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I spent a week writing a report on a 2008 drill program completed on what was Carina’s Black Lake property.&nbsp; The property is predominately underlain by mafic-intermediate volcanic rocks while gold mineralization occurs within&nbsp; quartz-carbonate-sulphide veins that occur within highly altered northeast trending shear.&nbsp;I spent a week writing a report on a 2008 drill program completed on what was Carina’s Black Lake property.&nbsp; The property is situated in the Abram-Minnitaki Greenstone belt and is largely underlain by interbedded mafic to intermediate flows &amp; flow breccias and their volcaniclastic equivalents with subsidiary iron formation and conglomerate.&nbsp; Gabbros, granodiorite and quartz-feldspar porphyrytic dykes and plugs are also present in smaller amounts.&nbsp;Gold on the property occurs most often as coarse often visible flecks within quartz-carbonate-sulphide +/- tourmaline veins and stockwork systems that are hosted within highly sheared and altered northeast trending fault/shear systems.&nbsp; The veins typically contain small amounts of pyrite, chalcopyrite, galena and arsenopyrite.