000 02423nem  2200385za 4500
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008150406s2013    onc    bd a  fo 0   eng d
020 |a978-1-100-19078-5
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-nu
0861 |aM183-1/22-2011E-PDF
1001 |aDyke, Arthur S.
24510|aSurficial geology, Cape Dyer north, Baffin Island, Nunavut |h[electronic resource] : |bNTS 16-L northeast and NTS 16-K northwest / |c[by] A.S. Dyke.
250 |aPreliminary version
255 |aScale 1:100,000
260 |aOttawa : |bNatural Resources Canada, |cc2013.
300 |a1 map : |bcol.
4901 |aCanadian geoscience map ; |vNo. 22
504 |aIncludes bibliographical references.
5203 |a"In 2009, as part of the GEM program of the Geological Survey of Canada, Cumberland Peninsula east and southeast of the National Park was mapped. Mapping included several aspects of the regional Precambrian geology, as well as the Quaternary geology. Regional till was sampled for sedimentological and geochemical purposes, and moraines and other deposits were sampled for cosmogenic exposure dating. The eastern part of the peninsula is today an area of intensive alpine glaciation and evidently has experienced this style of glaciation throughout the Quaternary. During the last glacial maximum (28-12ka), alpine glaciers thickened to form regional ice divides over the mountains. Ice flow from these divides covered most, possibly all, of the region and supplied ice streams along several fiords. This local ice coalesced with the Laurentide Ice Sheet in Cumberland Sound. Despite possibly repeated glaciation, substantial areas show little or no sign of glacial erosion and retain Tertiary surfaces mantled with block fields and tors"--Abstract.
546 |aIncludes abstract in French.
590 |a14-16|b2014-04-17
69207|2gccst|aGeological maps
69207|2gccst|aGeomorphology
69207|2gccst|aSurficial geology
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
830#0|aCanadian geoscience map ;|vNo. 22.|w(CaOODSP)9.506260
85640|qPDF|s11.33 MB|uhttps://publications.gc.ca/collections/collection_2014/rncan-nrcan/M183-1-22-2011-eng.pdf
85640|qHTML|sN/A|uhttps://doi.org/10.4095/288967