Annual report for the period 1 September 2009 to 31 August 2010

Abstract

During the current reporting period, ground follow-up work consisting of gamma-ray spectrometer survey and geological mapping was carried out to locate near-surface occurrence of uranium mineralisation. The spectrometer survey showed absence of near surface radiometric response suggesting exposed calcrete/silcrete is anomalously low in uranium. The ground follow-up work did not reveal presence of any near-surface uranium mineralisation that would explain the RadonX anomaly; it is, therefore, deduce that a relatively deeper uranium source may be responsible for this anomalous response. To test this idea a drilling program has been proposed.