Recent recognition of raised mounds in the widespread discontinuous permafrost zone of the Great Slave Lowland, NWT, has prompted questions regarding their...
Lithalsas of the Great Slave Lowland, Northwest Territories, occur within fine-grained glaciolacustrine, lacustrine, and alluvial deposits. Detailed...
Permafrost in the Great Slave region, Northwest Territories is absent beneath bedrock outcrops, but occurs beneath peatlands. A three-year (2010 to 2013)...
The Great Slave Lowland of the Taiga Shield is an 11,000 km2 low-elevation granitic bedrock plain along the north shore of Great Slave Lake, Northwest...
Lithalsas are permafrost mounds formed by ice segregation in mineral-rich soil that occur within the zone of discontinuous permafrost. Nearly 1800 lithalsas...
Permafrost underlies peatlands of the Great Slave region, Northwest Territories, Canada, but permafrost relations beneath other ecotopes of black spruce (Picea...
The distribution of ice-rich terrain is an important geotechnical consideration for the engineering of northern infrastructure. Lithalsas represent one form of...
This study reports on the ground thermal regime of permafrost occurring within distinct ecological settings of the Great Slave Lowland and Upland High Boreal...
This open file reports on recent geoscience data collected and monitoring sites installed by the Geological Survey of Canada (GSC) in collaboration with...
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