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  • Physical controls and resulting morphological forms of Quaternary ice-contact volcanoes in western Canada
  • British Columbia ; Canada ; Cold area ; Ice ; Magma ; Meltwater ; Quaternary ; Typology ; Volcanic rock ; Volcanism
  • Volcanism in association with large quantities of ice manifests itself in a variety of morphological forms developed under differing physical conditions. These physical conditions include the location amount, thickness, and type of confining ice
  • provides a review of ice-contact volcanism and volcanic products formed in these environments using Canadian examples for illustration.
  • The Little Ice Age in the Canadian Rockies
  • Canada ; Climatic variation ; Concept ; Dendrochronology ; Glacier fluctuation ; Glaciolacustrine ; Lichenometry ; Little ice age ; Moraine ; Palaeo-environment ; Rocky Mountains
  • This paper reviews the evidence and history of glacier fluctuations during the Little Ice Age (LIA) in the Canadian Rockies. Episodes of synchronous glacier advance occurred in the 12th-13th, early 18th and throughout the 19th centuries. The glacier
  • Canada ; Cenozoic ; Esker ; Geomorphology ; Glacial isostasy ; Lateglacial ; Little ice age ; Periglacial features ; Permafrost ; Postglacial ; Quaternary ; Slope ; Soil erosion ; Volcanism ; Weathering
  • . They are organised in the following temporal sequence : Tertiary landform evolution; Quaternary landforms and sedimentation; Late-glacial and postglacial crustal processes and landform evolution; The Little Ice Age; Contemporary hillslope and fluvial erosion. The AA
  • beneath an ice cover between 13,500 and 10,000 years BP, the scree slopes have to be seen as an integral part of a regional geosystem. The stratigraphic and chronologic data for individual slopes do permit the recognition and discussion of successive
  • Atlantic Ocean ; C 14 dating ; Canada ; Holocene ; Ice sheet ; Pacific Region ; Palaeo-environment ; Postglacial ; Quaternary ; Sea level ; Spatial distribution ; Tectonics
  • -channel systems, the role of supraglacial meltwater input and proglacial water bodies, the controls on esker pattern, and the glaciodynamic condition of the ice sheet at the time of esker formation are discussed. A morphologic classification of eskers