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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/9129
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dc.contributor.advisorBunting, B. T.en_US
dc.contributor.authorAlbert, Rubec Dean Claytonen_US
dc.date.accessioned2014-06-18T16:45:45Z-
dc.date.available2014-06-18T16:45:45Z-
dc.date.created2009-06-25en_US
dc.date.issued1976-02en_US
dc.identifier.otheropendissertations/428en_US
dc.identifier.other1186en_US
dc.identifier.other880973en_US
dc.identifier.urihttp://hdl.handle.net/11375/9129-
dc.description.abstract<p>Investigation of the morphology and mineralogy of a group of soils in the southern part of the District of Mackenzie, N.W.T is reported. A uniform suite of clay-size minerals, reflecting locally reported bedrock, is observed with weathering of surface horizons resulting in the formation of vermiculite and montmorillonite from illite and chlorite. Kaolinite, attributed to pre-glacial formation, is illuviated downwards in the these soils. Considerable quartz, feldspar, hornblende and anatase are also noted in the <2 micron fraction. Dominant soil types are Humo-Ferric Podzols and Degraded Dystric Brunisols. It is proposed that the use of Degraded Brunisol for these soils in inappropriate. The nature of fragic and placic soil horizons in the area is>discussed.</p>en_US
dc.subjectGeographyen_US
dc.subjectGeographyen_US
dc.titleClay Mineralogy and Morphology of Soils at Thor Lake, N.W.T., Canadaen_US
dc.typethesisen_US
dc.contributor.departmentGeographyen_US
dc.description.degreeMaster of Science (MS)en_US
Appears in Collections:Open Access Dissertations and Theses

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