Grizzly Discoveries Inc. announced that it has recently received analytical results for an additional 18 selective rock grab samples from the historical Silver (Ag)-Gold (Au)-Lead (Pb)-Zinc (Zn) Midway Mine area and 90 selective rock grab samples from 10 km north of Midway at the Copper Mountain Prospect in the Central portion of the Greenwood area, about 4 km and 14 km northwest of the town of Midway in the Kettle River Valley area of BC, respectively. The Midway - Picturestone mineral claims were recently acquired from Mr. Dan Hurd and are strategically located within the Company's Central Greenwood land holdings and in particular the Company's Midway to Copper Mountain lands. Assaying was conducted at ALS Global in Vancouver with each sample analysed for gold by a standard fire assay (Au-ICP-21), which involved the fusion of a 30 g sample aliquot and a wet chemical (ICP) finish.

"Overlimit" Au-ICP21 results (>10 g/T Au) were followed up with Au-GRA21 analysis. This involved a 30 g fire assay fusion and gravimetric finish. Additionally, each sample was submitted for multi- element geochemical analysis by the ME-MS61 technique, which is an ICP-MS analysis following a near-total, four-acid, digestion of a 0.25 g sample aliquot.

Initial silver and base metal (Cu, Pb and Zn) "overlimit" ICP-MS results (>100 g/T Ag and >1% for base metals) were analysed by a follow-up, "ore grade" ICP technique (OG62), which also involved ICP analysis following a four-acid digestion on a 0.4 g sample aliquot. Any samples with silver values by OG62 >1,500 g/T were re-analysed by 30 g fire assay with a gravimetric finish (Ag-GRA21). ALS Minerals has developed and implemented strategically designed processes and a global quality management system at each of its locations that meets all requirements of International Standards ISO/IEC 17025:2017 and ISO 9001:2015.

The Midway Mine and the Picturestone (aka Picture Rock) Quarry area have seen intermittent exploration and mining since the late 1800's through to as recent as 2012. In the case of the historical Midway Mine, limited underground and open pit development has occurred. The Midway Mine and the Picturestone Quarry are situated within the "Midway Window", a structural zone within the Toroda Graben exposing Late Paleozoic to Jurassic sediments, volcanics and intrusions, including the Knob Hill and Brooklyn formations, centered on an old thrust fault in a similar setting to the Golden Crown and Lexington Mine area near Greenwood, BC as displayed in Figure 1. The presence of serpentinite and listwanite in a thrust fault setting along with what is likely Jurassic aged quartz-feldspar porphyry and diorite has been noted.

The Company's Midway Lands have been a focus of exploration since acquiring lands in the area. The current status of historical and modern exploration by the Company is illustrated in Figure 1, with most of the recent work focused on lands to the west and southwest of the historical Midway Mine. Prior owners and operators describe significant epithermal mineralization in the form vertical polymetallic sulphide veins enriched in pyrite, arsenopyrite, galena, sphalerite and stibnite, quartz veins and significant alteration at the Midway Mine and Picturestone Quarry.

The Midway Mine is spatially associated with a northeast trending gold (Au), silver (Ag), lead (Pb), zinc (Zn) and arsenic (As) soil geochemical anomaly that is approximately 300 m in length and 100 m in width in the area of the Midway Mine. Historical trench sampling yielded 2.8 grams per tonne (g/t) Au and 218 g/t Ag over a 4.5 m interval in chip/channel sampling at the Midway Mine. Limited drilling with some significant intercepts was carried out in the 1980's to 1990 at the Midway and Picturestone prospects.

Minnova Inc. conducted a 7 hole core drilling program for a total of 1,170 m 1990 in the Midway Mine area2. No drilling has been conducted since. A total of 274 m of core was sampled and two holes tested the actual historical Midway Mine.

Hole 90-1 drilled to a depth of 84.45 m intersected 23 m of altered quartz-feldspar porphyry with pyrite and some pyrite-galena veins. The best result obtained in sampling was 1.14 g/T Au (0.033 oz/t Au) and 208 g/T Ag (6.1 oz/t Ag) over 1.5 m core length. A 10.5 m interval of strongly altered quartz-feldspar porphyry returned an average grade of 0.33 g/T Au (0.001 oz/t Au) and 52.7 g/T Ag (1.54 oz/t Ag).

A number of the drill holes completed intersected serpentinite, listwanite, diorite and then bottomed in Triassic Brooklyn Formation sharpstone conglomerate with pyrite and skarnified limestone clasts. A number of the other holes intersected similar geology, alteration and gold - silver values as hole 90-1. Additional trenching and drilling were recommended. The most recent work in 2012 resulted in a recommendation of ground geophysical surveys, additional soil sampling and drilling.

The work was never completed. The Company and APEX have commenced permitting for a number of other target areas, including drilling and trenching at Sappho, Midway and Copper Mountain.