Gateway Mining Limited reported significant new results from the recently completed reverse circulation (RC) drilling program around the Whistler Gold Deposit, within the company's 100%-owned Gidgee Gold Project in Western Australia. This drilling program was designed to undertake a first-pass assessment along strike to the north and south of the Whistler Gold Deposit to understand the potential to significantly grow the current resource. The drilling targeted both the main granodiorite-hosted gold mineralisation and the hanging wall mafic-hosted lode system. The drilling at Whistler formed part of a large 11,000m RC drilling campaign undertaken over several targets at Gidgee, which included both the recent discovery of an extensive zone of shallow oxide gold at Achilles and the expansion of the Montague Gold Deposit. Whistler South: A total of 18 holes for 2,110m of reverse circulation (RC) drilling were completed to test for continuity of gold mineralisation south of the current Whistler Resource and to provide key information on the broader structural and stratigraphic controls in the area to assist with the ongoing exploration targeting process. The South Whistler trend has now been defined in shallow positions over a strike length of at least 500m and is hosted on or near the margin of the Montague Granodiorite intrusion, which is the same setting as the Whistler Gold Deposit. The South Whistler trend is a distinctly separate gold mineralised structure and is offset approximately 100m to the east of the Whistler main structure. It is worth noting that the main Whistler structure has to date, not been closed off. Key results that currently define this gold mineralised trend are: GRC482: 13 metres @ 1.6g/t Au from 58 metres, GRC480: 5 metres @ 1.0g/t Au from 23 metres, 86MORC41: 6 metres @ 1.9g/t Au from 28 metres (Bottom of hole) and C87RB103: 6 metres @ 1.7g/t Au from 12 metres (Bottom of hole). The shallow gold mineralisation remains open down-dip and along strike to the north and south, and as seen at Whistler, there is considerable scope for high-grade domains to be delineated within this broader mineralised domain. It should be noted that mineralised intersections such as that returned in hole GRC482 (13m @ 1.6g/t Au) are common within the current Whistler Resource and can occur in close proximity to substantially higher grade zones. The position of the Whistler South mineralisation is in close proximity to the edge of the current optimised Whistler open pit shell and any future expansion of the resource would be easily captured. Whistler North: The 14-hole (1,975m) RC drilling program at Whistler North was designed to: Test the immediate northern strike extension to the current Whistler Resource; Provide key information regarding the orientation of the plunging nose of the Montague Granodiorite and confirm the geological analogy to the 3.1Moz King of the Hills deposit (owned by Red 5); and Provide a further test to delineate and understand the controls on the multiple hanging wall lode structures hosted within the mafic volcanic rocks. Significant intersections include: GRC398: 7 metres @ 1.0g/t Au from 53 metres, GRC397: 2 metres @ 3.6g/t Au from 62 metres, GRC400: 10 metres @ 1.0g/t Au from 43 metres, GRC454: 5 metres @ 2.1g/t Au from 25 metres, GRC402: 6 metres @ 1.5g/t Au from 43 metres, 88MRD24: 12.5 metres @ 2.2g/t Au from 128 metres and GRC378: 5 metres @ 2.8g/t Au from 138 metres. Drill holes GRC3978 (7m @ 1.0g/t Au) and GRC397 (2m @ 3.6g/t Au) successfully intersected the mineralised structure north of the current Whistler resource. These holes are interpreted to have intersected the top of the northern plunging high-grade domain. This significant zone of high-grade mineralisation remains open down-plunge to the north. Drill hole GRC454 (5m @ 2.1g/t Au) intersected the Whistler structure within the mafic volcanic rock stratigraphy above the granodiorite contact. The intersection of the structure with the contact of the granodiorite remains untested and is considered to be a highly prospective target. The recent drilling results from the Whistler area continue to demonstrate the emergence of a large-scale gold system within a structural corridor on or close to the margin of the Montague Granodiorite. Significant mineralisation has now been intersected over a strike length of at least 900m. In addition, the information gained from the drilling program continues to provide invaluable structural and stratigraphic data that is critical for ongoing exploration and resource delineation in the area. Armada Prospect: The Armada Prospect is located approximately 500m to the north-west of the Whistler Resource area. Historical drilling has intersected zones of relatively shallow, oxide gold mineralisation along what is interpreted to be the contact of the Montague Granodiorite. The target position is analogous with the setting of the Montague Gold Deposit, located approximately 1.6km to the south. The recent RC drilling program (6 holes for 605m) was undertaken to provide a first-pass test beneath the supergene gold mineralisation for primary shear zones within the mafic volcanic rock stratigraphy. Significant drilling results include: GRC412: 2 metres @ 3.4g/t Au from 68 metres and: 3 metres @ 1.3g/t Au from 78 metres, GRC413: 2 metres @ 1.1g/t Au from 69 metres, GRC414: 2 metres @ 2.9g/t Au from 83 metres. The results have confirmed the presence of bedrock shear zones within the mafic volcanic rocks on the margin of the granodiorite. This information will be integrated with geophysical datasets and follow-up exploration will be planned accordingly.