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| 02203cam 2200349za 4500 |
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001 | 9.835902 |
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003 | CaOODSP |
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005 | 20221107150755 |
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007 | cr ||||||||||| |
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008 | 170427s1985 oncbd||#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 |aM74-3/85-11E-PDF |
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100 | 1 |aMichel, F. A. |
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245 | 10|aNature and history of ground ice in the Yukon |h[electronic resource] : |bisotope investigations / |cF.A. Michel. |
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260 | |aOttawa : |bEnergy, Mines and Resources Canada, Earth Physics Branch, |c1985. |
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300 | |aix, 126 p. : |bmaps, charts |
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490 | 1 |aEarth Physics Branch open file = Dossier public de la Direction de la Physique du Globe ; |v85-11 |
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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"Massive ice and ice-rich sediments from a number of sites in central and northern Yukon have been examined stratigraphically and isotopically. Within the central Yukon, ice-wedge ice, segregated ice and frost-blister ice have been identified. Along the northern Yukon coastal plain, massive ice and ice-rich sediments, exposed in the headwalls of progressive thaw slides, have been interpreted as ice-wedge ice, segregated ice and buried glacier ice. The buried glacier ice, probably of early Wisconsinan age, exists near King Point, Kay Point, and on Herschel Island in what have been described as ice-thrust moraines. Each ice type displays a characteristic isotopic signature which is useful in identifying the origin of the ice"--Abstract, p. 2. |
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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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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. 85-11|w(CaOODSP)9.835819 |
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856 | 40|qPDF|s17.92 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M74-3-85-11-eng.pdf |
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