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| 03175nem 2200433za 4500 |
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| 001 | 9.858637 |
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| 003 | CaOODSP |
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| 005 | 20230131161138 |
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| 006 | m go c f |
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| 007 | cr ||||||||||| |
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| 008 | 180705s2013 onc bd a fo 0 eng d |
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| 020 | |a978-1-100-22364-3 |
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| 034 | 1 |aa|b100000|dW088000|eW087000|fN065000|gN064100 |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn-nu |
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| 086 | 1 |aM183-1/145-2013E-PDF |
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| 100 | 1 |aDredge, L. A. |
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| 245 | 10|aReconnaissance surficial geology, Yellow Bluff (west), Nunavut, NTS 46-D west |h[electronic resource] / |c[Authors: L.A. Dredge, I. McMartin, and J.E. Campbell]. |
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| 250 | |aPreliminary version |
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| 255 | |aScale 1:100,000 ; |bUniversal Transverse Mercator, zone 16 |c(W 88°00’--W 87°00'/N 65°00'--N 64°10’) |
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| 260 | |aOttawa : |bNatural Resources Canada, |c2013. |
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| 300 | |a1 map : |bcol. + |e1 map information document ([11] p.). |
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| 490 | 1 |aCanadian geoscience map ; |v145 |
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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"Preliminary surficial geology studies, based on air photo interpretation and limited field data, were undertaken in the Yellow Bluff West map area (NTS 46-D west) to provide an understanding of the distribution and nature of surficial materials, and regional glacial history. Much of the area is underlain by folded and faulted bedrock containing shallow glacially scoured lake basins. Striae on bedrock surfaces indicate ice flow toward the southeast. Till veneers are present in the area. Bare bedrock and modified till surfaces result from removal and/or reworking of glacial materials by glacial meltwater and postglacial marine wave-washing. Three major esker systems are associated with subglacial conduits, in which are aligned linear units of glaciofluvial hummocks and ridges. Below 150 m a.s.l, the flanks of the eskers have been reworked into beaches or flattened by the postglacial Tyrrell Sea. Except in areas around eskers where marine deposits are thickest, marine sediments are generally thin, and consist primarily of sand. Raised marine beaches oriented approximately parallel to the coast lie at low elevations"--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 |aMcMartin, Isabelle, |d1964- |
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| 700 | 1 |aCampbell, Janet E. M., |d1963- |
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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 ;|v145.|w(CaOODSP)9.506260 |
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| 856 | 40|qPDF|s19.49 MB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-145-2013-eng.pdf|zMap |
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| 856 | 40|qPDF|s441 KB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-145-2013-1-eng.pdf|zMap information document |
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| 856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/293047|zGEOSCAN DOI |
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