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| 01906cam 2200361za 4500 |
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| 001 | 9.835903 |
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| 003 | CaOODSP |
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| 005 | 20221107150755 |
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| 007 | cr ||||||||||| |
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| 008 | 170427s1985 oncabo|#ot|||f000 0 eng d |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|beng|bfre |
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| 043 | |an-cn-yk |
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| 086 | 1 |aM74-3/85-12E-PDF |
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| 100 | 1 |aFrench, Hugh M. |
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| 245 | 10|aGround ice investigations, Klondike District, Yukon Territory |h[electronic resource] / |cH.M. French and W.H. Pollard. |
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| 260 | |aOttawa : |bEnergy, Mines and Resources Canada, Earth Physics Branch, |c1985. |
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| 300 | |a35 p. : |bill., maps |
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| 490 | 1 |aEarth Physics Branch open file = Dossier public de la Direction de la Physique du Globe ; |v85-12 |
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| 500 | |aTitle from cover. |
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| 500 | |aAt head of title: Geothermal Service of Canada = Service géothermique du Canada. |
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| 500 | |aDigitized edition from print produced 2017 [by Natural Resources Canada] |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 3 |a"The origin of massive ground ice in the Klondike District, Yukon Territory is examined in an exposure in the Hunker Creek area. Stratigraphic and ice cryotexture data and ice petrofabric analyses suggest that a segregation origin is not appropriate for the massive clear ice body (1 - 3 m in thickness) . A residual snowbank origin is considered and found to be the most consistent with the nature of the body"--Abstract. |
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| 546 | |aIncludes abstract in French. |
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| 692 | 07|2gccst|aPermafrost |
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| 692 | 07|2gccst|aStratigraphy |
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| 700 | 1 |aPollard, W. H. |
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| 710 | 1 |aCanada. |bEnergy, Mines and Resources Canada. |
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| 710 | 1 |aCanada. |bEarth Physics Branch. |
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| 830 | #0|aOpen file (Earth Physics Branch)|vno. 85-12|w(CaOODSP)9.835819 |
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| 856 | 40|qPDF|s10.11 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M74-3-85-12-eng.pdf |
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