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COMMANDER RESOURCES LTD.

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SABIN

Sabin: Gold and Silver–rich VMS base metal deposit in Ontario

Target: Volcanogenic Massive Sulphide in historic mining region. Gold and Silver-rich suggesting possible Rainy River or La Ronde–style target

Historical work from 70’s and 80’s with small open ended ~200,000 T resource

Recent work by Commander ~ $150,000 including first modern geophysical survey

Recent sampling by Commander indicates zones of high gold and silver in addition to

copper and zinc

Expanded alteration envelope indicated from new mapping and recent geophysical survey

100% Commander except for 2 small internal parcels partly owned by Glencore

Underlying royalty of 1% NSR due to UMEX on core of property

Recommended program: drill ready in part but many targets require first pass sampling, IP geophysics

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Date: Dec. 21, 2019 Drafted by: S. Wetherup Figure: Sabin Property

Regional Geology of the Savant-Sturgeon Lake GreenstoneBelt

Ontario, Canada

COMMANDER RESOURCES LTD.

UTM NAD83 Zone 15

Line Property outline Waterbody Mineral deposit Rock types granitoid rocks diorite

clastic sedimentary rocks felsic volcanic rocks intermediate volcanics mafic volcanic rocks ultramafic rocks

Legend

Watercourse

0 10

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40°N 50°N 60°N 40°N 50°N 60°N 14 0°W 12 0°W 10 0 °W 8 0 °W 60°W 40°W 12 0°W 10 0 °W 80 °W Date: Dec. 21, 2019 Drafted by: S. Wetherup Figure: Sabin Property

Regional 1VD Mag. of the Savant-Sturgeon Lake Greenstone Belt

Ontario, Canada

COMMANDER RESOURCES LTD.

UTM NAD83 Zone 15

Line Property outline Waterbody Mineral deposit Legend Watercourse

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Date: Dec. 21, 2019 Drafted by: S. Wetherup Figure: Sabin Property Marchington DDH Plan and Total Magnetic Intensity

Ontario, Canada

COMMANDER RESOURCES LTD.

UTM NAD83 Zone 15

40°N 50°N 60°N 40°N 50°N 60°N 14 0°W 12 0°W 1 00 °W 80 °W 60°W 40°W 12 0°W 10 0 °W 80 °W VMS horizon Line Watercourse Road Highway Legend Sabin claims Waterbody Geology contact Mapping extents HoleID EOH mm given at scale of 1:1000 grade_eq TraceShade 0 - 5000 5000 - 10000 10000 - 20000 20000 - 50000 50000 - 500000 Zn+Cu% Drill Hole Assays

0 0.25

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Date: Dec. 21, 2019 Drafted by: S. Wetherup Figure: Sabin Property

Kash Zone DDH and Rho 100 m Conductivity

Ontario, Canada

COMMANDER RESOURCES LTD.

UTM NAD83 Zone 15

40°N 50°N 60°N 40°N 50°N 60°N 14 0°W 12 0°W 1 00 °W 80 °W 60°W 40°W 12 0°W 10 0 °W 80 °W VMS horizon Inferred VMS horizon Watercourse Road Highway Legend Sabin claims Waterbody Cu in Rocks (%) 2.0 - 7.2 1.0 - 2.0 0.1 - 1.0 Zn in Rocks (%) 2.0 - 4.2 1.0 - 2.0 0.5 - 1.0 Ag in Rocks (g/t) 100 - 484 25 - 100 Mineral Showings Galena Sphalerite Chalcopyrite 0 0.5 kilometers HoleID EOH mm given at scale of 1:1000 grade_eq TraceShade 0 - 5000 5000 - 10000 10000 - 20000 20000 - 50000 50000 - 500000 Zn+Cu% Drill Hole Assays

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• Sabin was first worked by Union de Miniere Exploration (UMEX) in the 1977 which led to the discovery of the Marchington Zone where shallow drilling on 15 m centres outlined a historical near surface resource from 15 m to 61 m depth. The goal was to outline a near surface zone suitable for trucking to their Thierry Mine at Pickle Lake, 130 km to the north.

Marchington Zone Historical Resource* (non-NI43-101 compliant)

123,000 tonnes @ 2.9% Zn, 0.7% Cu, 1.3 % Pb, 56 g/t Ag. Gold was not generally assayed

*The Marchington Zone resource was defined by UMEX (based on internal company documents dated June 19, 1980), is historic in nature, is the most recent resource estimate currently available and is not to be relied upon except to provide an indication of exploration potential on the property. It was calculated by exploration professionals working for a major company widely reputed as competent, utilizing methodology accepted and relied upon as standard industry practice at the time, but is not compliant with National Instrument 43-101 standards. The reader is cautioned that a qualified person has not done sufficient work to classify this historical estimate as current resources and Commander is not treating it as a current mineral resource.

DDH length Cu % Zn % Pb % Ag g/t Au g/t SA005 6.0 1.11 3.5 1.2 62.9 NA SA008 7.3 0.68 2.8 1.1 54.5 NA SA015 5.9 0.30 2.3 1.7 56.5 NA SA016 8.0 0.20 2.2 0.0 31.3 NA SA017 5.9 0.22 0.6 0.0 19.0 NA SA042 2.3 0.13 9.4 1.6 30.3 1.75 SA061 11.4 0.48 3.0 0.7 45.6 0.13 SA063 3.5 1.67 7.7 2.2 175.8 0.36 SA066 4.9 0.70 3.6 1.5 72.5 0.17 SA069 3.2 4.28 4.7 1.6 177.4 1.18 SAB-95-1 15.9 0.04 1.3 0.0 10.3 0.05

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Intermediate volcaniclastic rocks with

abundant garnets (i.e. aluminous alteration)

Beaver pond with outcrops of garnetiferous sericite-biotite schist (intermediate volcaniclastic rocks)

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Golsil – chalcopyrite lenses in

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West Kash – quartz-sericite-pyrite schist

West Kash – massive pyrite-pyrrhotite lense in

References

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