000 03248cem  2200409za 4500
0019.858769
003CaOODSP
00520221107160100
006m    go  c f      
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008180710s2014    onc    bd a  fo 0   eng d
020 |a978-1-100-22083-3
0341 |aa|b125000|dW108000|eW106000|fN063000|gN062000
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-nt
0861 |aM183-1/139-2013E-PDF
24500|aReconnaissance surficial geology, Lynx Lake, Northwest Territories, NTS 75-J |h[electronic resource] / |c[Authors: D.E. Kerr ... [et al.]].
250 |aPreliminary version
255 |aScale 1:125,000 ; |bUniversal Transverse Mercator, zone 13 |c(W 108°00’--W 106°00'/N 63°00'--N 62°00’)
260 |aOttawa : |bNatural Resources Canada, |c2014.
300 |a1 map : |bcol. + |e1 map information document ([10] p.).
4901 |aCanadian geoscience map ; |v139
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/
504 |aIncludes bibliographical references.
5203 |a"The Lynx Lake map area is characterized by three transitional zones based on distribution and nature of surficial sediments. In the southwest, large areas of bedrock and till veneer predominate. Northwest and central regions exhibit an increase in overburden cover, notably fluted till blanket. The northeast and southeast map areas have a greater cover of till veneer, till blanket which is fluted and drumlinized, and hummocky till. The later may contain large, subdued moraine ridges of variable orientation. The entire map area is dissected by glaciofluvial corridors consisting of eskers, ice-contact sediments and scoured bedrock, trending westward in the north and west-southwestward in the central and southern regions. The earliest ice flow, inferred from rare striae and subtle fluted landforms in the eastern half of the map area, was southwestward. The last dominant ice flow was westward in the north, grading slightly west-southwestward, in the central and southern regions. In the Whitefish Lake-Garde Lake area, as well as Lynx Lake-Howard Lake area, glaciolacustrine beaches and washing limits are developed on the flanks of some drumlinoids and glaciofluvial sediments. They occur up to 25-30 m above current lake levels but the extent of these short-lived glacial lakes remains uncertain"--Abstract.
546 |aIncludes abstract in French.
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 ;|v139.|w(CaOODSP)9.506260
85640|qPDF|s42.41 MB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-139-2013-eng.pdf|zMap
85640|qPDF|s159 KB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-139-2013-1-eng.pdf|zMap information document
85640|qHTML|sN/A|uhttps://doi.org/10.4095/293624|zGEOSCAN DOI