Goldplay Mining Inc. announced results from its 2021 field program on the Big Frank Project, located in southwestern British Columbia approximately 285 km north of Vancouver, withlogging road access to the western Project area. The Project was optioned by Goldplay in late August, 2021. The Project is a prime target for newdiscoveries based on more extensive exposure of favourable alteration and gossans due torapidly diminishing glacier cover in an area with known porphyry copper and gold-bearingshear/vein type mineralization.

The September 2021 field exploration program (the "Program")focused on an initial examination and evaluation of the Hoodoo North and Hannah porphyryprospects, the Discovery and Conductor F gold zones at Hannah, and the margins of the Darlenegold bearing polymetallic vein and skarn showing and follow up of a 1988 gold-silver talus fineanomaly in the Confederation Glacier area. A total of 104 rock and 165 soil/talus fine samples were collected by 4 geologists across the 20km long Project during the Program. Soil sampling in 2021 focused mainly on newly exposed areas (due to glacial retreat) to the northand northwest of the Hannah prospect.

The 1 by 1.2 km historical Hannahcopper±molybdenum±gold porphyry soil anomaly was extended approximately 400m to thenorthwest with values ranging from negligible to 243 ppm Mo and 0.57% Cu (average of 52 ppmMo and 0.064% Cu).Hannah Prospect Gold Zones2021 sampling of the Discovery zone confirmed significant previous gold results from shear/veinhosted mineralization yielding 3.06 g/t Au over 3.1m, including 5.72 g/t Au over 1m, from 1988historical Trench 2 and grab samples of 17.1 g/t with 4.76% Cu, and 7.05 g/t Au with 1.59% Cufrom the face of the exposure. Eight grab samples from similar style mineralization at theConductor F zone, 350m to the west ranged from 1.25 to 37.3 g/t Au, locally with high silver to 174 g/t and copper to 4.25%. Two chip samples from theincomplete exposure at 1988 historical Trench 3 at this location yielded lower results of 0.45 g/tAu over 1.8m.

The mineralization at both zones is generally accompanied by extremely highbismuth (to 5077 ppm) and significant silver and copper. Additional conductors were obtainedin the 1988 geophysical survey which remain untested.Other quartz vein zones were grab sampled by Goldplay within the Hannah porphyry alterationzone which returned significant gold results with similar geochemistry as above ± significant tohigh tellurium (21.59 ppm). Values of 5.45 g/t Au, and 1.12 g/t Au were obtained 500mnorthwest and 800m north of the Discovery zone and another vein zone about 2 km north of theDiscovery zone contained 1.96 g/t Au, 70.8 Ag, 2.75 Cu and 15 ppm bismuth.Goldplay discovered a 30 cm quartz-sulphide vein containing 16.0 g/t Au with 1162 g/t Ag, 0.68%lead and 0.09% zinc ("Darlene South") south of the previously known Darlene skarn/polymetallicvein showing in the northwestern Project area.

Three additional samples of smaller veins alonga 400m northerly trend returned 0.122 to 0.369 g/t Au with elevated silver, zinc, ± lead. Thisdiscovery may represent the southern extent of the source of polymetallic vein float from whichthe British Columbia Geological Survey obtained 15.5 g/t Au near the Darlene silver-lead veinshowing. Additional veins were noted, having been exposed by receding glaciers, which will besampled during the 2022 field program.Scattered soil samples through the Darlene South area returned >0.1 to 1.46 g/t Au withanomalous silver, lead, zinc, ± bismuth.

The anomalous soils may represent part of a much largergold anomaly emerging at the edge of an ice field. A 200 by 650m >0.1 to 13.5 g/t Au soil anomaly lies about 700m to the south, with the same geochemical signature except ± tellurium.Extensive quartz veining was encountered within this soil anomaly yielding low anomalous goldvalues of 0.1 to 0.54 g/t Au, also accompanied by significant silver, bismuth, commonly telluriumand occasional zinc. Veins continue to the south but are less extensive with lower gold.Follow up of a 1988 historical three station gold-silver talus fine anomaly of 1.24 to 1.55 g/t Auwith 4.8 to 11.2 g/t Ag in the Confederation Glacier area led to the discovery of a strong, variablyaltered zone of clay-sericite and locally strongly silicified Miocene feldspar porphyry about 250mupslope. A weakly brecciated clay-sericite altered sample with oxidized cubic pyrite yielded 5.5g/t Au.

A gold in talus fine anomaly of >0.065 to 2.68 g/t Au (average of 0.91 g/t Au from 14samples) extends for 300m below the alteration zone and directly uphill of the historical anomalyand is open in both directions. A number of sporadic gold (>0.1 to 0.81 g/t) and copper (>0.1 to0.33%) in soil values with 0.42 and 0.23% Cu in quartz-sulphide veins lie 400m to the west-northwest of the talus fine anomaly.All samples were sent to MS Analytical Laboratories ("MSALabs") in Langley, British Columbia forsample preparation and analysis. At the laboratory, rock sample preparation involved drying, finecrushing to better than 70% passing minus 2 mm, then pulverizing a 250g split to better that 85%passing 75 microns (PRP 910).

Soil sample preparation involved drying and screening to minus 80mesh (PRP-757). For the rocks the fine fraction was analyzed for gold by fire assay on a 30g aliquotwith an atomic absorption spectroscopy ("AAS") finish (FAS-111), and for 48 additional elementsby four acid digestion and inductively coupled plasma ("ICP") - mass spectroscopy ("MS") ultratrace level analysis (IMS-230). The fine fractions of the soils were analyzed for 39 elements,including gold, by aqua regia digestion and ICP-atomic emission spectroscopy ("AES")/MS ultratrace level analysis on a 20g aliquot (IMS-128).