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      <marc:subfield code="a">Kerr, Daniel Ernest, </marc:subfield>
      <marc:subfield code="d">1961-</marc:subfield>
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      <marc:subfield code="a">Reconnaissance surficial geology, Rae, Northwest Territories, NTS 85-K </marc:subfield>
      <marc:subfield code="h">[electronic resource] / </marc:subfield>
      <marc:subfield code="c">[authors: D. E. Kerr, P. D. Morse and S. A. Wolfe].</marc:subfield>
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      <marc:subfield code="a">Prelim.</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 118°00’--W 116°00'/N 63°00'--N 62°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:datafield tag="300" ind1=" " ind2=" ">
      <marc:subfield code="a">1 map : </marc:subfield>
      <marc:subfield code="b">col. + </marc:subfield>
      <marc:subfield code="e">Map information document ([6] p.).</marc:subfield>
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      <marc:subfield code="a">Canadian geoscience map ; </marc:subfield>
      <marc:subfield code="v">290</marc:subfield>
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    <marc:datafield tag="500" ind1=" " ind2=" ">
      <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>
    </marc:datafield>
    <marc:datafield tag="504" ind1=" " ind2=" ">
      <marc:subfield code="a">Includes bibliographical references.</marc:subfield>
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      <marc:subfield code="a">"Following deglaciation about 11–10 ka BP, fine-grained glaciolacustrine sediments, associated with glacial Lake McConnell, were deposited in most of the map area, up to 290 m above sea level (a.s.l.). These sediments overlie buried ice-flow features such as drumlinoids, drumlins, crag-and-tails and fluted bedrock, recording a southwestward ice flow during the last glaciation. A broad discontinuous band of till extends SE-NW in the central part of the map area. Glaciofluvial sediments and some bedrock ridges were reworked into glaciolacustrine beaches throughout the area. These beaches, present at an elevation up to 300–310 m a.s.l., mark the decreasing elevation of the glacial lake over time due to isostatic rebound. In the southwest, only the Horn Plateau, consisting of undifferentiated glacial deposits with colluvium on its slopes, remained above the limit of glaciolacustrine inundation. Minor glaciolacustrine iceberg scours in the southeast and postglacial eolian dunes in the south-central regions trend SE-NW. The fine-grained glaciolacustrine sediments may be overlain by organics and exhibit thermokarst activity"--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>
      <marc:subfield code="a">Geological maps</marc:subfield>
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      <marc:subfield code="2">gccst</marc:subfield>
      <marc:subfield code="a">Geomorphology</marc:subfield>
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    <marc:datafield tag="692" ind1="0" ind2="7">
      <marc:subfield code="2">gccst</marc:subfield>
      <marc:subfield code="a">Surficial geology</marc:subfield>
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      <marc:subfield code="a">Morse, Peter Douglass, </marc:subfield>
      <marc:subfield code="d">1975-</marc:subfield>
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      <marc:subfield code="a">Wolfe, Stephen Andrew, </marc:subfield>
      <marc:subfield code="d">1963-</marc:subfield>
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      <marc:subfield code="a">Canada. </marc:subfield>
      <marc:subfield code="b">Natural Resources Canada.</marc:subfield>
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      <marc:subfield code="a">Geological Survey of Canada.</marc:subfield>
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      <marc:subfield code="a">Canadian geoscience map ;</marc:subfield>
      <marc:subfield code="v">290.</marc:subfield>
      <marc:subfield code="w">(CaOODSP)9.506260</marc:subfield>
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    <marc:datafield tag="856" ind1="4" ind2="0">
      <marc:subfield code="q">PDF</marc:subfield>
      <marc:subfield code="s">27.28 MB</marc:subfield>
      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1-290-2016-1-eng.pdf</marc:subfield>
      <marc:subfield code="z">Map</marc:subfield>
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      <marc:subfield code="q">PDF</marc:subfield>
      <marc:subfield code="s">606 KB</marc:subfield>
      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1-290-2016-eng.pdf</marc:subfield>
      <marc:subfield code="z">Map information document</marc:subfield>
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      <marc:subfield code="q">HTML</marc:subfield>
      <marc:subfield code="s">N/A</marc:subfield>
      <marc:subfield code="u">https://doi.org/10.4095/298838</marc:subfield>
      <marc:subfield code="z">GEOSCAN DOI</marc:subfield>
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      <marc:subfield code="a">298838</marc:subfield>
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