From a technical review, it is apparent that the Central Manitoba property lies in a

geologic environment, which is similar to the San Antonio mine area at Bissett.

Both properties lie adjacent to the Ross River pluton, though on opposite sides of

the intrusion, in areas of high heat flow characterized by abundant felsic dike

intrusion and numerous gold occurrences. As well, both the San Antonio and

Central Manitoba veins lie within, or along the margins of, large concordant

gabbro sills, with clear patterns of structural control.