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008150406s2013    onc    bd a  fo 0   eng d
020 |a978-1-100-21790-1
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-bc
0861 |aM183-1/119-2013E-PDF
24500|aSurficial geology, Emile Creek, British Columbia |h[electronic resource] / |c[by] D.H. Huntley ... [et al.].
250 |aPreliminary version
255 |aScale 1:50,000
260 |aOttawa : |bNatural Resources Canada, |cc2013.
300 |a1 map : |bcol.
4901 |aCanadian geoscience map ; |vNo. 119
500 |aIncludes a legend.
504 |aIncludes bibliographical references.
5203 |a"Canadian Geoscience Map 119 depicts the surficial geology over some 790 km2 covered by the Emile Creek map sheet (NTS 94-O/15) in northeastern British Columbia. The Maxhamish Escarpment lies along the west margin of the map sheet. Much of the map area encompasses the northwest limit of the Etsho Plateau and a portion of the Petitot River watershed. Much of the map area is drained by Emile Creek and its tributaries which flow north into the Petitot River. Bedrock is mantled by unconsolidated earth materials dating to the Late Pleistocene (Late Wisconsinan Glaciation, > 25 ka to ca. 10 ka) and non-glacial Holocene (ca. 10 ka to present). Deposits of till, green on the map, are generally suitable for placement of infrastructure. Glaciofluvial deposits with mineral, aggregate, and groundwater potential are coloured orange. Slopes disturbed by landslides, debris flows. and rock falls appear brown and pink. Glaciolacustrine and organic deposits with sporadically discontinuous permafrost are coloured purple and grey. Alluvial deposits prone to flooding, erosion, and sedimentation appear yellow on the map"--Abstract.
546 |aIncludes abstract in French.
590 |a14-03|b2014-01-17
69207|2gccst|aGeological maps
69207|2gccst|aWatercourses
69207|2gccst|aSurficial geology
7001 |aHuntley, D. H. |q(David Hayes)
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
830#0|aCanadian geoscience map ;|vNo. 119.|w(CaOODSP)9.506260
85640|qPDF|s6.98 MB|uhttps://publications.gc.ca/collections/collection_2014/rncan-nrcan/M183-1-119-2013-eng.pdf
85640|qHTML|sN/A|uhttps://doi.org/10.4095/292396