Add to ORKGTwo excellent examples of sediments deformed by glacier ice occur on Nicholson Peninsula, Mackenzie District (Liverpool Bay, 69 54 N, 129 W). Sediments, topography and structure of the Peninsula are described. Altitudes in the hilly northern half attain 200-300 ft. above sea level, whereas those in the south rarely exceed 30 ft. The hills were formed either by glacier ice moved against a topographic obstruction, resulting in a large push moraine, or by the drag effect of ice moving over weak strata. Deformation could have occurred during the last ice advance or earlier, probably in a single period of deformation, but whether the ground was frozen at the time is not evident
On the stagnant ice of Wolf Creek Glacier, in the Canadian Yukon, fully 90 per cent of the superglac...
The northern terminus of Emerald Glacier (51ﾟ31'N, 116ﾟ32'W) in the Yoho Valley, British Columbia wa...
Glacially deformed permafrost at North Head, in the Tuktoyaktuk Coastlands of western Arctic Canada,...
This thesis investigates the geomorphology of retrogressive thaw slumps and active layer slides on H...
The 150-km.-long stretch of the coast between Herschel Island and the Mackenzie Delta terminates in ...
Four measured sections of unconsolidated Pleistocene strata exposed on the Yukon coast between Shing...
The upper 5-20 m of ice-rich permafrost at three sites overridden by the northwest margin of the Lau...
The upper 5–20 m of ice-rich permafrost at three sites overridden by the northwest margin of the Lau...
Wollaston Peninsula and most of southern Victoria Island comprise Palaeozoic carbonate lowlands, sca...
The upper 5^20mof ice-rich permafrost at three sites overridden by the northwest margin of the Laure...
In this paper the development of a large-scale gravitational deformation involving the eastern later...
Maps and describes features indicating marine transgression and ice movement in the area approx. 64-...
Detailed investigations of the sediment-landform associations being actively created in modern-day p...
Glacier surges are characterized by order-of-magnitude increases in flow that can be sustained for m...
Tidal flats are widely distributed on high-latitude coasts, where sea ice processes have been invoke...
On the stagnant ice of Wolf Creek Glacier, in the Canadian Yukon, fully 90 per cent of the superglac...
The northern terminus of Emerald Glacier (51ﾟ31'N, 116ﾟ32'W) in the Yoho Valley, British Columbia wa...
Glacially deformed permafrost at North Head, in the Tuktoyaktuk Coastlands of western Arctic Canada,...
This thesis investigates the geomorphology of retrogressive thaw slumps and active layer slides on H...
The 150-km.-long stretch of the coast between Herschel Island and the Mackenzie Delta terminates in ...
Four measured sections of unconsolidated Pleistocene strata exposed on the Yukon coast between Shing...
The upper 5-20 m of ice-rich permafrost at three sites overridden by the northwest margin of the Lau...
The upper 5–20 m of ice-rich permafrost at three sites overridden by the northwest margin of the Lau...
Wollaston Peninsula and most of southern Victoria Island comprise Palaeozoic carbonate lowlands, sca...
The upper 5^20mof ice-rich permafrost at three sites overridden by the northwest margin of the Laure...
In this paper the development of a large-scale gravitational deformation involving the eastern later...
Maps and describes features indicating marine transgression and ice movement in the area approx. 64-...
Detailed investigations of the sediment-landform associations being actively created in modern-day p...
Glacier surges are characterized by order-of-magnitude increases in flow that can be sustained for m...
Tidal flats are widely distributed on high-latitude coasts, where sea ice processes have been invoke...
On the stagnant ice of Wolf Creek Glacier, in the Canadian Yukon, fully 90 per cent of the superglac...
The northern terminus of Emerald Glacier (51ﾟ31'N, 116ﾟ32'W) in the Yoho Valley, British Columbia wa...
Glacially deformed permafrost at North Head, in the Tuktoyaktuk Coastlands of western Arctic Canada,...