000 03237nem  2200421za 4500
0019.858772
003CaOODSP
00520230131161138
006m    go  c f      
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008180710s2014    onc    bd a  fo 0   eng d
020 |a978-1-100-22080-2
0341 |aa|b125000|dW104000|eW102000|fN063000|gN062000
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-nt
0861 |aM183-1/136-2013E-PDF
1001 |aMaynard, Dennis Edward, |d1949-
24510|aReconnaissance surficial geology, Carey Lake, Northwest Territories, NTS 65-L |h[electronic resource] / |c[Authors: D. Maynard and D.E. Kerr].
250 |aPreliminary version
255 |aScale 1:125,000 ; |bUniversal Transverse Mercator, zone 13 |c(W 104°00’--W 102°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 ; |v136
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"Reconnaissance mapping, through aerial photograph interpretation and limited legacy field data in the Carey Lake map area, provides an understanding of surficial sediments and glacial history. The last major ice flow was predominantly westward, as indicated by crag-and-tails, drumlins, and other glacially fluted landforms occurring throughout the map area. Exposed granitic and gneissic bedrock, till veneer, and fluted till dominate the topographically lower region east of Mosquito, Mary, and Gravel Hill lakes. To the west of this series of lakes, hummocky till, till blanket, and large glaciofluvial corridors characterize the landscape. In the shallow basins of these same lakes, fine-grained glaciolacustrine sediments and raised beaches occur up to 320-330 m elevation, and are associated with glacial Lake Thelon. Other glaciolacustrine sediments, found around Carey Lake, as well as to the southwest and southeast, locally overlying areas of ridged till, may relate to an extension of glacial Lake Thelon, an isolated glacial lake, or possibly a phase of glacial Lake Kazan. Areas of organic deposits are presumably underlain by glaciolacustrine sediments, reflecting the uncertainty of glaciolacustrine sediment thickness and extent"--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 ;|v136.|w(CaOODSP)9.506260
85640|qPDF|s16.94 MB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-136-2013-eng.pdf|zMap
85640|qPDF|s144 KB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-1/M183-1-136-2013-1-eng.pdf|zMap information document
85640|qHTML|sN/A|uhttps://doi.org/10.4095/293627|zGEOSCAN DOI