Future Prospects

River Orchy 383.2 g/t Au, 321.5 g/t Au and 197.3 g/t Au 145.5 g/t Au 134.5 g/t Au,in rock chip samples molybdenite-rich quartz veins assaying up to 0.62% molybdenum.

24 breccia pipes in the nearby Beinn Udlaidh area. Previous exploration in this area by Ennex International plc in the 1980s identified high grade boulders, up to 358.9 g/t Au.

High grade vein systems at Auch ·
Creag Sheileach o Outcrop 13.2g/t Au, 36.6g/t Ag
AQ drill hole 25.5g/t Au 14.3g/t Ag over 1.0m

Coire Ghabhalach
o Outcrop 23.4g/t Au, 29.6g/t Ag
o AQ drill hole 15.2g/t Au, 36.2g/t Ag over 2.1m

Clach Bhadach
o Outcrop 62.4g/t Au, >200g/t Ag
o Outcrop 20.7g/t Au, 164.7g/t Ag

Beinn Odhar
o Outcrop 9.8g/t Au 80.4g/t Ag
o Outcrop 8.9g/t Au, >200g/t Ag, 47.1g/t Te

Breccia Pipe identified ·
Breccia pipe identified - highly anomalous gold value recorded - 1.7g/t Au

Clach Bhadach
Rockchip sampling of the outcrop has returned values including 62.4g/t Au and >200g/t Ag, 20.7g/t Au and 164g/t Ag and 16.4g/t Au and >200g/t Ag.

River Vein Area
Rockchip sampling of the outcrop has returned values including 62.4g/t Au and >200g/t Ag, 20.7g/t Au and 164g/t Ag and 16.4g/t Au and >200g/t Ag.
River Vein Gold vein - 194.6 g/t Au, >200g/t Ag and 103.2 g/t Au, 76.6 g/t Ag
o 7 samples from 20 above 0.1% Mo

Beinn Udlaidh Vein
NE extension
o Confirmation of previous high grade outcrop including o 73.3g/t Au, >200g/t Ag o 17.7g/t Au, >200g/t Ag · Vein traced for 1900m on strike

River Vein
RV01: o 9.7g/t Au, 13.3g/t Ag, 0.6% Pb, 2.1% Zn over 40cms (intersection width) - 60 metres below surface
o 3.5g/t Au, >200g/t Ag, 1.4%Pb, 100ppm Mo and 34g/t Te over 52 cms (intersection width) - 78 metres below surface •
RV02: o 4.39g/t Au, >200g/t Ag, 1.8% Pb, 167ppm Mo, 43g/t Te over 40cms (intersection width) - 70 metres below surface

Sron Garbh Mafic complex ·
Selected AQ drill hole results best intercepts include ·
SQ AQ 16 - 0.22g/t Au, 0.78g/t Pd, 0.58g/t Pt, 0.75% Cu, 0.18% Ni and 0.01% Co over 2 metres ·
SQ AQ 15 - 0.08g/t Au, 0.43g/t Pd, 0.35g/t Pt, 0.58%Cu, 0.17% Ni and 0.02% Co over 1.25 metres
SQ AQ 26 - 0.11g/t Au, 0.31g/t Pd, 0.37g/t Pt, 0.65% Cu, 0.21% Ni and 0.04% Co over 1 metre ·
SQ AQ 28 - 0.03g/t Au, 0.29g/t Pd, 0.25g/t Pt, 0.17% Cu, 0.12% Ni and 0.03% Co over 1.5 metres ·
SQ AQ 21 - 0.15g/t Au over 20 metres ·
SQ AQ 22 - 0.12g/t Au over 22.5 metres

Rock chip sample grading 0.82% Cu, 0.21% Ni, 1.14g/t Pt, 0.79g/t Pd, 0.18g/t Au, 4g/t Ag, 16.1 g/t Se and 0.03% Co
A check rock chip sample in the vicinity of a high Cu - Ni sulphide occurrence previously sampled, returned a value of 0.18g/t Au, 4.3 g/t Ag, 0.82% Cu, 0.21% Ni and 0.03% Co.

The sample was re-assayed for Platinum and Palladium and returned values of 1.14g/t Pt and 0.79g/t Pd (Assays for other PGEs (Osmium, Iridium, Rhodium, and Ruthenium) are yet to be conducted).

Dr Dave Holwell of the University of Leicester's Department of Geology and contributing author to the recent Society of Economic Geologists publication "Magmatic Ni - Cu - PGE deposits" has visited the site and has reviewed the current results.
He commented:
"This is most certainly an exciting discovery. The mineralisation at Sron Gharb has the characteristics of a classic magmatic Cu-Ni sulphide deposit with elevated precious metals. The ratios of sulphur and selenium indicate that the magma has been contaminated by sulphur-bearing crustal rocks - a key factor in helping to generate deposits of this kind. Intriguingly, the geochemical signatures show that the sulphides cannot have gained their high precious metal contents without the presence of a much larger magmatic system than is current exposed. If this has been preserved beneath the current surface (as a larger intrusion or conduit system), it could represent a potential host for massive sulphide mineralization at depth."