Titlebook: Landscapes and Landforms of Eastern Canada; Olav Slaymaker,Norm Catto Book 2020 Springer Nature Switzerland AG 2020 Geomorphology.Landscap

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2213-2090 eaches of Hudson Bay bear comparison with the classic fjords of Norway and the Baltic Sea raised beaches. As for wetlands, there are distinctive Arctic, Subarctic, Boreal, Eastern Temperate and Atlantic wetland978-3-030-35137-3Series ISSN 2213-2090 Series E-ISSN 2213-2104

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Pierre Dietrich,Alexandre Normandeau,Patrick Lajeunesse,Jean-François Ghienne,Mathieu Schuster,Alexi

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Glacial Landform Assemblages of Mainland Nunavut, West of Hudson Bay and Their Palaeoglaciological Stions, meltwater features, end moraines, and raised beaches and shorelines related to proglacial lakes and marine transgression. It is clear that whilst the distribution of landforms is a complex interplay between the overriding ice sheet properties (thickness, velocity, basal thermal regime) and th

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Anticosti Island: Geomorphological Context of a Unique Karst Areadeposits. Outcrops of preglacial weathered bedrock remain. Karst features are found everywhere on the island. In most areas, karst is of recent Holocene age with shallow underground flows. The Upper Salmon River karst is the most developed and seems somewhat older and is partly inherited from an ear

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Geomorphology of the Great Lakes Lowlands of Eastern Canadaand glacifluvial sediments along shorelines. Post-glacial isostatic uplift has resulted in entrenchment of both subsequent and consequent river systems exposing mixed channel boundaries of glacial sediments and bedrock. Modern infrastructure has developed on these surfaces that are still undergoing