Operations Updated

Solomon Gold PLC 26 July 2006 Solomon Gold plc - Operations Update 26/7/06 Summary and Highlights •Commencement of drilling on the Hambusimaloso North target (Mbetilonga) •Encouraging sampling results from first pass at Sutakiki •High grade copper - zinc skarn mineralisation identified at Vuralanggoma (Mbetilonga) •Next drill target at Hahala porphyry prospect (Mbetilonga) Introduction Solomon Gold plc ('Solomon Gold' or the 'Company') was admitted to AIM on 10 February pursuant to a £5m placing by Williams de Broe plc. Solomon Gold is exploring for world class copper-gold targets on Guadalcanal, Solomon Islands. The project area is located on the southwest Pacific Rim of Fire, which belt hosts numerous ore bodies including Ok Tedi, Panguna (Bougainville) and Lihir. Solomon Gold commenced a drilling program which was hampered by drilling support and logistic issues, sample transport problems, the establishment of a sample preparation facility, a requirement to negotiate a new helicopter service contract, landowner negotiations and riots as result of racial tensions. These issues have now been resolved and the Company is making important advances in the exploration of the area. Solomon Gold now has a more powerful helicopter at its disposal and a new drilling contract which has provided for re-equipping and additional support for the drilling rig by the contractor. The Company recommenced drill testing on the Hambusimaloso target on 22 July 2006 with drill hole MB03. A complete copy of this update may be viewed with a map on the Company's website www.solomongold.com Mbetilonga (PL04/05) During the past quarter Solomon Gold field crews have continued to upgrade mapping and sampling information in the core Mbetilonga project on Guadalcanal, 15 km south of the capital, Honiara. Two drill holes were drilled on the southern section of the Hambusimaloso copper anomaly, a 1.3 km2 area of soil sampling results over 1,000 parts per million copper. Only one of these holes (MB02) adequately tested the anomaly at the drill site and the other hole (MB01) failed to reach the target as a result of equipment failure. These issues have been resolved with the renegotiation of the drilling contract and a new drill target location has been identified 450 metres north of the initial drill holes. This hole site (MB03) has been located on the basis of an interpretation of copper and molybdenum anomalism which strengthens to the north from Hambusimaloso, and the results from MB02. Both MB01 and MB02 returned consistent low grade copper mineralisation which was predominantly localised in sporadic thin veins and shears and common in fragments of mineralised volcanics and intrusive porphyry containing visible chalcopyrite in the drill core. The holes intersected essentially barren sediments underneath the fractured volcanics. Hole Azimuth Declination From To Intersection (m) Copper grade degrees degrees (m) (m) MB01 030 -70 40 48 8 0.26% MB02 300 -70 46 66 20 0.07% The origin of the mineralised fragments in the fractured volcanics has not yet been determined. The geology at Hambusimaloso has not yet been resolved and the complex package of sediments and volcanics appears to be masking the intrusive source of the abundant copper mineralisation at surface. It appears that north east oriented faulted and fractured zones are more broadly anomalous and that the structural corridor on this trend between Hambusimaloso and Hahala is therefore a priority drill target. The Company will visually assess the result of MB03 prior to drilling further holes at this location or moving the rig to Hahala. At Hahala, 1.1 kilometres to the north north east of the Hambusimaloso North drill hole MB03, the Company has outlined a high priority gold drill target, 400 x 400 metres and open to the north, coincident with a porphyry style aeromagnetic signature, strong gold values in soil samples and outcropping intrusive porphyry rocks. Field mapping and sampling is continuing with extensions of the soil sampling lines to the north and west of the Hahala and the nearby Upper Chipakalau area, prior to drill testing. At Vuralanggoma, 5 km east of Hambusimaloso, float samples of epidote skarn rocks rich in visible zinc and copper minerals sphalerite and chalcopyrite, have been located and these samples assayed up to 9.8% copper. Although the outcrop location of this material is not yet identified, the mineralisation, based on soil sampling, occurs over a 300 x 500 metre zone. Previous drilling by Utah in the 1970s yielded 38m at a grade of 0.34% copper in volcanic agglomerates overlying and intruded by a diorite porphyry complex. The hole also intersected a narrow zone of fractured and mineralised porphyritic diorite, grading 1.0% copper at a depth of 208 metres. No gold assaying was undertaken. Regional outcrops Strong gold anomalism in the soil sampling grid has been outlined by Solomon Gold and it is intended that the Company drill test this anomaly, and the copper zone located immediately west of the old Utah holes following completion of the soil sampling grids in the area. In addition, infill soil sampling lines are planned over the 200 metre spaced soil sampling grid at Vurakuvekuve, south east of Hambusimaloso, to further delineate NE trending copper - molybdenum anomalies which may signify porphyry sources to the widespread Mbetilonga mineralisation. Future soil sampling lines are planned to infill the area between Vatuchichi and Hahala and between Vuralanggoma and the nearby Vuralosa prospect. Solomon Gold management considers that soil sampling is providing the best guide to the centre of the mineralising system. Sutakiki (PL05/05) At Sutakiki, initial reconnaissance mapping and sampling which commenced on 1st June, has revealed a large intrusive porphyry system mineralised with copper and gold. The system commences 200 metres upstream from the last sampling conducted by Newmont geologists in 1988 and continues upstream in a south-westerly direction for approximately 2 km, in a drainage basin approximately 2 km wide. The mineralisation is frequently but irregularly exposed and 5 metre rock chip channel samples across the mineralisation and any apparent structures were taken where possible. Sixty - two samples from the central zone of mineralised outcrops along the Sutakiki River have been assayed to date and results received (refer discussion below). Assaying of a further 87 rock chip, 33 stream sediment and 75 orientation soil samples has been expedited and the results are are awaited. These samples will provide reconnaissance results over the bulk of the area of the drainage basin at the head of the Sutakiki River. The style of the mineralisation is a classic south west pacific copper gold mineralised quartz hornblende diorite porphyry system with overprinted fault controlled second and third phase epithermal quartz vein systems. The area is roughly coincident with an extensive zone of diagnostic geophysical signatures in magnetic and radiometric surveying conducted in 1997 by Australian Resource Management (A.R.M.) Pty Ltd, a wholly owned subsidiary of Solomon Gold. The faults host quartz veins yielding values up to 35.9g/t gold and 22.4 g/t silver based on assaying to date. Composite 5 metre channel samples of mineralised outcrop show up to 5.17g/t gold. Up to 85 metres at 0.79 g/t gold and 0.15% copper was sampled from the best exposed section of mineralisation in the upper Sutakiki River. Copper results range up to 0.99%. The porphyry system outcrops in the head of the Sutakiki Valley and is surrounded by overlying altered andesitic volcanics which show skarn mineralisation containing visible copper, lead and zinc sulphide mineralisation. The epithermal textures of the late stage quartz veins, proximity of the overlying volcanics, copper to gold ratios and high tellurium assay results suggest that outcropping rocks are positioned high in the intrusive system and better copper and gold grades are likely to be encountered at depth within the intrusive complex. On the basis of these results and the presence of high order gold mineralisation in the head of the Koloula Valley four kilometres to the south south west of the current south western extent of the sampling at Sutakiki, Solomon Gold believes the area covers an extensive intrusive system hosting widespread gold mineralisation. Solomon Gold intends to expedite the drill testing of the most obvious gold mineralised zones at Sutakiki as soon as possible. Kuma (APL) Access negotiations at Kuma are continuing. Central (PL03/05) The discovery of the mineralisation associated with the intrusive complex at Sutakiki has led to the identification of exploration targets in the area approximately 8 km south west of the Gold Ridge Mine. These targets are coincident with magnetic features suggestive of skarn mineralisation adjacent to an intrusive complex. General Solomon Gold now has 10 contractors and staff geologists working on two rosters on its projects on Guadalcanal and is well supported by local field workers with whose communities the Company maintains a close relationship. With the re - equipped drilling rig and revised contract, drilling rig and more powerful helicopter Solomon Gold is planning to complete 10,000 metres of drilling on the Mbetilonga, Koloula and Sutakiki project areas over the next 12 months. Subject to the outcome of access negotiations and reconnaissance mapping and sampling which would follow, drilling activities at Kuma to the south east of Sutakiki may also be considered. A complete copy of this update may be viewed with a map on the Company's website www.solomongold.com . Contact : Abigail Singleton or Leesa Peters, Conduit PR +44 207 429 6666 Nicholas Mather, CEO or Duncan Cornish ( Secretary )Solomon Gold plc +61 7 33030680 This information is provided by RNS The company news service from the London Stock Exchange

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