These series of veins were intersected within the marble/skarn unit which is typically associated with a zone of alteration occurring at the contact between the intrusive body and the limestone host rock. The Calcite Veins were defined by a 72 metre (240 foot) section of pyrite-rich calcite veins occurring between 708 and 780 metres (2,320 to 2,560 feet) depth. The M-S Veins consist of two massive sulphide veins. The first M-S Vein was intercepted at a depth of 828 to 840 metres (2,720 to 2,760 feet), about 48 metres (160 feet) deeper than the Calcite Veins. The second M-S Vein was intercepted at a depth of 855 to 857 metres (2,800 to 2,810 feet). Assays from these intercepts are being confirmed and will be released as soon as confirmed.