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  • Pingos and pingo-like forms, Banks Island, Western Canadian Arctic
  • Late Quaternary paleoceanography of the western Baffin Bay region : evidence from fossil diatoms
  • Periglacial slopewash investigations, Banks Island, Western Arctic
  • Banks Island ; Canada ; Ecoulement ; Ecoulement superficiel ; Géographie des régions polaires ; Permafrost ; Périglaciaire ; Ruissellement ; Versant ; Western Arctic ; Zone froide
  • Water circulation in not glaciated part of the north-western Sorkappland (Spitsbergen)
  • Present morphogenetic processes in a periglacial zone of Wedel-Jarlsberg Land, South-Western Spitsbergen
  • From an examination of seismic conditions and the located site of origin for the tsunami of 1969 probable borders of the tsunamigenic zone in the western Bering Sea were determined. A chart of covering the coast by tsunamis was compiled
  • the height of tsunamis in the western Bering Sea because of refraction is 0.88, i. e. three times as many as the corresponding probability for the Pacific coast of the Kuril Islands and the Kamtchatka Peninsula. - (L'Ed.).
  • Old Crow tephra: a new Late Pleistocene stratigraphic marker across north-central Alaska and western Yukon Territory
  • Radiocarbon-dated whalebones from raised beaches record a relative sea-level history for Broggerhalvoya, western Spitsbergen, that suggest a two-step deglaciation on Svalbard at the end of the late Weichselian glaciation.
  • The morphology, sediments and processes associated with the construction of a moraine along the western margin of the ice-shelf in George VI Sound, Antarctica, are discussed. A conceptual model of the moraine is developed and may help to explain
  • Summer in western Spitzbergen is caracteristic of the oceanic polar climate: temperatures most of the time are situated between 0C and 12C, frost and snow are rare, except at the beginning and the end of the season. The hostility of the climate
  • Coastal conditions and processes, Sachs Harbour, Banks Island, Western Canadian Arctic in Coastal and inland periglacial processes. Canadian Arctic.
  • The Pleistocene fauna from Canyon Creek consists of rodents (indicated by burrows), Mammuthus primigenius (woolly mammoth), Equus lambei (Yukon wild ass), Camelops hesternus (western camel), Bison sp. cf. B. crassicornis (large-horned bison), Ovis