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Glacial landforms of northwest Saskatchewan

机译:萨斯喀彻温西北部的冰川地貌

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A comprehensive map of glacial landforms is presented for the area of northwest Saskatchewan, Canada. Remote sensing of 1-arc (~30?m resolution) Shuttle Radar Topography Mission digital elevation models over an area of approximately 15,000?km~(2) were used as the primary data source for landform identification. A total of 16,856 landforms were identified pertaining to Quaternary glacial and postglacial activity. Ten landform types were mapped: ice flow parallel lineations (flutings, drumlins, mega-scale glacial lineations, and crag-and-tail ridges), moraines (major and minor), ice-thrust ridges, crevasse-fill ridges, meltwater landforms (major and minor meltwater channels and eskers), palaeo-shorelines and dunes. Collectively, these landforms constitute a glacial and postglacial landform record, which exhibits a more complex pattern than previously recognised, with evidence of multiple cross cutting ice flow directions. This geomorphological mapping of the regional landform record provides the prerequisite for future reconstructions of the glacial dynamics and chronology of northwest Saskatchewan.
机译:提供了加拿大萨斯喀彻温省西北部地区冰川地形的综合地图。 1弧(约30?m分辨率)的航天飞机雷达地形任务数字高程模型(约15,000?km〜(2))的遥感被用作识别地形的主要数据源。总共确定了与第4冰期和冰期后活动有关的16,856个地貌。绘制了十种地貌类型:冰流平行线型(沟纹,鼓林,大型冰川线型和长尾脊),冰mo(大,小),冰冲断脊,裂隙填充脊,融水地貌(主要和次要的融水河道和加沙地带,古海岸线和沙丘。这些地貌共同构成了冰川和冰川后的地貌记录,与以前所认识的相比,它表现出更为复杂的模式,并具有多个横切冰流方向的证据。该区域地貌记录的地貌图为今后重建萨斯喀彻温西北部的冰川动力学和年代学提供了前提。

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