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| 03264cem 2200469za 4500 |
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| 001 | 9.834454 |
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| 003 | CaOODSP |
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| 005 | 20221107150435 |
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| 006 | m go c f |
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| 007 | cr ||||||||||| |
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| 008 | 170818s2017 onca bd a fo 0 eng d |
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| 020 | |a978-0-660-08105-2 |
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| 034 | 1 |aa|b100000|dW0650000|eW0640000|fN0560000|gN0553000 |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn-qu |
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| 086 | 1 |aM183-1/316-2017E-PDF |
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| 100 | 1 |aRice, J. M. |q(Jessey Murray) |
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| 245 | 10|aSurficial geology, Lac Mistinibi, Quebec, NTS 23-P northeast |h[electronic resource] / |c[authors, J.M. Rice, R.C. Paulen, and M. Ross]. |
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| 250 | |aPrelim. |
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| 255 | |aScale 1:100,000 ; |buniversal transverse Mercator proj., zone 20 |c(W 65°00’--W 64°00'/N 56°00'--N 55°30’). |
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| 260 | |a[Ottawa] : |bNatural Resources Canada, Geological Survey of Canada, |c2017. |
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| 300 | |a1 map : |bcol. + |e1 map information document ([7] p.). |
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| 490 | 1 |aCanadian geoscience map ; |v316 |
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| 500 | |aRelief shown by contours. |
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| 500 | |aThis publication is related to Canadian geoscience map 333 (call number M183-1/333-2017E-PDF). |
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| 500 | |aIncludes text, index map and location map. |
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| 500 | |aThis 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/ |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 3 |a"The Lac Mistinibi area is of moderate relief characterized by extensive till blankets and at higher elevations, till veneers and bedrock outcrops. The region was glaciated by the Laurentide Ice Sheet throughout Wisconsin time, east of the Quebec-Labrador ice centre. Two general phases of glacial landform development have occurred in the map-area, with northeast-trending large crag-and-tail landforms and streamlined eastward-trending landforms. These two orientations represent two phases of radial ice flow that have affected the region. Large eskers and related glaciofluvial deposits also transect the map sheet along west to east direction, indicative of the westward deglaciation of the region. Abundant, small meltwater channels in the upland areas of the region are evidence of late-phase ice ablation during final deglaciation. Below 488 m elevation, the region was inundated by glacial Lake Naskaupi, which occupied the George River basin and its tributaries and winnowed till surfaces"--Abstract. |
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| 546 | |aIncludes abstract in French. |
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| 692 | 07|2gccst|aGeological maps |
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| 692 | 07|2gccst|aGeomorphology |
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| 692 | 07|2gccst|aSurficial geology |
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| 700 | 1 |aPaulen, Roger C., |d1970- |
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| 700 | 1 |aRoss, Martin, |d1970- |
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| 710 | 1 |aCanada. |bNatural Resources Canada. |
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| 710 | 2 |aGeological Survey of Canada. |
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| 830 | #0|aCanadian geoscience map ;|v316.|w(CaOODSP)9.506260 |
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| 856 | 40|qPDF|s21.35 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1/M183-1-316-2017-eng.pdf|zMap |
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| 856 | 40|qPDF|s455 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-1/M183-1-316-2017-1-eng.pdf|zMap information document |
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| 856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/300656|zGEOSCAN DOI |
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