Rockcliff Copper Corporation announced additional drill hole assay and geophysical drill hole survey results from its ongoing phase 2 exploration program on the Talbot Property. The property forms part of Rockcliff's Snow Lake Project centered on the Snow Lake Mining Camp, Manitoba. At the Talbot deposit main lens, drill hole TB-012 intersected the main lens mineralization confirming continuity of the main lens in an area void of drilling along the deposit's north boundary of the main lens. At the Talbot deposit north lens, the Company completed several drill hole geophysical surveys on historic holes and on its recently completed drill holes TB013 and TB014 which intersected 7.1 metres grading 4.1% Cueq and 2.6 metres grading 2.4% Cueq respectively for additional information). The survey results identified a new drill target that represents one of the large undrilled conductive plates yet discovered on the property below the existing Talbot deposit north lens mineralization, measuring 300 metres along strike and 600 metres of depth extent. Historic hole TLS007 appears to have intersected the very top edge of the conductive plate intersecting 4.4% Cueq across 2.1 metres. A preliminary longitudinal image of the conductive plate location relative to the Talbot deposit is shown below. TB-012 was drilled at UTM NAD83 co-ordinates 458520E/5997036N, to a depth of 962 metres, along an azimuth of 285 degrees and a dip of -70 degrees. The depositional environment at the Talbot Property is similar to that of present and past producing base metal mines of bi-modal volcaniclastic rocks in the prolific Flin Flon - Snow Lake Greenstone Belt. The gold-rich Talbot copper deposit is defined as a stratabound, VMS deposit consisting of several lenses of stringer to massive sulphides of pyrite, chalcopyrite, sphalerite and pyrrhotite in a quartzofeldspathic gneiss.