scholarly journals Geological and geophysical investigations of ground ice in glaciofluvial deposits, Slave Province, District of Mackenzie, Northwest Territories

1997 ◽  
Author(s):  
S Wolfe ◽  
M Burgess ◽  
M Douma ◽  
C Hyde ◽  
S Robinson
Keyword(s):  
Northwest Territories ◽  
Ground Ice ◽  
Slave Province ◽  
Glaciofluvial Deposits ◽  
Geophysical Investigations

scholarly journals Geological and geophysical investigations of massive ground ice in glaciofluvial deposits, Slave Geological Province, Northwest Territories

1997 ◽  
Author(s):  
S A Wolfe ◽  
M M Burgess ◽  
M Douma ◽  
C Hyde ◽  
S Robinson
Keyword(s):  
Northwest Territories ◽  
Ground Ice ◽  
Glaciofluvial Deposits ◽  
Geophysical Investigations

Large-scale effects of subglacial meltwater flow in the southern Slave Province, Northwest Territories, Canada

2000 ◽  
Vol 37 (1) ◽  
pp. 81-93 ◽  
Author(s):  
V N Rampton
Keyword(s):  
Northwest Territories ◽  
High Velocity ◽  
Large Scale ◽  
High Pressures ◽  
Scale Effects ◽  
Dispersal Patterns ◽  
Slave Province ◽  
Glaciofluvial Deposits ◽  
Gravel Bars ◽  
Subglacial Meltwater

Broad corridors in the southern Slave Province of the Northwest Territories are marked by meltwater-scoured bedrock, irregular and transverse gravel ridges, gravel bars, crag and tail features (tails formed of gravel), drumlins, boulder lags, potholes, plunge pools, meltwater-sculpted slopes (in some cases defining till plateaus), and eskers. Most of the above features can either be attributed to the subglacial erosion of till by high-velocity, turbulent meltwater under high pressures and (or) meltwater transport and deposition of the eroded material. Potholes, plunge pools, and meltwater-sculpted slopes developed in unconsolidated deposits have received little attention in the literature, although they are the equivalent of similar features in bedrock that have had their origin attributed to subglacial meltwater erosion. In the case of inverted plunge pools, eroded materials, including boulders, have been transported upwards by meltwater some tens of metres during their formation. Features and deposits owing their origin to subglacial meltwater can lead to complex dispersal patterns of minerals and metals contained within both till and glaciofluvial deposits.

scholarly journals Why the Slave Province, Northwest Territories, got a little bigger

2000 ◽  
Author(s):  
W Bleeker ◽  
R Stern ◽  
K Sircombe
Keyword(s):  
Northwest Territories ◽  
Slave Province

Geology and mineral occurrences of the southern part of High Lake Greenstone Belt, Slave Province, Northwest Territories

1993 ◽  
Author(s):  
J R Henderson ◽  
M N Henderson ◽  
J A Kerswill ◽  
Z Arias ◽  
D Lemkow ◽  
...  
Keyword(s):  
Northwest Territories ◽  
Greenstone Belt ◽  
Slave Province

Till geochemistry, Slave Province, Northwest Territories and Nunavut

2005 ◽  
Author(s):  
D E Kerr ◽  
R D Knight
Keyword(s):  
Northwest Territories ◽  
Slave Province

Mineralogy of primary carbonate-bearing hypabyssal kimberlite, Lac de Gras, Slave Province, Northwest Territories, Canada

Lithos ◽  
2004 ◽  
Vol 76 (1-4) ◽  
pp. 415-433 ◽  
Author(s):  
John P. Armstrong ◽  
Mark Wilson ◽  
Robert L. Barnett ◽  
Tom Nowicki ◽  
Bruce A. Kjarsgaard
Keyword(s):  
Northwest Territories ◽  
Slave Province ◽  
Hypabyssal Kimberlite
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