The area of low resistivity (blue - green) to the Northwest is the Princeton group sediments, while the higher resistivity (yellow –red - purple) is associated with the volcanics and intrusives of the Upper Triassic Nicola Group. However the area of lower resistivity in the center of the map appears to correlate with zones of fracturing and alteration within the Nicola Group.

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Areas of low chargeability (blue) surround areas of moderate(green) to high ( yellow –red – purple). In the southeast and southwest chargeability highs represent large anomalies coming to surface from depth. Exploration has located wide zones of mineralization in the southwest (See News Release *June 5, 2008* ).

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