Risk and valuation analysis of the Hammond Reef Project |
Status Risk : Advanced discovery |
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Title(s) of the Hammond Reef Project |
![](http://www.24hgold.com/24hpmdata/pub/1100_osisko.gif) | Osisko Mining Corp. Interest: 100% |
![](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) | ![Company project page](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/43_kinross.jpg) | Kinross Gold Corporation Net Smelter Return: 2% |
![](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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Location of the Hammond Reef Project |
The property is located in the Sawbill Bay/Marmion Lake Area (in the Thunder Bay Mining Division, approximately 220 km west of Thunder Bay, Ontario. The property consists of 122 contiguous unpatented
claims and 22 patents/leases totalling 3830 hectares.
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History of the Hammond Reef Project |
The Sawbill Bay Gold District has been the locus of intermittent gold exploration since the original discovery on what became the Hammond Reef property by Joe
Mistahasen in 1895. Subsequently the property was acquired by a Thunder Bay (Fort William) more...
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Geology of the Hammond Reef Project |
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The property is predominantly underlain by the Marmion Lake granitoid suite comprising fresh to intensely altered tonalite-trondhjemite; subordinate, unaltered granitoid gneiss; and minor mafic lenses, typically highly altered. Pegmatite dykes and pe more...
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