Golden Birch Resources Inc. provided detailed information on its recently discovered Waki Prospect located east of the Omu Prospect. Initial discovery of the Waki Prospect made by Golden Birch geologists in May 2019. Reconnaissance exploration by Golden Birch geologists yields visual copper mineralisation in float and outcrop 1 kilometre ("km") east of Omu Prospect. Exploration results yield anomalous copper and gold, with best results to date from separate outcrops being 0.34% Cu and 15.5 g/t Au and 4.9% Cu and 0.05 g/t Au. Assay values from selective rock float samples in drainages associated with Waki Prospect area yields values as high as 6.8% Cu and 15.45 g/t Au from separate samples. Exploration at Waki is at an early stage and assay values from in situ outcrop and float samples are selective in nature and therefore not representative of the overall target at Waki. Further work is required before a representative grade for copper and gold can be determined for the Waki Prospect. Waki Prospect has yielded anomalous copper and gold mineralisation in multiple in situ outcrops and selective float samples over an area of approximately 1.0 km north-south by 0.8 to 1.0 km east-west Wide spaced, reconnaissance soil survey yields anomalous and coincident copper (Cu), gold (Au) and molybdenum (Mo) values over a 400 metre to 600 m north-south by 800 m to 1000 m east-west area. The Cu-Au-Mo anomalies are coincident with an airborne magnetic "high" anomaly. A total of 71 rock samples were obtained from the Waki Prospect for analytical and petrological investigations during the initial geologic mapping campaign. Geologic mapping to date at the Waki Prospect has confirmed strongly fractured porphyry-style intrusive rocks, hydrothermal alteration as characterised by porphyry deposits being chlorite, epidote and secondary hydrothermal magnetite with phyllic (quartz+sericite+pyrite) overprint. Some of the samples from creeks and outcrops display visible supergene-hypogene copper mineralization (chalcopyrite and malachite). Results of the geological mapping are illustrated.