Geology and Mineral Occurrences of the Yalakom River Area*

(Glover et al . , 1988a, 1988b) and 1988 (Schiarizza et a l . , 1989d, 1989b). and extends the mapping eastward to include the eastem part of the Shulaps Range, the Yalakom and Bridge River valleys and the adjacent Camelsfoot Range. In addition, several weeks were spent re-examining critical areas in the Tyaughton Creek area and traversing the area south of Gun Creek in an effort to mesh our work with the maps produced by B.N. Church during his mineral deposit studies of the Bridge River mining camp (Church, 1987;