Canadian Arrow Mines Limited announced that it has intersected sulphide mineralization on its Glatz nickel copper project located 40 kilometers south of Dryden Ontario and 70 kilometers east of its flagship Kenbridge advanced nickel copper project.

Diamond drill hole GZ-09-02 intersected coarse blebby and finely disseminated sulphides from surface to the 90 meters interval. The mineralization is consistent with that displayed in trenches and outcrop exposures occurring at surface above the hole. More significantly it also intercepted vein and stringer breccia sulphide bands over a 12 meters down hole interval between 41.0 meters and 53.0 meters.

Initial examination of the core has identified encouraging widespread magmatic sulphide mineralization associated with breccia zones within a gabbro and pyroxenite intrusion. The geological model bears a resemblance to the Company's Kenbridge nickel-copper deposit. The Kenbridge deposit is also characterized by near-surface, wide-spread disseminated nickel-copper sulphide mineralization suitable for open pit extraction that resolves at depth into narrower, high grade semi-massive lenses and disseminated mineralization suitable for underground extraction.