The glacial geomorphology of the Mackenzie Mountains region, Canada
ABSTRACTDuring the Last Glacial Maximum, the Mackenzie Mountains region was glaciated by three distinct ice sources; the Laurentide Ice Sheet, the Cordilleran Ice Sheet, and independent montane glaciers. Rapid ice sheet thinning of the Laurentide-Cordilleran ice saddle in the south of this region co...
Furkejuvvon:
| Váldodahkkit: | , , |
|---|---|
| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Taylor & Francis Group
2023-12-01
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| Ráidu: | Journal of Maps |
| Fáttát: | |
| Liŋkkat: | https://www.tandfonline.com/doi/10.1080/17445647.2023.2203333 |
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