Investor Presentaiton

Other Prospects in Focus OVERVIEW 11 Flapjack | MB 12 Torpedo Creek | MB 13 Josephine | MA Pri Cu | Sec. NA | Ab. Mine | Very Small <500t 14 Bomb Gorge | MA 15 Pom Pom | LA 16 Amanda | UA Pri. Au Sec. NA | Outcrop | Very Small <0.5t 17 Big Ben | UA 18 Little Nathan | UA 19 19 Unicorn UA 20 20 Crowbar | UA Pri. Cu | Sec. NA | Outcrop | Very Small <500t 21 Old Man Creek | UA 22 Mercy | UA Quililar Formation | Structurally controlled mineralisation with ENE fault, haematitic quartz veins and rhyolitic dykes (potential IOCG) | Possible replacement carbonate mineralisation | 981ppm Cu Gunpowder Creek Formation and Paradise Creek Formation | Mineralisation style and occurrence poorly understood Surprise Creek Formation [mid-lower sections] | Mineralisation confined to a fault bound block | Host rocks characterised by fine feldspathic sandstone, iron-rich sandstone and mica-rich siltstone | 283ppm Cu Surprise Creek Formation. | Hosted in pink feldspathic quartzite, prominently veined with quartz | Potential for the quartz veins to be a source of gold | 62.7ppm Cu Surprise Creek Formation. | Mineralisation confined to a fault bound block | 69.2ppm Cu Lochness Formation [Myally Subgroup] | Mineralisation proximal to east-west fault located northwest side of a sizable regional anticline that plunges northward Quililar Formation [upper section] | Mineralisation identified close to contact with the Upper Quartzite Member. | Host material characterised by alluvial-covered sandstones to dolomitic sandstone, siltstone and shales Lochness Formation | Hosted in breccia associated with north-east trending fault | Fault divides Lochness Formation from the Quililar Formation | Area covered by quartzite debris and alluvial sands | Limited outcrop Quililar Formation | | Mineralisation style and occurrence poorly understood Lochness Formation [Myally Subgroup] | Close to Weberra Granite | Mineralisation style and occurrence not well understood Upper Mount Isa Group Rocks | Hosted in west fault-bounded and folded sequence consisting of the Warrina Park Quartzite and Native Bee Siltstone | 4.8ppm Cu Mineralisation style and occurrence not well understood NWQ COPPER PROJECT - INVESTOR PRESENTATION 34

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