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

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Landscapes and Landforms of the Hudson Bay Lowlandsthe main features in the landscape. These include open and forested bogs and peat plateaus; flat fen meadows, and stringed and palsa fens; and swamps, marsh, and open water. Local relief is commonly <2 m. The landscape of the lowlands is the product of its geologic history and present conditions. Th

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Anticosti Island: Geomorphological Context of a Unique Karst Areae Gulf of St. Lawrence, the Strait of Belle Isle and the Newfoundland Coastal Lowland. The region is underlain by the St. Lawrence Platform geological province whose formations are made up of different types and proportions of Paleozoic limestones and detrital rocks. Anticosti Island itself covers a

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Karst Geomorphology of the Saugeen-Bruce Peninsula, Ontario Given that it has formed within late glacial and postglacial times, it is considered as a young karst that is actively expanding. But palaeokarst forms have also been identified. The Lockport Group carbonates (Early Silurian) are the most significant karst forming rocks on the peninsula. The releas

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Ice Masses of the Eastern Canadian Arctic Archipelago sheets of Greenland and Antarctica. The ice masses are focused in the eastern part of the CAA, and stretch from the ice shelves of northernmost Ellesmere Island to glaciers in the southernmost parts of Baffin Island, together with a few mountain glaciers in northern Labrador. The majority of glacie

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Large-Scale Rock Slope Deformation from the Tablelands and Lookout Hills of Western Newfoundland, Cainstabilities in eastern Canada. The Lookout Hills GSDF (8.3 km.) on Bonne Bay (glacial trough) may be the largest GSDF in eastern Canada. It appears to be a post-glacial feature, has vertical total displacement up to 100 m, and exhibits a complex arrangement of scarps and fissures. Four other large