Taruga Minerals Limited presented an exploration update for the Mt Craig Copper Project (MCCP), where an extensive reconnaissance exploration and drilling program is ongoing. The diamond drilling at Wyacca successfully intercepted visible copper mineralisation in all 3 holes. At Worrumba 19, blebby to semi-massive chalcopyrite hosted within massive dolomite was intercepted in the primary ore zone, which started at 92.5m through to 95.2m, and transitioned into finely disseminated chalcopyrite in shale downhole. At Powder Hill, in drillhole WCDD002, a gossanous zone was intercepted from 6m, before transitioning into the primary Ore Zone from 18 - 24 metres. The overall alteration zone extended for 18m from 6 to 24m. The primary ore zone is comprised of manganese and iron oxide minerals which contain fine chalcocite banding throughout. At Worrumba 21, shallow mineralisation was targeted to understand the mineralisation, lithology and structural controls. A 0.55m zone of copper-oxide mineralisation was intercepted from 12.25m, within a dolomite-siderite carbonate matrix. RC drilling has identified broader chalcopyrite-bornite mineralisation downdip of this intercept, and has further identified potential for multiple stacked lenses of copper mineralisation where structures cross cut the Tapley Hill Formation sediments. Diamond drillhole MCDD001 successfully intercepted visible malachite mineralisation from 27m - 32m. Following this, Strontium and Barium ore (Celestite and Baryte) were intercepted along with minor chalcopyrite and galena from 49.25m to 74 metres (24.75m). Drillhole MCDD003 targeted zinc, lithium and REE mineralisation identified from recent RC drilling (RC drillholes MCRC009, MCRC010, and MCRC022) at the Oxide Hill prospect. Heavily oxidised and brecciated sediments known to contain lithium, zinc and REE mineralisation were intercepted from surface. The brecciated marble unit which recently reported the grade REE intercepts (up to 0.46% TREO - MCRC009) along the margin of the adjacent dolerite was intercepted from 65.7m to 185.3m end of hole, where the hole was terminated. The drillhole skimmed the edge of the mafic-ultramafic intrusion which is host to the primary scandium and vanadium mineralisation intercepted from surface in MCRC009. At Hydrothermal Hill, the diamond drill rig recently completed the final diamond hole for the program. So far at Hydrothermal Hill, heavily altered brecciated mafic-ultramafic intrusions and dolomite-carbonates have been intercepted with accompanying serpentine, biotite, chlorite, magnetite, haematite and pyrite alteration. This alteration zone contacts on the western margin of a diapiric breccia, which the hole was collared into. Sulphides including pyrite and minor chalcopyrite have been noted within the sediments and mafic-ultramafic intrusions. The alteration identified at Hydrothermal Hill so far is indicative of intense hydrothermal alteration, with the altered carbonates potentially representing contact skarn metamorphism. Detailed ground gravity and magnetics surveys are currently underway at Wyacca and Morgan's Creek. The ground gravity surveys are being completed using ATV's using a 200m x 50m spacing in key areas and 400m x 50m grid spacing surrounding key areas. The ground magnetic surveys are being conducted on foot over selective portions of Wyacca and Morgan's Creek, using a high resolution 50m line spacing. The gravity and magnetic data are expected to highlight key structures, intrusions, lithologies and alteration zones which will used in combination with the soils, rock chip and previous drilling data to undertake further precision RC drill-testing. The geophysical data will also be used to conduct inversion modelling of prospective anomalies to assist with drill planning. The Company will present the results of the geophysical program, including new areas of interest to the market shortly, once processing is complete.