In addition to the Glacier, Cap and Mount Henry Clay prospects described above, there are numerous other massive sulphide occurrences which are worthy of further investigation.

The 737 Zone target lies 2,500 feet east of the Lower Main Zone on the east part of the Main Zone  trend. It is a Pulse EM geophysical target interpreted by Cominco to have the signature of a large massive sulphide deposit. One hole drilled in the interpreted location of the anomaly did not hit any significant mineralization. A new surface showing discovered in 1998 assayed 12.0% Zn, 2.66% Pb, and 47.6 g/t Ag over 0.5 feet.

The Nunatak prospect, about 1 km south of the Cap yielded a bulk sample (91 kg – 200 lb) from three stacked barite occurrences which yielded an average grade of 11.84 oz/ton Ag and 0.092 oz/ton Au.

Grab samples from the Boundary prospect returned values up to 6.6% Cu, 3610 ppm Zn, 12 ppm Ag and 1980 ppm Au.

The Red Creek occurrence discovered by Cominco (1993) is 3 km from the Glacier Creek mineralized zones in correlative units.

The HG and Gullies occurrences also have evidence of massive sulphide and correlative stratigraphic settings with the main areas of interest described above.  Grab samples from HG mineralized zone contain up to 0.36% Cu, 14.1% Zn, 2.3% Pb, 198.9 ppm Ag and 1.58 ppm Au.

None of these occurrences have been drilled to date.