Origin and polycyclic behaviour of tundra thaw slumps, Mackenzie Delta region, Northwest Territories, Canada

Author:

Kokelj S. V.,Lantz T. C.,Kanigan J.,Smith S. L.,Coutts R.

Publisher

Wiley

Subject

Earth-Surface Processes

Reference41 articles.

1. Aylsworth JA, Burgess MM, Desrochers DT, Duk- Rodkin A, Traynor JA. 2000. Surficial geology, subsurface materials, and thaw sensitivity of sediments In The Physical Environment of the Mackenzie Valley: A Baseline for the Assessment of Environmental Change, Dyke LD, Brooks GR (eds). Geological Survey of Canada, Bulletin 547: 41-48.

2. Burgess MM, Smith SL. 2000. Shallow ground temperatures In The Physical Environment of the Mackenzie Valley, Northwest Territories: A Baseline for the Assessment of Environmental Change, Dyke LD, Brooks GR (eds). Geological Survey of Canada, Bulletin 547: 89-104.

3. Cryostratigraphy, paleogeography, and climate change during the early Holocene warm interval, western Arctic coast, Canada;Burn;Canadian Journal of Earth Sciences,1997

4. The thermal regime of a retrogressive thaw slump near Mayo, Yukon Territory;Burn;Canadian Journal of Earth Sciences,2000

5. Tundra lakes and permafrost, Richards Island, western Arctic coast, Canada;Burn;Canadian Journal of Earth Sciences,2002

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