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- W4285154552 abstract "The glaciated landscape of the Sloan River map area records evidence of old southwestward ice flow, followed by younger dominant northwestward flow in northernmost areas, and westward to west-southwestward flow in central and southern regions. Glacially and meltwater-scoured bedrock dominates the map area, with various till deposits discontinuously covering northern regions. Eskers and other glaciofluvial sediments define a poorly developed meltwater system, ranging in orientation from westward to northwestward. Meltwater channels show broader ranges of paleoflow directions in topographic highs. During deglaciation, which began about 10.5 ka BP, discontinuous north-south-trending recessional moraines were formed, defining a former margin of stagnating ice. Moraines in the northeast may represent the northern extension of the Forcier Moraine. Glaciolacustrine sediments associated with glacial Lake McConnell occur in the west, up to 300 m elevation. Other unrelated, isolated glaciolacustrine deltas, including those in the Coppermine River valley, occur further east up to 425 m elevation." @default.
- W4285154552 created "2022-07-14" @default.
- W4285154552 creator A5090852067 @default.
- W4285154552 date "2022-01-01" @default.
- W4285154552 modified "2023-10-18" @default.
- W4285154552 title "Reconnaissance surficial geology, Sloan River, Northwest Territories-Nunavut, NTS 86-K" @default.
- W4285154552 doi "https://doi.org/10.4095/329452" @default.
- W4285154552 hasPublicationYear "2022" @default.
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