Four measured sections of unconsolidated Pleistocene strata exposed on the Yukon coast between Shingle Point and Herschel Island are described. The sediments have suffered ice thrust deformation and are unconformably overlain by fluvio-glacial retreatal gravels. The results of palynological examination, study of mollusca and a new 14C determination are discussed. Deformation of the coastal strata probably occurred between 37 900 and 9510 years ago
Ice-rich glaciolacustrine sediments near Mayo, Yukon Territory, reveal a thaw unconformity in the fo...
A thermokarst lake sediment core from the centre of Herschel Island was analysed in order to reconst...
This thesis investigates the geomorphology of retrogressive thaw slumps and active layer slides on H...
Reports geological investigations is 1956-1957 to aid in dating the archeological finds. Quaternary ...
The 150-km.-long stretch of the coast between Herschel Island and the Mackenzie Delta terminates in ...
Quaternary glacial and non-glacial sediment exposed at White River and Silver Creek provide a record...
Sedimentary deposits from two Middle to Late Pleistocene glaciations and intervening non-glacial int...
New stratigraphic and chronometric data show that Bonnet Plume Basin, in northeastern Yukon Territor...
Northern Yukon cliff-top eolian deposits are indicators of past climates and environments. The depos...
In spring 2009, a 730 cm sediment core was recovered from the largest lake on Herschel Island (Yukon...
ABSTRACT. New stratigraphic and chronometric data show that Bonnet Plume Basin, in northeastern Yuko...
Two late Pleistocene limits of glaciation were delineated in the Snag-Klutlan area. Radiocarbon date...
At least five Middle to Late Pleistocene advances of the northern Cordilleran Ice Sheet are preserve...
Terrestrial permafrost archives along the Yukon Coastal Plain (northwest Canada) have recorded lands...
Two excellent examples of sediments deformed by glacier ice occur on Nicholson Peninsula, Mackenzie ...
Ice-rich glaciolacustrine sediments near Mayo, Yukon Territory, reveal a thaw unconformity in the fo...
A thermokarst lake sediment core from the centre of Herschel Island was analysed in order to reconst...
This thesis investigates the geomorphology of retrogressive thaw slumps and active layer slides on H...
Reports geological investigations is 1956-1957 to aid in dating the archeological finds. Quaternary ...
The 150-km.-long stretch of the coast between Herschel Island and the Mackenzie Delta terminates in ...
Quaternary glacial and non-glacial sediment exposed at White River and Silver Creek provide a record...
Sedimentary deposits from two Middle to Late Pleistocene glaciations and intervening non-glacial int...
New stratigraphic and chronometric data show that Bonnet Plume Basin, in northeastern Yukon Territor...
Northern Yukon cliff-top eolian deposits are indicators of past climates and environments. The depos...
In spring 2009, a 730 cm sediment core was recovered from the largest lake on Herschel Island (Yukon...
ABSTRACT. New stratigraphic and chronometric data show that Bonnet Plume Basin, in northeastern Yuko...
Two late Pleistocene limits of glaciation were delineated in the Snag-Klutlan area. Radiocarbon date...
At least five Middle to Late Pleistocene advances of the northern Cordilleran Ice Sheet are preserve...
Terrestrial permafrost archives along the Yukon Coastal Plain (northwest Canada) have recorded lands...
Two excellent examples of sediments deformed by glacier ice occur on Nicholson Peninsula, Mackenzie ...
Ice-rich glaciolacustrine sediments near Mayo, Yukon Territory, reveal a thaw unconformity in the fo...
A thermokarst lake sediment core from the centre of Herschel Island was analysed in order to reconst...
This thesis investigates the geomorphology of retrogressive thaw slumps and active layer slides on H...