71300 082ESW028 Osoyoos JOE 7 082E003 082E04E Showing 49° 02' 23'' 119° 35' 34'' 49.039722 -119.592778 11 5434875 310600 Silver, Copper, Molybdenum Omineca Okanagan, Plutonic Rocks L04 : Porphyry Cu +/- Mo +/- Au, I06 : Cu+/-Ag quartz veins The Joe 7 showing is located at 1160 metres elevation along a prominent northwest-trending ridge, 2 kilometres west of Blue Lake (Assessment Report 970). The southern two-thirds of the property are underlain by Jurassic Kruger syenite and nepheline syenite. To the north are granodiorite and quartz diorite of the Middle Jurassic Similkameen intrusion. Jointly, these have intruded a northwest-trending roof pendant of Carboniferous to Permian Kobau Group metasediments and metavolcanics. Quartzite, phyllite, quartz-mica schist and greenstone are the dominant lithologies surrounding the showing. Alteration consists primarily of silicification with minor carbonate alteration. The greenstone has been more intensely propylitic altered to chlorite, epidote, carbonate, and potassic altered to potassium feldspar. Low grade copper mineralization occurs in all rock types except syenite and nepheline syenite. Disseminated chalcopyrite and bornite with pyrite and magnetite comprise sulphides which appear to have been hydrothermally introduced in quartz and calcite veinlets up to 5 millimetres thickness. Malachite stains are also present in an abandoned pit at the Joe 7 showing. Copper mineralization appears associated with regional northwest-trending shears. A typical sample from one of these shear zones is reported to yield 17.14 grams per tonne silver, 0.373 per cent copper and 0.004 per cent molybdenum EMPR AR 1968-21 EMPR ASS RPT *970, 1228, 2027, 3701, 4423, *4919 EMPR GEM 1969-298; 1971-384; 1972-39; 1973-45 EMPR OF 1989-5 GSC MAP 85A; 341A; 538A; 539A; 541A; 15-1961; 1736A; 2389 GSC MEM 38, pp. 425-478; 179 GSC OF 481; 637; 1505A; 1565; 1969 GSC P 37-21 EMPR PFD 812169, 812170, 812171, 812172, 812173