Several single line anomalies have been outlined by the deep penetrating IP survey, clustering around the Lorraine Main zone. Due to the wide spacing of survey lines, single line anomalies could represent significant targets considering possible alkalic porphyry geometries such as the Ridgeway deposit.

The first single line anomaly is on line 000N towards the east end of the line centered at station 7900E. The anomaly is an overburden covered 10-12msec chargeability anomaly that is open to the southeast off of the grid.

The second single line anomaly is at the east end of line 2200N centered around 7650E, is within 50 m of surface and is 50-100 m thick. This anomaly is comparable in amplitude and size to the Chargeability response at the Bishop Zone, implying that it may contain significant sulfide mineralization.

The third single line anomaly is a 12-16msec chargeability anomaly located towards the west end of line 4900N centered around 3100E. The strength of this response is stronger than that of the response from the sulfide system of the Bishop zone. The line 4900N anomaly appears to be closed off to the southeast but is open to the northwest where survey lines are not long enough to test this area. In 2005, anomalous copper values were outlined in a talus sample line through this area.

New Anomalies 2008 IP Targets 299 KB, approx. 57 seconds at 56.6Kbps