April 9, 2008 Reported that during a ground geophysical program consisting of 38.5 line kilometres over a 3.5 km by 8 km area where a regional magnetic anomaly had previously been identified during an airborne survey . The magnetic anomaly is interpreted to overlie the northern limb of a buried anticline along strike and down dip from small mineral prospects with weak fracture and stratigraphically controlled replacement and breccia bodies, and may represent the presence of an intrusion into the favorable host rocks at the core of the anticline.