000 02400cem  2200433za 4500
0019.572175
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008150406s2013    onc    bd a  fo 0   eng d
020 |a978-1-100-19580-3
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-nu
0861 |aM183-1/36-2011E-PDF
1001 |aUtting, Daniel J.
24510|aSurficial geology, Conn Lake (southwest), Baffin Island, Nunavut |h[electronic resource] / |c[by] D.J. Utting, E.C. Little, and D.E. Kerr.
250 |aPreliminary version
255 |aScale 1:100,000
260 |aOttawa : |bNatural Resources Canada, |cc2013.
300 |a1 map : |bcol.
4901 |aCanadian geoscience map ; |vNo. 36
500 |aIncludes a legend.
504 |aIncludes bibliographical references.
5203 |a"The southwest part of the Conn Lake map sheet lies within the Baffin Uplands Physiographic Region, where bedrock is extensively covered by thick glacial deposits. Some areas exhibiting scour were eroded by active, warm-based ice for longer periods of time than regions of cold-based ice. A northeastward early Holocene flow is associated with ice in Foxe Basin to the northeast. Four phases of ice flow were recognized. The Last Glacial maximum relates to phase 1, northeastward, when the region was covered by actively eroding warm-based ice. The second is a north-northeastward flow during the early stages of the Barnes Ice Cap. The next two phases (a later readvance, phase 3, and continued deglaciation, phase 4) are thought to relate to the proto-Barnes Ice Cap"--Abstract.
546 |aIncludes abstract in French.
590 |a13-29|b2013-07-19
69207|2gccst|aGeological maps
69207|2gccst|aLakes
69207|2gccst|aSurficial geology
7001 |aLittle, E. C.
7001 |aKerr, Daniel Ernest, |d1961-
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
794 |tSurficial geology, Conn Lake (southwest), Baffin Island, Nunavut, NTS 37-E/3, NTS 37-E/4, NTS 37-E/5, and NTS 37-E/6 |w(CaOODSP)9.801324
830#0|aCanadian geoscience map ;|vNo. 36.|w(CaOODSP)9.506260
85640|qPDF|s9.24 MB|uhttps://publications.gc.ca/collections/collection_2013/rncan-nrcan/M183-1-36-2011-eng.pdf
85640|qHTML|sN/A|uhttps://doi.org/10.4095/292365