Here comes the Boom !!!, page-2

15 September 2015 ASX Code: WCN Visible Gold Outcrop Summary: Aucu Gold Deposit Highlights
 Visible gold now identified in the three separate major structures: o Upper Gold Zone, Lower Gold Zone and Southern Gold Zone  Each structure extends over 3,000 metres in length

 Each structure contains visible gold AT SURFACE White Cliff Minerals Limited (“White Cliff” or the “Company”) is pleased to provide a summary of all the visible gold samples panned from outcropping mineralised zones at and adjacent to the Aucu Gold Deposit.
Figure 1 Gold extracted by panning a crushed 100kg sample extracted from the Southern Gold Zone (SGZ) Figure 2 Surface outcrop of the Southern Gold Zone. Bright orange colour is typical of highly mineralised shear zone rich in gold Southern Gold Zone Abundant visible gold has been panned from an exceptionally rich mineralised outcrop AT SURFACE at the eastern end of the Southern Gold Zone (SGZ). This new outcrop extends the SGZ to at least 3,000 metres with visible gold identified at three different locations spread along 2,500 metres of the strike length (Figure 7). Mineralisation occurs as a 3-5 metre wide shear zone and the mineralisation cuts across granodiorite, conglomerate and mafic volcanics. Mineralisation including visible gold occurs in all three rock types. The SGZ is just 400 metres south of the inferred Aucu gold resource of 156, 000 ounces (1.2Mt at 4.2 g/t) and is easily accessible from existing tracks. The SGZ which is yet to be drill tested will be drilled in the Company’s forthcoming drill program. White Cliff Minerals Limited 2 Figure 3 Gold extracted from a 1kg sample taken from the Lower Gold Zone (LGZ). Figure 4 Surface outcrop of the Lower Gold Zone (yellow-brown zone) containing visible gold. Figure 5 Gold extracted from a 1 kg sample taken from the Upper Gold Zone (UGZ) 900 metres east of Aucu gold deposit Figure 6 Surface outcrop of the Upper Gold Zone containing visible gold in 1 kg sample from trench Lower Gold Zone Visible gold was panned from a 1 kilogram sample taken from the outcrop at 2,730 metres elevation shown in Figure 4. Mineralisation occurs in as a 10 metre wide zone cutting across silicified sandstone and mudstone. The sedimentary rocks are intruded by late stage granodiorite dykes that have fractured the sandstones allowing substantial gold deposition.