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      <marc:subfield code="a">Predictive surficial geology, Wecho River, Northwest Territories, NTS 85-O </marc:subfield>
      <marc:subfield code="h">[electronic resource] / </marc:subfield>
      <marc:subfield code="c">Authors: P. D. Morse ... [et al.].</marc:subfield>
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      <marc:subfield code="a">Preliminary version</marc:subfield>
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      <marc:subfield code="a">Scale 1:125 000 ; </marc:subfield>
      <marc:subfield code="b">Universal Transverse Mercator, zone 11 </marc:subfield>
      <marc:subfield code="c">(W 116°00’--W 114°00'/N 64°00'--N 63°00’)</marc:subfield>
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      <marc:subfield code="a">Ottawa : </marc:subfield>
      <marc:subfield code="b">Natural Resources Canada, </marc:subfield>
      <marc:subfield code="c">2016.</marc:subfield>
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      <marc:subfield code="b">col. + </marc:subfield>
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      <marc:subfield code="a">Canadian geoscience map ; </marc:subfield>
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      <marc:subfield code="a">This record only includes the map and the “Map information document” in PDF, the complete data set with all the files in various formats is available for free download at http://geoscan.nrcan.gc.ca/</marc:subfield>
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      <marc:subfield code="a">Includes bibliographical references.</marc:subfield>
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      <marc:subfield code="a">"The glaciated landscape exhibits ice flow features associated with ice advance such as drumlinoids, crag-and-tails and fluted bedrock, which together with striations, record a southwestward ice flow during the last glaciation. Glacially scoured bedrock dominates the area. Discontinuous till veneer is generally restricted to the northeastern map area. Glaciofluvial sediments, including eskers and kames generally trend southwestward. Many eskers consist of a series of short segments. During deglaciation about 11–10 ka BP, fine-grained glaciolacustrine sediments, associated with glacial Lake McConnell, were deposited in many western and southern topographic lows, up to 240 m or possibly higher. Related glaciolacustrine deltas and beaches, marking the decreasing elevation of the glacial lake over time due to isostatic rebound, occur at 270–295 m, although isolated deltas have also been observed at 310, 320, 330 m and as high as 350 m in the northeast. Postglacial eolian sediments exhibit dunes recording both north-northwestward and south-southeastward paleowind directions"--Abstract.</marc:subfield>
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      <marc:subfield code="a">Includes abstract in French.</marc:subfield>
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      <marc:subfield code="2">gccst</marc:subfield>
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      <marc:subfield code="a">Morse, Peter Douglass, </marc:subfield>
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      <marc:subfield code="a">Canada. </marc:subfield>
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      <marc:subfield code="a">Geological Survey of Canada.</marc:subfield>
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      <marc:subfield code="q">PDF</marc:subfield>
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      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1-277-2016-1-eng.pdf</marc:subfield>
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      <marc:subfield code="q">PDF</marc:subfield>
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      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1-277-2016-eng.pdf</marc:subfield>
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      <marc:subfield code="u">https://doi.org/10.4095/298686</marc:subfield>
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