[en] The property exhibits local anomalous gamma radiation associated with segregations in the granite. Most of the anomalous gamma radiation results from probable secondary uranium minerals on fracture surfaces; most of the remaining anomalous gamma radiation comes from uraninite and metamict accessory minerals; most of the fluorescence comes from weakly uraniferous opal. The uranium was probably a late stage differentiate. Neither gamma-ray logs nor scanner samples, nor cut samples (excepting one radiometric assay which, on chemical analysis, assayed 0.06% U₃O₈) reveal the presence of mineralized material containing more than 0.08% U₃O₈