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Canada Carbon Inc V.CCB

Alternate Symbol(s):  BRUZF

Canada Carbon Inc. is a Canada-based mining exploration and development company. The Company is focused on the acquisition, exploration and development of graphite deposits. It holds a 100% interest in two graphite properties located in Quebec: the Miller Graphite Project located in Grenville-Sur-La-Rouge and the Asbury Graphite Mine located in Notre-Dame-du-Laus. The Miller hydrothermal lump-vein historical graphite mine and surrounding property covers approximately 100 square kilometers (km2) and is located around 80 km west of Montreal in the Grenville Township. The Asbury Graphite Mine property is made up of two claims for a total of 119 hectares (ha). The Mine is located around 8.1 kilometers (km) northeast of Notre-Dame-Du-Laus in the Laurentides Region of southern Quebec.


TSXV:CCB - Post by User

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Comment by pipsthefrogon Apr 05, 2013 4:50pm
183 Views
Post# 21218140

RE: The Miller Mine

RE: The Miller Mine

Excellent Info... Thanks geeraf1

 

From Cirkel, 1907, in describing the Miller property:

There can be noticed, in the open cut and shaft, four veins of graphite from a few inches up to eighteen inches wide, which are reported to increase at the bottom of the shaft (which could not be examined on account of being filled with water) to a width of thirty inches. Sixty-five tons of this vein graphite were mined and sent to the Globe Refining Company of Jersey City, N.J., and yielded thirty-two tons of clean crucible graphite. The Morgan Crucible Company of London and also J. H. Gauthier and Company, Jersey City, used some of this graphite in their crucibles and they pronounced it equal to the best Ceylon.

Of course, the Ceylon they refer to is the most valued vein graphite from Sri Lanka. As today's geophysics and drilling should be able to better define what exists at depth, Miller has outstanding potential, much better than Zenyatta's "graphite veins" in my opinion until Zen shows us real chunks or lumps of almost entirely graphite. It is believed that the surface vein outcrops which have been recently assayed at up to around 80% Cg may be pinched by non-graphitic dikes and are likely much wider at further depth. This is rare and appears to be a true vein deposit. Time will tell whether it is of significance in size to be commercialized.

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