Saint Jean Carbon Closes Acquisition Wallingford & Saint Jovite Lump Graphite Properties
Saint Jean Carbon Inc. announced it has acquired the Wallingford Property and Saint Jovite (the "St. Jovite Property lump graphite properties.
The Company issued 1,000,000 shares as partial consideration for the Wallingford Property and 1,000,000 shares as partial consideration for the St. Jovite Property all at a deemed value of $0.06 per share.
Additional consideration for the Transaction included a $2,000 payment on the signing of the term sheet for each of the New Properties. A further $5,000 payment is to be made in 2014 for each of the St. Jovite Property and the Wallingford Property. The Company is required to issue an additional 500,000 shares for the Wallingford Property and an additional 500,000 shares for the St. Jovite Property, on the first anniversary date of the closing, subject to the mining claims associated with each respective property producing graphite with a grade of 30% and a quality of 90% Gc, and an ore quantity of 2,000,000 metric tonnes after the Company has made up to $250,000 in exploration expenditures on each property to verify same. All securities issued will be subject to a hold period of four months and one day pursuant to applicable security laws.
The Wallingford Property is located 10 km north of Buckingham village in the Central Metasedimentary Belt of the Grenville geological Province, some 182 km west of Montréal. It includes the historic Wallingford-Buckingham mine, a feldspar and quartz pegmatite dyke which crosscuts a sillimanite-garnet gneiss. The deposit was discovered by prospection in 1923 and the mine was in operation from 1923 to 1938 (SIGEOM database of MRN).
The St. Jovite Property is located 8.5 km south-south-east of the village of Brebeuf, in the Laurentian region, approximately 153 km northwest of Montreal. It is underlain by metasedimentary rocks of the Grenville Province which had been invaded by the igneous rocks of the Morin series. It includes the Brebeuf-SSE deposit which was mined sporadically from 1954 to 1961. It consists of a vein type deposit with a most important pegmatitic vein measuring 30 m.
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