000 03379cem  2200433za 4500
0019.808614
003CaOODSP
00520221107140428
006m    go  c f      
007cr |||||||||||
008160718s2016    onc    bd a  fo 0   eng d
020 |a978-0-660-04123-0
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-bc
0861 |aM183-1/252-2016E-PDF
1001 |aFerbey, T. |q(Travis)
24510|aSurficial geology, Moffat Creek area, British Columbia, parts of NTS 93-A/3, NTS 93-A/4, NTS 93-A/5, and NTS 93-A/6 |h[electronic resource] / |c[authors, T. Ferbey, V.M. Levson, and A. Plouffe].
250 |aPreliminary version
255 |aScale 1:50 000 ; |bUniversal Transverse Mercator, zone 10 |c(W 121°40’--W 121°10'/N 52°25'--N 52°10’)
260 |a[Ottawa] : |bNatural Resources Canada, |cc2016.
300 |a1 map : |bcol. + |e1 map information document ([6] p.).
4901 |aCanadian geoscience map ; |v252
4900 |aBritish Columbia Geological Survey, geoscience map ; |v2016-1
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 Moffat creek area includes the Woodjam porphyry Cu-Au-Mo developed prospect. Between Moffat and Woodjam creeks, this prospect consists of six mineralized zones: Megabuck, Deerhorn, Spellbound, Southeast, Takom, and Three Firs. Till deposited during the Late Wisconsinan Fraser Glaciation is the predominant glacial sediment in the area. Landform-scale ice-flow indicators such as drumlins and crag-and-tail ridges, and outcrop-scale features such as striations, demonstrate that ice initially flowed south-southwest and later flowed north-northwest. Hummocky topography and eskers suggestthat deglaciation was, at least in part, via downwasting of stagnant ice masses. Important accumulations of glaciofluvial sand and gravel deposits in the Horsefly River valley, and in lower volumes in the southwest part of the study area, represent sources of construction aggregate. Retreat-phase glaciolacustrine sediments were deposited in the Horsefly area and Beaver Creek valley at elevations of up to 800 m above sea level. These deposits could be contemporaneous with, and related to, higher water levels in the Fraser or Quesnel river systems during deglaciation and the formation of glacial Lake Fraser. Alternatively, they could be related to local damming of the Beaver Creek and Horsefly River drainages"--Abstract.
546 |aIncludes abstract in French.
69207|2gccst|aGeological maps
69207|2gccst|aGeomorphology
69207|2gccst|aSurficial geology
7001 |aLevson, V. M.
7001 |aPlouffe, Alain, |d1963-
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
830#0|aCanadian geoscience map ;|v252.|w(CaOODSP)9.506260
85640|qPDF|s24.51 MB|uhttps://publications.gc.ca/collections/collection_2016/rncan-nrcan/M183-1-252-2016-1-eng.pdf|zMap
85640|qPDF|s119 KB|uhttps://publications.gc.ca/collections/collection_2016/rncan-nrcan/M183-1-252-2016-eng.pdf|zMap information document
85640|qHTML|sN/A|uhttps://doi.org/10.4095/297591|zGEOSCAN DOI