scholarly journals Report of activities on the structural geology of southern Peel Plateau and Peel Plain region, Northwest Territories and Yukon

2007 ◽  
Author(s):  
Y Lemieux ◽  
L P Gal ◽  
L J Pyle ◽  
T Hadlari ◽  
W Zantvoort
Keyword(s):  
Structural Geology ◽  
Northwest Territories ◽  
Plain Region ◽  
Peel Plateau

scholarly journals 2005 reconnaissance field program in Peel Plateau and Peel Plain region, Northwest Territories and Yukon Territory

2006 ◽  
Author(s):  
L J Pyle ◽  
A L Jones ◽  
L P Gal ◽  
J G Abbott ◽  
A D McCracken ◽  
...  
Keyword(s):  
Northwest Territories ◽  
Yukon Territory ◽  
Plain Region ◽  
Peel Plateau

Field-based stratigraphic studies in the Peel Plateau, Peel Plain, and adjacent areas, Northwest Territories and Yukon

2007 ◽  
Author(s):  
L J Pyle ◽  
T L Allen ◽  
T A Fraser ◽  
L P Gal ◽  
T Hadlari ◽  
...  
Keyword(s):  
Northwest Territories ◽  
Peel Plateau

scholarly journals Impacts of variations in snow cover on permafrost stability, including simulated snow management, Dempster Highway, Peel Plateau, Northwest Territories

2017 ◽  
Vol 3 (2) ◽  
pp. 150-178 ◽  
Author(s):  
H. Brendan O’Neill ◽  
Chris R. Burn
Keyword(s):  
Snow Cover ◽  
Northwest Territories ◽  
Snow Accumulation ◽  
Active Management ◽  
Permafrost Degradation ◽  
The Road ◽  
Ground Temperatures ◽  
Permafrost Table ◽  
Thaw Depth ◽  
Peel Plateau

Permafrost conditions were examined near the Dempster Highway embankment on Peel Plateau, Northwest Territories. Ground temperatures were recorded in 2013–2015 at five sites at the embankment toe and at two sites in undisturbed (control) tundra. Annual mean ground temperatures at approximately 5 m depth ranged from −2.2 to 0.0 °C at the embankment toe and were −1.8 and −2.6 °C at control sites. Permafrost is degrading beside the road at four of five sites. Thaw depths are greater at the embankment toe, where deep snow accumulates, than in undisturbed tundra. A numerical model was used to examine the influence of varying snow cover properties on the ground thermal regime. Simulations indicated that delaying the onset of deep (1 m) snow accumulation and (or) prolonging the duration of the same total accumulation accelerates removal of latent heat from the active layer, increases sensible ground cooling, and results in reduced thaw depth. Furthermore, reducing snow depth and increasing snow density may rapidly raise the permafrost table, lower ground temperatures at the embankment toe, and cool permafrost at depth over several years. In consequence, mechanical snow removal and (or) compaction should be investigated as an active management strategy for mitigating permafrost degradation in ice-rich settings.

Albian to Turonian stratigraphy and palaeoenvironmental history of the northern Western Interior Sea in the Peel Plateau Region, Northwest Territories, Canada

2011 ◽  
Vol 302 (3-4) ◽  
pp. 270-300 ◽  
Author(s):  
Danielle Thomson ◽  
Claudia J. Schröder-Adams ◽  
Thomas Hadlari ◽  
George Dix ◽  
William J. Davis
Keyword(s):  
Northwest Territories ◽  
Plateau Region ◽  
History Of ◽  
Peel Plateau
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