The Klippen Project consists of two contiguous licenses covering 10,400 hectares located in the southern portion Gold Line belt.
The Klippen Project contains >15 km of an interpreted second order splay structure off the main Gold Line structural corridor. Historic work has identified a 5 km Au, As, Cu, Zn anomaly in shallow glacial till coincident with the structural corridor identified from airborne magnetic data. Follow up top of bedrock and diamond drilling have confirmed in situ mineralization under a small portion of the anomaly with several kilometres of structural corridor so far untested.
The Geology of the Klippen project consists of an inverted volcano-sedimentary sequence intruded by several pre- to syn-kinematic granitic intrusions within a broad, anastomosing high strain structural corridor. Mineralization on the project has been identified along high strain corridors along the margins of and within a highly deformed and altered granodiorite intrusion.