Physiographic Notes on Features in the Mackenzie Delta Area
Bibliographic Data
| ID | 8424147 |
|---|---|
| Authors | J K Fraser (corresponding author) |
| Year | 1956 |
| Volume | 2 |
| Issue | 7 |
| Pages | 20-20 |
| Publication date | 1956-01-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Canadian Geographies / Géographies canadiennes (JOURNAL) |
| Journal identifiers | ISSN: 0008-3658 • E-ISSN: 1541-0064 |
| Publisher | Wiley (PUBLISHER • GB) |
| DOI | 10.1111/j.1541-0064.1956.tb01851.x |
| OpenAlex | W4234328390 |
| Language | EN |
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
Alluvial fan · Alluvium · Debris · Delta · Deposition (geology) · Geography · Geomorphology · Glacial period · Landslide · Physical geography · River delta · Sediment · Silt · Aeolian processes and effects · Geology · Geology and Paleoclimatology Research · Landslides and related hazards · Oceanography
| Highly cited | No |
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