00000nem 2200000za 4500 9.576236 CaOODSP 20230131161133 m go c f cr ||||||||||| 150406s2014 onc bd a fo 0 eng d 978-1-100-22082-6 CaOODSP eng eng fre n-cn-nt M183-1/138-2013E-PDF Surficial geology, Reliance, Northwest Territories, NTS 75-K [electronic resource] / [by] D.E. Kerr ... [et al.]. Preliminary version Scale 1:125,000 Ottawa : Natural Resources Canada, c2014. 1 map : col. Canadian geoscience map ; 138 Includes bibliographical references. "The Reliance map area is characterized by three main elements based on distribution and nature of surficial sediments. The northeast and southeast map areas have a greater cover of fluted and drumlinized till blanket, with some transitional till veneer. Throughout the rest of the map sheet, extensive areas of bedrock predominate, with minor isolated deposits of till. The Lockhart and Snowdrift river valleys are predominantly infilled by meandering alluvial and terraced glaciofluvial sediments, some with active dunes. In these valleys, terraces and outwash plains occur at various elevations, including 230 m, 245 m, 260 m, 305 m, and 320 m a.s.l. Some may be related to glacial Lake McConnell, as are raised beaches at 335 m a.s.l. in McLeod Bay. Glaciofluvial corridors, of various magnitudes, consisting of eskers, ice-contact sediments, and scoured bedrock, trend generally southwestward to westward across the map area. Isolated glaciolacustrine deltas record local ponding of glacial meltwater. The last dominant ice flow varied from southwestward to westward"--Abstract. Includes abstract in French. 14-16 2014-04-17 gccst Geological maps gccst Geomorphology gccst Surficial geology Kerr, Daniel Ernest, 1961- Canada. Natural Resources Canada. Geological Survey of Canada. Canadian geoscience map ; 138. (CaOODSP)9.506260 PDF 25.85 MB https://publications.gc.ca/collections/collection_2014/rncan-nrcan/M183-1-138-2013-eng.pdf HTML N/A https://doi.org/10.4095/293424 293424