Mawson Gold Limited announced drill results from the final 36 drill holes totaling 8,756.5 metres from the Company's 76 hole, 19,422 metre 2020/21 drill program at the Company's 100%-owned Rajapalot gold-cobalt project in Finland. Gold and cobalt assay results are reported here from the final 36 drill holes totaling 8,756.5 metres from the 2020/21 drill program. In total, since drilling commenced in September 2020, Mawson has drilled 76 drillholes for 19,422 metres. All holes released in this and earlier news releases on Nov. 10,2020, Nov. 18, 2020, Nov. 25, 2020, Dec. 21, 2020, Apr. 12, 2021, Jun. 29, 2021, Jul. 13, 2021 and Aug. 03, 2021. Intersections are reported with a lower cut of 0.3 g/t AuEq over a two metre lower cut. No upper cut-off was applied. Higher-grade intersections use a 1.1 g/t AuEq lower cut over two metres. A resource upgrade at Rajapalot is scheduled during August 2021. Four diamond drill rigs from Kati Oy, Nivalan Timanttikairaus Oy and MK Core Drilling Oy all with water recirculation and drill cuttings collection systems are used in the drill program. Core diameter is NQ2 (50.7 mm). Core recoveries are excellent and average close to 100% in fresh rock. After photographing and logging in Mawson's Rovaniemi facilities, core intervals averaging 1 metre for mineralized samples and 2 metres for barren samples are cut in half at the Geological Survey of Finland (GTK) core facilities in Rovaniemi, Finland. The remaining half core is retained for verification and reference purposes. Analytical samples are transported by commercial transport from site to the CRS Minlab Oy facility in Kempele, Finland. Samples were prepared and analyzed for gold using the PAL1000 technique which involves grinding the sample in steel pots with abrasive media in the presence of cyanide, followed by measuring the gold in solution with flame AAS equipment. Samples for multi-element analysis (including cobalt) are pulped at CRS Minlab, then transported by air to the MSA labs in Vancouver, Canada and analyzed using four acid digest ICP-MS methods. The QA/QC program of Mawson consists of the systematic insertion of certified standards of known gold content, duplicate samples by quartering the core, and blanks the within interpreted mineralized rock. In addition, CRS inserts blanks and standards into the analytical process. The host rocks to the gold and cobalt mineralization comprise sulphides (pyrrhotite>>pyrite) with biotite-muscovite-chlorite schists and Mg-Fe amphibole-biotite-chlorite rocks. Veining and fracture fill minerals include pyrrhotite, magnetite and magnetite-pyrrhotite (+/-quartz, tourmaline). Retrograde chlorite after biotite, generations of secondary muscovite ("sericite") and vein-controlled chlorite+/-tourmaline and magnetite are also present. Preliminary hand-held XRF analysis confirms the presence of associated scheelite and molybdenite, the former visible under UV light as tiny veinlets and disseminations. The silicate mineral alteration assemblages associated with the gold are clearly post-metamorphic, reduced, and most likely driven by hydrothermal fluids from nearby granitoid intrusions. Chlorite and fine muscovite are regarded as the lowest temperature silicate minerals with gold, structurally controlled in apparent spatial association with quartz and/or K-feldspar veins. Altered rocks enclosing the mineralized package contain locally abundant talc and tourmaline.