Constantine Metal Resources Ltd. to report initial results from its prospecting and soil sampling program at the Big Nugget Gold project in Southeast Alaska. The work program confirmed the historical reported high grade gold mineralization and has provided new information to develop targets for follow up drilling. Two key gold prospects, Golden Eagle and McKinley Creek Falls are located upstream from the Porcupine Creek gold placer operations along McKinley Creek. The gold prospects, as described in historic government reports, have high-grade gold sample results that have received no systematic exploration for their economic potential. Both gold prospects are located on Constantine's 100% leased lands, about 8 kilometers east of the Company's advanced-stage Palmer Cu-Zn-Au-Ag massive sulphide project. The exploration field program consisted of prospecting along McKinley Creek (95 rock samples), soil sampling on 100-200 meter spaced lines along the east side of McKinley Creek (566 soil samples) and the evaluation of the geological setting of the gold mineralization. Confirmation of high grade gold mineralization at the Golden Eagle prospect (Vug vein zone) with outcrop grab samples ranging from trace to 44.7 g/t gold. The Vug vein zone is characterized by quartz-pyrite-pyrrhotite-sphalerite veins that cut through a 4 meter wide, tan coloured, silica-carbonate altered mafic dyke hosted in metasediments (Porcupine Slate). Chip samples across the Vug vein zone returned 9.8 g/t gold over 2.3 meters and 3.6 g/t gold over 1.0 meter. Pyritic-quartz vein grab samples from outcrops located 140 and 185 meters downstream of the Golden Eagle prospect returned 22.4 g/t gold and 38.9 g/t gold, respectively. Upstream of the Golden Eagle prospect, at about 400 meters, quartz-pyrite-sphalerite boulder samples returned 8.0 g/t gold (34.5% Zn) and at about 800 meters, quartz-pyrite veins in altered mafic dyke boulders returned 8.1 g/t gold. Soil sampling outlined a broad, 250 to 300 meter wide >50ppb gold-in-soil anomaly at the McKinley Creek Falls prospect with results ranging up to 970 ppb gold. The gold-in-soil anomaly extends approximately 650 meters to the east along a previously interpreted fault zone. Soils appear to be an effective exploration tool and additional sampling is required to determine the full-extent of the anomaly. The McKinley Creek gold mineralization is associated with quartz-carbonate-muscovite ± sulphide (pyrite-sphalerite-pyrrhotite-chalcopyrite) veining within altered mafic dykes and to a lesser extent within the Porcupine slates. The altered mafic dykes range in thickness from a few centimeters to upwards of 10 meters in width and crosscut and parallel the slate stratigraphy. The Porcupine slates and altered mafic dykes are moderate to tightly folded about east-west trending fold axes with an overall shallow to moderate westerly plunge. Mineralized gold bearing veins appear to be controlled in part by extension linked to the folding.