Aston Bay Holdings Ltd. announced the final results of its recently completed drill program at the Buckingham Gold Project located in central Virginia, USA. Six large diameter (HQ) diamond drill holes totaling 878 metres (m) were completed in April, with partial results from quartz veined intervals previously reported. Results from the remaining portions of the drill holes are presented here. All six drill holes intersected significant near-surface gold mineralization, either in quartz veins or in wider zones of sericite-quartz-pyrite alteration. As previously released, three drill holes intersected significant gold mineralization in quartz veins, including 35.61 g/t Au over 2.03m in hole BUCK19-001, 20.44 g/t over 3.30m and 34.25g/t over 0.5m in hole BUCK19-003, and in hole BUCK19-004 24.73 g/t over 3.57m including 62.51 g/t over 1.39m. Most significant of the new results, BUCK19-005 intercepted two broad zones of gold mineralization associated with sericite-quartz-pyrite alteration: 2.16 g/t Au over 18.07m including 17.45 g/t Au over 1.57m and 1.90 g/t Au over 22.22m including 19.30 g/t Au over 1.5m. This hole is a 40 m step-out along strike from previous drilling. All mineralized intercepts are located below sub-cropping quartz containing visible gold that have yielded up to 701 g/t Au (20.4 ounces Au per short ton) in surface grab samples. Based upon multiple vein intersections, the estimated true width is 80% of the core interval. The new assay results are based upon a standard 30g Fire Assay with an AA (Atomic Absorption) finish from halved HQ core for the mineralized intervals; previous results for quartz veins are based upon one kilogram pulp metallic screen analyses. The current drilling targeted an area in which visible gold had been identified and sampled, followed by a limited but successful drilling completed by a previous owner. That previous program consisted of three holes on the Buckingham Property, all of which intersected significant gold, including 15.57 g/t Au over 4.1m and 11.69 g/t Au over 3.1m. In addition to gold-bearing quartz veining, the previous drilling intersected a zone of sericite-pyrite alteration yielding 0.4 g/t Au over 24m including 0.71 g/t Au over 13.72m (all historic intercepts are core intervals, i.e., not true width; see March 4, 2019 Aston Bay press release). The current drill program was designed to test along strike and down dip from the northwest-southeast trending area of boulders and sub-crop of quartz veining, as well as test for zones of gold-bearing alteration. The gold-bearing system is hosted within a package of likely Cambrian-age sediments, including greywackes with minor quartz-arenites (phyllite, schist and quartzites), within the Appalachian orogenic belt. This region is the site of the historically prolific Pyrite Belt which hosted a reported 250 gold mines that were in production prior to the California gold rush of 1849 but has seen little recent mineral exploration. Gold production has also occurred to the south in the Carolina Slate Belt, notably at Oceana Gold's Haile Mine located in South Carolina with commercial production commencing in 2017 and slated to produce up to 150,000 ounces of gold per year. Samples from the Company's 2019 Buckingham drill program were shipped for analysis at the ALS Laboratory in Reno, Nevada. A secure chain of custody was maintained, and the program included a comprehensive QAQC program, which did not identify any analytical issues.