000 02488cem  2200385za 4500
0019.575827
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008150406s2013    onc    bd a  fo 0   eng d
020 |a978-1-100-21743-7
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-nt
0861 |aM183-1/110-2013E-PDF
24500|aSurficial geology, Artillery Lake, Northwest Territories, NTS 75-O |h[electronic resource] / |c[by] D.E. Kerr ... [et al.].
250 |aPreliminary version
255 |aScale 1:125,000
260 |aOttawa : |bNatural Resources Canada, |cc2013.
300 |a1 map : |bcol.
4901 |aCanadian geoscience map ; |vNo. 110
504 |aIncludes bibliographical references.
5203 |a"The Artillery Lake map area is characterized by three broad zones based on distribution and nature of surficial sediments. In the northwest, hummocky till with a few north-south trending moraine ridges, and smaller areas of till veneer and bedrock dominate the landscape. The northeast is defined by extensive regions of exposed, scoured bedrock and till veneer. The southern regions consist of a combination of bedrock, till veneer and fluted till blanket. Till is dissected by glaciofluvial corridors consisting of eskers, ice-contact sediments and scoured bedrock. These features record a westward meltwater paleoflow in the south, a northwestward flow in the central regions, and a northwestward to northward flow in the northern regions of the map area. The earliest ice flow, defined by rare striae and subtle sculpted bedrock in the north, was southwestward. The last, dominant ice flow forms a radiating pattern defined by striae, fluted bedrock crag-and-tails and drumlins. Ice flow was westward in the south, to northwestward in the central regions, but locally southwestward, in the northeasternmost region"--Abstract.
546 |aIncludes abstract in French.
590 |a14-16|b2014-04-17
69207|2gccst|aGeological maps
69207|2gccst|aLakes
69207|2gccst|aSurficial geology
7001 |aKerr, Daniel Ernest, |d1961-
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
830#0|aCanadian geoscience map ;|vNo. 110.|w(CaOODSP)9.506260
85640|qPDF|s19.08 MB|uhttps://publications.gc.ca/collections/collection_2014/rncan-nrcan/M183-1-110-2013-eng.pdf
85640|qHTML|sN/A|uhttps://doi.org/10.4095/292268