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

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Olav Slaymaker,Norm CattoServes as a complementary book to Landforms and Landscapes of Canada (west).Includes numerous illustrations presenting the landscapes and geomorphology of eastern Canada.Provides and informative and a

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Eastern Canadian Landscapes as a Function of Structure, Relief and Processc megaregions whose boundaries are controlled exclusively by geological structure. These megaregions are (a) the Canadian Shield, which is the craton or core of North America; (b) the surrounding plains arranged in a broken ring around the Shield together with an inlier of similar lithology stratigr

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Quaternary Glacial, Glacimarine and Glacilacustrine History geomorphology relates to Marine Isotope Stage 2. Areas of resistant bedrock are dominated by glacial erosional features, such as roches mountonées. Glacial depositional landforms are prominent in southern Ontario, Québec, and the Maritime provinces. In Arctic Canada, glaciation had lesser effects o

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Northwestern Ontario: The Thunder Bay Region of the Sleeping Giant, Mt. McKay and others, resulting from the intrusion of the Logan diabase sill into the Precambrian shales and sandstones of the Animikie formation. There are no Palaeozoic or younger rocks other than Pleistocene glacial sediments. The region has a complex glacial history, havi

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Labrador and the Northern Peninsula of Newfoundland: Foreshore and Flanking Geomorphologyphic features. Structural geology and lithology underpin landscapes from Killiniq to the Strait of Belle Isle. In central and southern Labrador, extending to the northernmost Northern Peninsula, glacial features are related to MIS 2 Laurentide glaciation. Local glaciation influenced the distinctive