published in: | Canadian Journal of Earth Sciences |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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Canadian Science Publishing
1977
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| Online Access: | http://dx.doi.org/10.1139/e77-108 http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-108 |
| Summary: | Exploration has been continuing on the karst system developed within the cliffs of the First Canyon (300–1050 m deep) of the South Nahanni River(61°18′ N, 124°10′ W). Probably the most northerly on the North American continent, this karst region is within the discontinuous permafrost zone, at the southern limit of the tundra. The caves contain ice of the type which depends on the present subarctic climate (two-dimensional hexagonal ice crystals, ice like calcite speleothem and 'secondary' ice), or on a long-term climatic change of ± 2400 years (massive ice deposits and sponge-like ice deposits). |
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