• The magnetite-ilmenite mineralization is present as a body that plunges steeply towards the southeast. Its character south of 5190100N is little known due to relatively widespread wet ground. Relatively strong magnetism extends southeasterly.
• Titanium and Vanadium are present in the intrusive complex away from the areas of pronounced magnetite content although in lower amounts.
• Susceptibility and assay data generally correlate directly.
• At present the mineralization is open, in part, towards the east, towards the west, the south and to depth.

Magnetite, ilmenite, titanium dioxide, and vanadium mineralization at Titan occurs in a southeast plunging body in gabbro to leucotroctolite in the northeastern corner of the Fall Lake complex.  The Titan deposit is located at the northern end of an aeromagnetic anomaly that is approximately1,200 by 800 meters in area.

A total of 4,898 assay intervals are recorded from 38 core holes drilled by Randsburg on the property.  Drilling highlights reported by Randsburg included 142 meters of 0.27% Vanadium (0.48% Vanadium Pentoxide) from hole RA-5-21 and 174 meters of 0.26% Vanadium (0.46% Vanadium Pentoxide) from hole RA-5-10. The mineralization started from surface to an open vertical depth of 500 meters. The complete horizontal and vertical extent of the deposit is still to be determined.  Information on the geology at Titan and assay results reported by Randsburg are available below.

An updated Technical Report dated February 26, 2010 prepared by Mines Development Associates for Randsburg calculated a National Instrument 43-101 compliant Inferred resource for the Titan project.  This Technical Report can be accessed here.