SAPPHO

The Sappho prospect, on which the Company conducted extensive exploration in 2009 and 2010, has yielded strong evidence of copper-gold-silver-platinum-palladium (“Cu-Au-Ag-PGE”) alkalic porphyry mineralization.   Exploration at the Sappho zone has resulted in numerous high grade samples from the historic workings.  However, the nature of its origin and the surrounding geology is not fully understood. The remaining area of the Sappho claim block is relatively underexplored compared to the extensive work at the main showings.

Three well documented surface copper occurrences in the northeastern portion of the complex yielded numerous high grade selective grab sample results including up to 8.28% copper (“Cu”) 298 grams per tonne (“g/t”) silver (“Ag”), 2.2 g/t gold (“Au”), 27.1 g/t Platinum (“Pt”) and 2.57 g/t palladium (“Pd”). All three occurrences yielded multi gram Pt and Pd values.  The Sappho prospect is unusual relative to most British Columbia platinum group elements-bearing alkaline intrusive complexes, in that it contains Pt concentrations greater than Pd and Au.  As reported in the Technical Report, government geologists have conducted extensive geochemical and mineralogical work on the Sappho alkaline complex and associated Cu-Ag-PGE-Au mineralization and, based upon textural and geochemical evidence, suggest that the mineralization is late magmatic or magmatic-hydrothermal in origin and bares mineralogical traits most common in alkaline porphyry style associated metals.

A drill program conducted by the Company in 2010 targeted two showings at the Sappho prospect, the Main and Northern showings, with a drillhole beneath each showing and two additional drillholes testing two proximal blind magnetic features with no previously known mineralization. The two holes beneath the Sappho Main and Sappho North showings intersected weak but anomalous Cu-Ag-PGE-Au. The best intersection was provided by drillhole 10SP03, which targeted a blind magnetic anomaly close to the Bodie Mountain fault and yielded a wide anomalous interval of 0.28% CuEq over 93.5 m core length including a higher grade zone of 0.38 % CuEq over 63.5 m core length that is comprised of 0.12% Cu, 8.68 g/t Ag, 0.22 g/t Au, 0.10 g/t Pd and 0.07 g/t Pt. This wide anomalous interval contains two higher grade intervals, an upper and lower zone, which yielded 1.43% CuEq over 7 m and 1.04% CuEq over 6.5 m core length, respectively. The mineralization in drillhole 10SP03 is hosted in a wide and intensely hornfelsed to skarnified pyroxenite that is brecciated and silicified in places. Hornfels alteration consists of biotite-garnet-magnetite and is associated with abundant pyrite and chalcopyrite.  Further drilling will be required to follow up on the results of 10SP03.

• The Sappho area is being targeted for copper-gold-PGEs skarn and porphyry type targets associated with an alkalic intrusion and several diorite intrusions south of Greenwood near the US border.
• At least five new showings of copper oxide/sulphide mineralization were found during the 2022 program at the Sappho Target.
• Previous surface sampling and drilling by Grizzly at the Sappho area has yielded significant anomalous copper, gold, silver along with platinum and palladium.
• Numerous rock grab samples have yielded greater than 1% copper, 1 g/t gold, 1 g/t platinum and 1 g/t palladium. The sampling work in 2022 yielded 17 rock grab samples with >1% Cu up to 9.06% Cu.
• Historical drilling (by the Company) has yielded up to 0.31% Cu, 0.75 g/t Au, 0.34 g/t Pt, 0.39 g/t Pd and 6.57 g/t Ag over 6.5 m core length in skarn at Sappho in 2010.

Mineralization at Sappho 2022

Copper bloom at the Main Sappho Adit Showing

MOTHERLODE

Motherlode was first staked and explored in 1891, with commercial production commencing in 1901. The mine and smelter closed in 1918 due to decreasing ore grades. Woodgreen Copper Mines Ltd. put the Motherlode Mine back in production in 1956 as an open pit operation, and operated the mine until 1962, at which time it was permanently closed.

The historic Motherlode underground and open pit mine produced close to 175,000 ounces of Au, 700,000 ounces of Ag and 77 million pounds of Cu at an average grade of 1.27 g/t Au, 5.04 g/t Ag and 0.82% Cu from a skarn between 1900 and 1962 (British Columbia Minfile 082ESE034).

A total of 1,722 m in nine core holes was completed at Motherlode North, approximately 500 to 750 m north of the historical Motherlode copper-gold-silver mine and 387 m in two core holes were completed at the Marguerite Target as part of the 2022 Phase 1 drilling program. The Company announced final results from 2022 exploration drilling at Motherlode North, with the following highlights:

• The Motherlode North polymetallic and skarn targets are comprised of copper-gold-silver +/- lead-zinc (Cu-Au-Ag +/- Pb-Zn) targets 500 to 750 m north and northeast of the historical Motherlode Mine (not owned by the Company), which produced significant amounts of Cu, Au and Ag including 173,000 ounces (oz) of Au, 688,000 oz of Ag and 77 million lbs of Cu between 1896 and 1918 and 1956 to 1963 (BC Minfile 082ESE034).
• Prior drilling by Grizzly intersected up 17.15 g/t Au, 41.7 g/t Ag, along with, 0.56% Pb and 1.51% Zn over 1.5 m core length at one of the skarn targets north of the Motherlode Pit.
• Skarn and sulphide rich mineralization, along with widespread hornfels and propylitic alteration have been intersected in most of the 2022 Motherlode North (22ML07 to 15) and the two (22MR01 & 02) Marguerite core holes.
• Final assay results for the nine Motherlode holes have yielded anomalous Au, Ag, Cu, Pb and Zn in every hole with a best high-grade sample of 5.86 g/t Au and 6.36 g/t Ag over 1 m core length along with several wide low grade intersections in particular adjacent to porphyritic intrusions in Triassic sulphide rich hornfelsed or skarnified Brooklyn sedimentary rocks.
• A number of the Motherlode North holes have yielded wide low grade Au-Ag+/-Cu-Zn intersections such as hole 22ML07 with 0.415 g/t Au, 2.19 g/t Ag, 0.019% Cu and 0.08% Zn over 17.56 m core length, along with hole 22ML08 with 0.108 g/t Au, 2.43 g/t Ag, 0.013% Cu and 0.059% Zn over 11.09 m core length and 0.332 g/t Au, 2.63 g/t Ag and 0.053% Zn over 15 m core length, interpreted to be part of a large alteration footprint in a well mineralized skarn-porphyry system.
• The porphyritic intrusions are widespread and are likely Cretaceous or Eocene in age. Sulphide mineralization with anomalous geochemistry appears to be spatially associated with these intrusions.
• The two holes in the vicinity of the Marguerite historical shaft intersected near surface skarn with anomalous Au-Ag-Cu and deeper hornfelsed sediments and breccias that are silica-sulphide rich and with widespread anomalous Cu over 50 to 100 m in thickness (Holes 22MR01 and 02). The deeper mineralization is associated with propylitic alteration and potentially could highlight deeper copper-gold porphyry potential beneath the Motherlode area skarn system.
• Holes 22MR01 and 22MR02 returned upper skarn related zones of 0.442 g/t Au, 5.61 g/t Ag and 0.028% Cu over 5.32 m, and 0.227 g/t Au, 4.36 g/t Ag and 0.037% Cu over 9.5 m core length.
• The lower highly anomalous copper-gold rich zones are highlighted by 0.123 g/t Au, 2.06 g/t Ag and 0.127% Cu over 8 m core length in hole 22MR02, but this is contained within a 46 m wide zone to the end of the hole where all but 4 of 45 samples yielded >100 ppm Cu up to 1,980 ppm Cu.
• Similarly, in hole 22MR01, there is lower zone of copper rich mineralization that is 119 m in thickness to the end of the hole where 80 of 116 samples yielded >100 ppm Cu up to 1,600 ppm Cu.
• Although low grade, the wide highly anomalous intersections of low to moderate grade gold and copper are likely indicative or part of a large mineralized hydrothermal system.

Motherlode North & Marguerite 2022 Drill Program

COBALT REVIEW

During late 2017, the Company performed an initial review to see if its land holdings were prospective for the presence of cobalt (Co). The strategic review identified the presence of at least 13 rock grab samples with greater than 0.05%, including up to 0.10% Co, from at least five separate target occurrences across the eastern half of Grizzly's Greenwood Project area. The database shows an additional 31 rock grab samples that have yielded assays of between 0.02 and 0.05% Co. Maps showing the anomalous values and locations for Co at the Greenwood Project:

A preliminary review of the sample database indicates that many of the rock samples with anomalous Co also contain anomalous values for Cu and precious metals including Au and Ag. In many cases, the samples with anomalous Co were collected from Cu-enriched skarn and hornfels developed in Paleozoic sediments and intrusions, where the original sampling targeted precious metals. Grizzly has initiated a property wide review, including its extensive soil and drillhole database along with much of the historic data for the district that it has compiled over the years. The goal will be to target potential Co-Cu-Au-Ag mineralization associated with skarn across the district and come up with targets for follow-up exploration during 2019.

Greenwood West Cobalt in Rocks

Greenwood East Cobalt in Rocks