Mkangombe

Pacific Wildcat Resources is also exploring the Mkangombe Project in the Kwale District of Kenya which is located in the north-western section of SPL 256. The Mrima Hill carbonatite is situated 50kms away to the south-east. At Mkangombe copper-lead-zinc mineralisation has been identified by a Japanese exploration consortium in the early 1990s and was interpreted as being structurally controlled related to an extensive regional fault system with many kilometers of mineralized strike potential. Associated with faulting are abundant occurrences of lead-zinc-barite/quartz-vein mineralisation along faults parallel to the regional Jurassic age fault. These occurrences appear to form within a mineralised quartz vein system which persists over more than 10km with the potential to host a significant base metal resource. High-grade but narrow zinc mineralization (up to 59% zinc over 30cms) was intersected in diamond drilling in the 1990s.