Renforth exposes 180m of continuous visible mineralization Renforth’s wholly owned 260km 2 Surimeau property, located in the Pontiac sediments, contiguous to the Canadian Malartic Mine, near Malartic Quebec. Surface visible copper mineralization has been encountered, consisting of stringers of medium to coarse grained chalcopyrite and occasional trace clots of bornite, the channel samples have been sent for assay.
The program, targeting an area between two groups of the holes drilled in the 2.2km long drill program earlier this year has, to date, successfully exposed 180m of sulphide bearing bedrock and completed the southern portion, approximately 50m long by 7m wide, of the eastern crosscut, once complete the crosscut will be approximately 150m in length. The southern contact between the ultramafic and the Pontiac was successfully intersected in the cross cut, along with another band of alteration similar to the main alteration running through the centre of the stripped area.