86527 092JSE043 Lillooet CAY, BLUE ROCK 092J049 092J08W Showing 50° 29' 24'' 122° 18' 05'' 50.490000 -122.301389 10 5593128 549558 Silver Coast Crystalline Bridge River I05 : Polymetallic veins Ag-Pb-Zn+/-Au The Cay occurrence is located on the north side of a peak, approximately 600 metres south of Melvin Lake. The region is underlain by metasedimentary rocks of the Mississippian to Jurassic Bridge River (Complex) Group, intruded by dominantly granodioritic stocks of the Jurassic to Tertiary Coast Plutonic Complex. The showing is underlain mainly by metasedimentary rocks: argillite, chert and conglomerate with some andesite and serpentinite. Locally, vuggy and limonitic quartz veins host pyrite, galena, malachite and possible tetrahedrite mineralization. In 1983, a 0.4-metre chip sample (CR-5) assayed 68.0 grams per tonne silver, while a 0.9-metre chip sample (CR-8) assayed 18.8 grams per tonne silver (Assessment Report 12281). In 1980 and 1981, Denison Mines completed programs of geochemical sampling and geological mapping on the area as the Mel claims. In 1983, a program of geochemical sampling and geological mapping was completed on the area as the Cay property. EMPR AR 1935-F11,12; 1954-108; 1967-131; 1968-162 EMPR ASS RPT 9715, *12281 EMPR PF (Report by H.H. Cohen 1963) GSC OF 482