Titlebook: Landscapes and Landforms of Western Canada; Olav Slaymaker Book 2017 Springer International Publishing Switzerland 2017 Geomorphology.Glac

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Corporeal

意外

florid

Book 2017 and the nature of the geomorphological landscape, which deserves wider publicity. Three of the most important geomorphological facts related to Canada are that 90% of its total area emerged from ice-sheet cover relatively recently, from a geological perspective; permafrost underlies 50% of its land

Decline

2213-2090 ppreciated diversity of Canada’s landscapes and the nature oThis is the only book to focus on the geomorphological landscapes of Canada West. It outlines the little-appreciated diversity of Canada’s landscapes, and the nature of the geomorphological landscape, which deserves wider publicity. Three o

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Holocene and Anthropocene Landscapes of Western Canadalude landscapes impacted by volcanism, periglaciation, aeolian, mass movement, fluvial and coastal processes. The proposed Anthropocene epoch is discussed under landscapes modified by human activity, climate change and associated hazards and risks.

elastic

The Banks Island Tundraem. The landscape consists of broad fluvial surfaces that are currently being modified by weak fluvial incision and mass wasting processes. It is a permafrost landscape that contains ice-wedge polygons, thermokarst lakes and ponds, frost mounds and active-layer phenomena.

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Landscapes of the Assiniboine River Watershed (d) the flat floors of former ice-dammed glacial lakes, and (e) inactive sand dunefields. In addition, the watershed contains a large glacial delta and has undergone several extraordinary changes to its river network.

PAN

The Foothills Erratics Train Region transported in a medial moraine position between mountain glaciers and a continental ice sheet. Based upon its rapid removal by human activities, it is suggested that other comparable erratic trains may have existed elsewhere but were erased by agriculture over the millennia.

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