Bryah Resources Limited announced that it has received assay results for drilling completed at its Bryah Basin Olympus copper gold project. Bryah was granted $130,000 in round 24 of the Western Australian Government's EIS (Exploration Incentive Scheme) to undertake a 2,000m RC drilling program to test the Olympus geochemical anomaly on the northern limb of the Mars Dome. The program completed 9 holes totalling 2,148m.

The EIS co-funded RC drilling program includes 9 holes drilled across the full strike length of the Olympus Soil Geochemical Anomaly. These holes were drilled on five 320m spaced lines with some sections containing multiple holes to provide stratigraphic section. A total of 2148m of RC drilling was completed in June/July 2022.

Olympus lies on the Northern limb of the Mars Dome, which forms part of a series of double- plunging anticlinal dome structures in the northern Bryah Basin. This is termed the Aquarius trend and consists also of the Saturn and Jupiter Domes to the north-west. These dome structures connect laterally with outcropping Narracoota Formation to the northeast through a series of possible covered dome and basin structures.

Reverse Circulation drilling at Olympus has so far identified a downhole pathfinder anomalous zone with copper-gold potential in the stratigraphic footwall. Drilling has identified numerous lithofacies, textures, mineralogy, alterations, and styles of mineralisation that are typical of high sulphidation VMS deposits such as the nearby Horseshoe Lights Cu-Au mine. Highlight observations include: Identification of a spatially coherent Pb-Bi-Mo-(Cu-Zn-Te-Se) anomaly approaching the hanging wall contact to mineralised stratigraphic horizon.

This level of enrichment is also observed in the hanging wall volcaniclastics at Windalah. Observation of semi-massive sulphide mineralisation. The most significant intercept of sulphide mineralisation includes 1m @ 33 wt% pyrite.

Some chips of semi-massive pyrite appear to show a fine-grained, granular texture - a distinctive textural feature of the Windalah and Horseshoe Lights massive sulphide. Reverse Circulation drilling at Olympus has identified a geochemical pathfinder enrichment similar to that observed in the hanging wall transition facies stratigraphy at the Windalah Cu-Au prospect. These pathfinder elements, especially Pb, Bi, Te, and As, suggest there is potential for a Windalah- style massive sulphide system in the stratigraphic footwall to the current limit of drilling at Olympus.

This will be the target of further drill campaigns. This enrichment forms a spatially coherent, vaguely stratiform multi-element anomaly in the hanging wall to observed sulphides and approaching the interpreted mineralised stratigraphic horizon. A similar spatial distribution of enrichment in hanging wall volcanics observed is considered encouraging and may imply a similar hydrothermal system.