Mineralisation of davidite-(La) in the metasomatic Proterozoic-Archean basement. The host rock contains albite, actinolite, epidote, titanite, apatite. Davidite occur as blebs from 1-5 mm, generally extremely weathered with yellowish creamy fissures. Hematite forms intergrows with davidite.
Several trenches and drill hole were made in 1950-1952.
Average uranium assayed was 0.18% U3O8 from “trench E”.
Dickinson S.B. et al. (1954), Uranium deposits in South Australia. Bull No30, Geol. Surv. S.Australia. Part IV, p115-125
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Map Reference: 34°48'30"S , 138°46'20"E
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Mineral List:5 entries listed. 5 valid minerals.
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