Coast Copper Corp. provided an update on exploration of its 100% owned Scottie West property (the Property) located in British Columbia's ("BC") Golden Triangle district approximately 35 kilometers ("km") northwest of Stewart, BC and 8 km west of the past producing Scottie Gold Mine. The company's exploration program included prospecting, sampling and mapping of veins and structures in areas of newly exposed, altered and sheared volcanic and sedimentary rocks. 130 rock samples were collected from vein, grab and float materials, which resulted in anomalous gold, silver and tellurium assay values at the SE Exposure and Leduc East Central Ridge locations. Surficial sampling of vein and select float samples at the SE Exposure and Leduc East Central produced ten samples ranging from 0.5 to 5.5 grams per ton ("g/t") gold ("Au"), 10.9 to 189.0 g/t silver ("Ag"), and up 0.75% lead ("Pb") and 0.59% zinc ("Zn"), with two anomalous tellurium ("Te") values of 16.99 and 25.26 g/t noted at the SE Exposure. Theeduc c NE, Leduc East Central and SE Exposure zones are hosted iJurassic age andesitic volcanic rocks from thehe Unuk River Member of the Betty Creek Formation, which are in contact with the Summit Lake stock, part of the early Jurassic aged Texas Creek Plutonic Suite. At both the SE Exposure and Leduc East Central areas, a sedimentary package consistent with Stuhini Group sediments was identified which could indicate the lower contact of the Hazleton-Stuhini stratigraphic contact to be confirmed with detailed mapping. The precious metal mineralization on the Property consists of east-west trending, steeply dipping quartz-carbonate-pyrite-arsenopyrite-pyrrhotite veins that are characteristic of
other intrusion-related, mesothermal precious metal mineralized veins reported along this regional mineralized trend.