Ann: Visible Gold and Copper Sulphides Identified in Trenching, page-2

17 July 2014 ASX Code: WCN Visible Gold and Copper Sulphides Identified in Trenching Highlights  Visible gold and copper sulphides identified in new trenches, results include: o 10m at 2.94% copper and 8 g/t gold including;  3 metres at 7.7% copper and 19.8g/t gold o 22 metres at 2.5 g/t gold including;  4 metres at 4.5 g/t gold and;  6 metres at 5.5 g/t gold  Rock chip sampling extends mineralised zones 450 metres west to adjacent hill o Upper West zone: 5 samples average gold grade of 7.9 g/t gold o Lower West Zone: 2 samples average gold grade of 9.9 g/t gold o Upper North Zone: 5 samples average copper grade 1.02% White Cliff Minerals Limited (“White Cliff” or the “Company”) is pleased to report that results from the first two trenches completed in this year’s Kyrgyz field program contain extensive zones of copper and gold mineralisation and in some samples visible gold and chalcopyrite were identified. Trench channel sample results include:  10 metres at 2.94% copper and 8 g/t gold including 3 metres at 7.7% copper and 19.8 g/t gold and;  22 metres at 2.5 g/t gold including 4 metres at 4.5 g/t gold and 5 metres at 5.5 g/t gold The first two trenches were designed to extend and deepen the high grade mineralisation reported in January this year (ASX Release 27th January 2014). The new trenches confirm the initial results and have extended the initial mineralisation to the south (Figure 1 and 2). Multiple additional smaller zones of copper and gold mineralisation were also identified surrounding the major mineralised zones which strike West North West (310 degrees) and dip steeply to the Southwest. The mineralisation appears to be deposited from fluids related to the adjacent copper-gold porphyry intrusions two kilometres to the East. The shear zones consist of brecciated and massive quartz veins containing copper sulphides, pyrite and in some cases visible gold. Mineralisation also occurs in alteration zones in all lithology types (granodiorite, sandstone, limestone, and conglomerate) either side of the shear zones (Table 1).