Most of a small licence area located ~19 km west-northwest of Cleve has been surrendered following the completion of a helicopter-borne EM survey over the entire tenement during July 2012, looking for signs of possible buried graphite mineralisation that might have formed within highly metamorphosed Archaean to Proterozoic bedrock sediments located adjacent to large crustal penetrating regional linear structures [the relevant geophysical datasets are included herein]. No other field work was performed on the now surrendered ground.