Risk and valuation analysis of the KEY LAKE Project |
Status Risk : Green exploration |
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Title(s) of the KEY LAKE Project |
![](http://www.24hgold.com/24hpmdata/pub/205_canalaska.gif) | Canalaska Uranium Ltd |
![](http://www.24hgold.com/style/all/img/bouton/website.png) | ![Company Profile Company Profile](http://www.24hgold.com/style/all/img/bouton/website.png) | ![All Projects All Projects](http://www.24hgold.com/style/all/img/bouton/website.png) | ![Company website Company website](http://www.24hgold.com/style/all/img/bouton/website.png) | ![](http://www.24hgold.com/style/all/img/bouton/website.png) |
Title | Company Profile | All Projects | Company website | Company project page |
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![](http://www.24hgold.com/24hpmdata/pub/3127_arimex.gif) | WestCan Uranium Corp. |
![](http://www.24hgold.com/style/all/img/bouton/website.png) | ![Company Profile Company Profile](http://www.24hgold.com/style/all/img/bouton/website.png) | ![All Projects All Projects](http://www.24hgold.com/style/all/img/bouton/website.png) | ![](http://www.24hgold.com/style/all/img/bouton/website.png) | ![](http://www.24hgold.com/style/all/img/bouton/website.png) |
Title | Company Profile | All Projects | Company website | Company project page |
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Location of the KEY LAKE Project |
This project comprises three separate, relatively small claim blocks, one 10 km ENE of the Key Lake Mine and the other two overlying basement rocks respectively 8km SW and 12 km W of the Key Lake mine.
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History of the KEY LAKE Project |
During the 1970's and 1980's, extensive exploration was done primarily in the area of the Key Lake mine by Uranerz. Regional geochemical and geophysical studies located numerous anomalies in the district and some of these targets were drilled prior to the discovery of the Key Lake mine.
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Geology of the KEY LAKE Project |
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Project areas cover different geologic environments, one overlies Athabasca sandstone and conglomerates (50 to 150 metres to basement). The other two cover exposures of the underlying Wollaston domain. The Wollaston domain is of Lower Proterozoic (Trans-Hudson) age and is composed of metamorphosed sediments (Psammites, Pelites, and minor Calc-Silicates).
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