00000000nem 2200000zi 4500
0019.918473
003CaOODSP
00520230131161140
006m     o  d f      
007cr cn|||||||||
008221216t20222022oncag  bh a  fo 0   eng d
020 |a9780660467719
040 |aCaOODSP|beng|erda|cCaOODSP
0410 |aeng|beng|bfre
043 |an-cn-nt|an-cn-yk
0861 |aM183-1/455-2022E-PDF
1102 |aGeological Survey of Canada.|ecartographer, |eissuing body.
24510|aSurficial geology, La Biche River northwest, Yukon-Northwest Territories, NTS 95-C/11, 12, 13, and 14 / |cauthor: I.R. Smith.
255 |aScale 1:100,000 ; |buniversal transverse Mercator projection, zone 10 |c(W 126°00'--W 125°00'/N 61°00'--N 60°30').
264 1|aOttawa ON : |bNatural Resources Canada = Ressources naturelles Canada, |c2022.
264 4|c©2022
300 |a1 online resource (1 map) : |bcolour + |e1 map information document (8 unnumbered pages) + 1 surficial symbols file (1 unnumbered page).
336 |acartographic image|bcri|2rdacontent
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aCanadian geoscience map ; |v455
500 |aShows extensive areas of till cover across the undulating Highland Plateau, and extensive bedrock-controlled landsliding.
500 |aRelief shown by contours and spot heights.
500 |aIncludes text, index map, location map, and colour photograph.
500 |aThis record only includes the map and the "map information document" and the "surficial symbols" 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"This map is situated in the Hyland plateau, west of the Mackenzie Mountains, in southeast Yukon. The area was inundated by the Cordilleran Ice Sheet during the Late Wisconsinan glaciation. Ice advanced east to northeast across the rolling bedrock terrain, producing dense networks of sometimes crosscutting bedrock flutings and drumlinoid ridges. During deglaciation, ice flow became increasingly topographically constrained, shifting to more northward flow along major valleys. Meltwater flowing north initially crossed the drainage divide into the Nahanni River basin. Later, as ice retreated south and eastwards, ice-contact deltas and kame terraces formed along the retreating margins. The area is largely covered by till veneer, with bedrock exposed along most ridge crests and glacially incised valley walls. Shale units within the Besa River and Mattson formations are prone to failure, and large rotational landslides are common"--Abstract.
546 |aIncludes abstracts in English and French.
650 0|aGeology|zYukon|vMaps.
650 0|aGeology|zNorthwest Territories|vMaps.
650 6|aGéologie|zYukon|vCartes.
650 6|aGéologie|zTerritoires du Nord-Ouest|vCartes.
655 7|aGeological maps|2lcgft
655 7|aDigital maps|2lcgft
655 7|aCartes géologiques|2rvmgf
655 7|aCartes géographiques numériques|2rvmgf
7001 |aSmith, Ian R. |q(Ian Robert)|eauthor.
7101 |aCanada. |bNatural Resources Canada, |eissuing body.
830#0|aCanadian geoscience map ;|v455.|w(CaOODSP)9.506260
85640|qPDF|s17.88 MB|uhttps://publications.gc.ca/collections/collection_2023/rncan-nrcan/m183-1/M183-1-455-2022-eng.pdf|zMap
85640|qPDF|s595 KB|uhttps://publications.gc.ca/collections/collection_2023/rncan-nrcan/m183-1/M183-1-455-2022-1-eng.pdf|zMap information document
85640|qPDF|s486 KB|uhttps://publications.gc.ca/collections/collection_2023/rncan-nrcan/m183-1/M183-1-455-2022-2-eng.pdf|zSurficial symbols
85640|qHTML|sN/A|uhttps://doi.org/10.4095/330591|zComplete data set