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

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21#
發(fā)表于 2025-3-25 04:42:07 | 只看該作者
Slave Geological Province: An Archetype of Glaciated Shield Terrainories to the Coronation Gulf in Nunavut. Underlain by metavolcanic and metasedimentary rocks intruded by granitoid plutons, the region is rich in gold, base metals, and diamonds and hosts numerous historic, active, and prospective mines. Most recently glaciated in the Late Wisconsinan, till and glac
22#
發(fā)表于 2025-3-25 11:28:45 | 只看該作者
23#
發(fā)表于 2025-3-25 11:55:09 | 只看該作者
24#
發(fā)表于 2025-3-25 19:44:10 | 只看該作者
25#
發(fā)表于 2025-3-26 00:02:04 | 只看該作者
Little Limestone Lake: A Beautiful Marl Lake in the Interlake Region, Manitoba CaCO., with crystallites precipitating in the water to give it a rich and opaque duck-egg blue colouration. Such lakes are largely limited to recently glaciated carbonate rock terrains. Most are also shallow, with much or all of the water column being in the photic zone. Little Limestone Lake (lat.
26#
發(fā)表于 2025-3-26 01:40:23 | 只看該作者
Landscapes of the Assiniboine River Watershedin deposited by stagnating ice sheets, (b) closed depressions containing small lakes and sloughs of the Prairie Pothole region, (c) glacial spillways, (d) the flat floors of former ice-dammed glacial lakes, and (e) inactive sand dunefields. In addition, the watershed contains a large glacial delta a
27#
發(fā)表于 2025-3-26 07:33:39 | 只看該作者
Red River Valley, Manitoba: The Geomorphology of a Low-Relief, Flood-Prone Prairie Landscapeosits, the Red River valley forms the southern extension of the Manitoba Lowlands. The dominant landform of the central valley is a low-relief clay plain composed of glacilacustrine deposits that?accumulated in glacial Lake Agassiz. The north-flowing Red River is a low-energy, suspended sediment, mu
28#
發(fā)表于 2025-3-26 11:21:42 | 只看該作者
29#
發(fā)表于 2025-3-26 15:36:21 | 只看該作者
30#
發(fā)表于 2025-3-26 16:53:50 | 只看該作者
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