An area in the south-west of the Frome Embayment, that is centred ~80 km south-southeast of the Beverley uranium mine, has been taken up to explore for possible buried palaeochannel and sandstone hosted roll front style secondary uranium mineralisation which may have formed within the Tertiary age Namba and Eyre formations. Potential was also thought to exist for unconformity style base metal mineralisation and gold deposits that could be associated with faulting within Lower Cambrian limestone. No field work was done during the first licence year. Activities were limited to a making literature review and compilation of historical exploration data. The occurrence of reduced and oxidised sediments was noted and considered encouraging, with planned exploration aiming to determine the position of target redox fronts. No field work was done during licence Year 2. During licence Year 3, in September 2015, to test the Tertiary strata near basement highs interpreted from historic airborne EM survey data, 2 vertical rotary mud open drillholes were put in to total depths of 264 m and 258 m respectively. Both holes encountered a sedimentary sequence comprising the Willawortina, Namba and Eyre formations, which is comprised mainly of silt and clay, with poorly developed sand beds. Both holes were terminated within Adelaidean metasediments. No significant radioactivity peaks were recorded on their wireline gamma ray logs (the maximum log reading was obtained at 183 m depth in hole MFN002, within the upper Eyre Formation).