Phoenix Torp Lake Beaverdam Bamako Hope Bay Hay Duck Anialik Lac de Gras Hammer Cal / Dotty

Location: Anialik Location Map 53 KB, approx. 11 seconds at 56.6Kbps The Anialik project is located in the western portion of Nunavut, approximately 170 km east southeast of Kugluktuk and approximately 575 km north northeast of Yellowknife, Northwest Territories. Size: The Anialik project consists of portions of 3 Nunavut Tunngavik Incorporated (NTI) parcels of Inuit Owned Lands (IOL) (parcels CO-30 and CO-81) and 12 mineral claims. Combined retained portions of the parcels and the claims total 43,458 acres. Ownership: 100% North Arrow. Highlights: Covers portions of the Anialik River volcanic belt and the High Lake volcanic belt. The High Lake volcanic belt hosts the High Lake VMS deposit (17.3 million tonnes grading 3.3% Zn and 2.2 % Cu). Historical work at North Arrow's Run Lake prospect located 28 km from High Lake has identified significant stringer copper mineralization related to the Run Horizon. Previous work by Strongbow Exploration Inc., has identified a number of prospective gold showings. Historical sampling at the Greenstone Lake showing included: a single sample returned 2.78 g/t gold from a quartz vein with 4% pyrite; 1 g/t gold for six of eight samples, including 33.83, 22.63 and 7.98 g/t gold respectively. 2011 prospecting at Greenstone Lake resulted in six of twelve samples returning assays of greater than 1 g/t gold, including 11.2, 6.8 and 3.6 g/t gold respectively Summary: The Anialik project covers Archean greenstone terrain which is favourable for volcanogenic massive sulphide (VMS) and gold deposits. In the fall of 2011 prospecting identified additional mineralized shears with six of twelve samples returning assays of greater than 1 g/t gold and including assays of 11.2, 6.8 and 3.6 g/t gold respectively. The results to date identify a series of subparallel shears within a corridor measuring over 600 m long and over 50 m wide. A program of detailed geologic mapping, sampling and ground geophysics is planned for the 2012 field season. VMS prospects include the mineralized Run Lake horizon and the Rush base metal showing. In the mid 1970's seven of eight drill holes drilled at Run Lake to shallow depths (<60 m) within a sequence of felsic to mafic volcanics returned Cu values ranging from 0.30% to 3.85% over widths of 1.4 to 7.6 m. More recently in 1993, deeper drilling returned 0.91% copper over 22.5 m including 0.40 m of massive sulphide mineralization returning 8.06% Zn and 1.70% Cu. The Rush showing consists of several gossans with anomalous base metal mineralization. Surface grab samples from the area have returned from 0.08% to 2.1% copper and up to 24.5% zinc. Gold mineralization includes the Felicia showing and the Locanna prospect. The Felicia showing consists of quartz-chalcopyrite veinlets in carbonate altered intermediate to mafic volcanics. Anomalous samples included 18.8 and 8.7 g/t Au. The Locanna gold prospect is characterized by deformed stockwork pyritic quartz veins that locally contain significantly anomalous concentrations of gold. Mineralization occurs within a 300 m wide by 3000 m long corridor. Forty seven of 146 prospecting samples collected along this corridor returned in excess of 1 g/t gold with high values of 44.2 g/t gold, 20.9 g/t gold, and 14.2 g/t gold. Channel sampling of three areas along a 7 m strike length of one vein near the southern end of the corridor returned 14.4 g/t gold over 1.6 m, 51.2 g/t gold over 0.25 m, and 6.8 g/t gold over 1.18 m. News Releases November 09, 2011 North Arrow Intersects 7.55 m Grading 4.91 g/t Gold at Hope Bay Oro Project, Nunavut Highlights North Arrow Minera... (706 KB)

	HomeCorporateProjectsInvestorsNewsQwikReportContactDisclaimer