Rek Rinti - Agam Vein Phase 1 Drill Results: Only two holes (RRD004 and RRD007) were completed to test the Agam vein during the Phase 1 program. Both holes were drilled on the same section. RDD004 was drilled to test the projected vein occurrence to the southeast of hole RRD001-RRD003.

No vein was exposed at surface but it was projected along strike from the location of historical artisanal mining. The RRD004 hole intersected the vein over a drilled width of 61.3m from 98.5 to 159.8 (true width of approximately 56m). The quartz is predominately massive crystalline with common multiphase quartz breccia containing prominent colloform and crustiform banded quartz with common ginguro banded zones containing locally abundant dark grey- black sulphides.

A very rare occurrence of fine-grained electrum mineralization was noted in hole 004 at 108.8m downhole in a narrow zone of ginguro banded quartz. This section assayed 78g/t Au and 631 g/t Ag over 0.5m. Pyrite is common as fine grained disseminations and coarse clots up to 20% in quartz matrix.

Minor chalcopyrite, galena and sphalerite also occur. Assay results indicate the intersection to average 3.4 g/t AuEq over 30m (98- 128m) including an 8.1m wide zone of 8.9 g/t AuEq (102.4 -110.5m). A deeper 6.5m wide zone of 1.47 g/t AuEq was intersected in the Agam vein from 147-153.5m.

Hole RRD007 was drilled on the same section and beneath hole RRD004 to test the wide Agam vein intersection at approximately 100m greater depth. As shown in Figure 9 the hole intersected the projected depth extension of the Agam vein over a drilled width of approximately 28m (154-182m). RRD007 intersected several narrow quartz veins and stockwork zones that returned compiled assay intercepts of generally low-grade AuEq (<1g/t) however a 2m wide zone of 5.45 g/t AuEq (2.7 g/t Au, 223.5 g/t Ag) was intersected from 154.3-156.5m.

A 20m wide brittle fault zone was also intersected at the hangingwall contact. Assay results also indicate that significant Pb-Zn concentrations (up to 0.36% Pb, 0.57% Zn) and weak Au-Ag (0.1 g/t AuEq) over a 4m width immediately adjacent to the vein contact (154m). Significant Pb (0.19%) and Zn (0.43%) concentration also occurs with a 2m wide brittle fault zone from 162m downhole.

Holes RRD004 and RRD007 also intersected an approximately 10m wide zone of stockwork quartz veining with narrow (1m) massive veins before the Agam vein that has been identified as the Pertama vein. Assays from the zone returned several narrow (<2m) zones of 0.35-0.6 g/t AuEq in RRD004 and 0.75 g/t AuEq over 8.1m (66.9-75m) in hole RDD007. Brittle fault zones also occur at and adjacent to vein/zone contacts.

Hole RRD009 located to the southwest did not intersect the Agam vein but appears to have intersected the Pertama vein with an approximate 7m wide quartz stockwork and vein zone from 99.4-106.8m. Assay results indicate low-grade mineralization with up to 0.18 g/t AuEq. Hole RRD011 was drilled from the same location as RRD009 to test the Bohay vein at depth.

The hole did intersect a narrow chalcedonic quartz vein and breccia with minor black manganese from 43.-45.1m. The intersection assayed 1.45 g/t AuEq over 2.1m (43-45.1) including 2.9 g/t AuEq over 0.5m. The intersection is unlikely of the Bohay vein and may be a narrow en enchelon vein adjacent to the Bohay vein zone.

Although only one drill section has intersected the Agam vein it is apparent the vein has considerable width and contains the textures and type of mineralization consistent with high grade Au-Ag mineralisation It is Company intention that the Phase 2 drill program include detailed drilling centered on holes RRD004 and RRD007 as part of a resource delineation program. Rek Rinti ­ Acong and Anggur Veins Phase 1 Drill Results: Holes RRD005, RRD006 and RRD008 were completed to test the Acong and Anggur veins. INTERPRETATION AND REMAINING DRILL TARGETING AT REK RINTI PHASE 2 DRILL PROGRAM: The Phase 1 scout drill program at Rek Rinti was successful in that it confirmed the interpreted extent and expected characteristics of the vein-breccia zones as mapped on surface.

The drilling also confirmed the Rek Rinti veins where drilled, to locally contain significant grades of Au and Ag mineralization associated with vein textures (crustiform, colloform banding) and styles of mineralization (ginguro bands) typical of high grade vein systems. Holes RRD004 and RRD012 in particular show well developed ginguro banding with variable amounts of grey Ag- rich sulphide minerals and very rare electrum as seen in RRD004. It is also apparent that such high grade zones and vein textures are highly variable in occurrence and likely restricted in extent. This is typical of many epithermal vein systems. The common occurrence of open vugs and cavities indicate that open-space filling was an important mechanism of vein formation.

The presence of euhedral quartz crystals lining some cavities which indicate low hydraulic gradients during system closure. The deeper high-grade Au-Ag veins as seen in RRD012 and RDD003 high-grade veins can occur with little or no wallrock alteration aside from chlorite (and epidote?) alteration of the adjacent volcanic wallrock. These veins can be narrow and finely banded and often opaline and contain well developed ginguro bands as seen in RRD012.

These veins may represent a separate vein event distinct from the main vein zone and additional drilling is required to evaluate their resource potential. Based on results, it is clear the veins within the Rek Rinti prospect area show features characteristic of an epithermal vein system exposed at a relatively high level. As such it represents a highly prospective vein system with the potential for high-grade Au-Ag mineralization in the veins drilled.

Such zones will likely be of limited extent so high- grade intersections should be followed up with close-spaced drilling (50m?) with the objective to define zone dimensions. All high-grade zones intersected in the Phase 1 drill program remain open to depth and along strike. Zones showing continuity across two or more holes should be considered for a targeted program of detailed resource delineation.

The Phase 2 program should also test other defined veins in the prospect area as part of a continuation of the Phase 1 scout drill program. It may be necessary to modify ideal hole locations depending on the presence of local artisanal mining activity.