Exploration

The Golden Triangle is one of the world’s richest mineral regions. It is also home to some of the region’s richest biodiversity including habitat for moose, caribou, grizzlies and three species of salmon.

This region hosts some of BC’s most successful historical and present-day mines and mineral projects. The attractiveness of the area is due to a combination of favourable geology and limited mineral exploration to date with an estimated $15 billion of reserves in the ground. 50% of the mineral wealth in BC is in Tahltan Territory who have unceded claim to 150,000km2. The Tahltan have mined in the territory for more than 12,000 years for tools, spears and arrowheads, while maintaining the balance within the local ecosystems. Today, the Tahltan are rebuilding their Nation and influencing how big mineral development is done in their territory to ensure respect for their lands and waters. Through multiple generations who lived on the land and with the natural world, there remains a long history, expertise and knowledge of the area, together with modern mapping, data and resources developed in order to understand and properly work with the land.

Our focus is on gold and copper assets in the Golden Triangle within the Tahltan Territory in NW British Columbia. SRR owns 100% interest in its claims within well-known ore bodies and historically sound properties. We are focusing on three areas for our initial exploration program:

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Forest Kerr

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Samotua

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Dease Creek

Forest Kerr – In the heart of the Golden Triangle

Property Summary – Forest Kerr (Au, Ag, Cu, Zn)

Property: 3 multi-cell claims totaling 3623 hectares.

Location: 17 km NW of Eskay Creek Mine, just NW of KSM and Brucejack, NE of Snip and Johnny Mountain, just SE of Galore Creek, in heart of Golden Triangle

Owned: Spirit Rock Resources holds a 100% interest in the claims on the property.

Good to Date: All claims are in good standing until 2024.

Target: VMS.

Rock Types: Au bearing quartz veins.

Historic Production and Assay Results:Overlies barely explored Hazelton Group rocks, the same strata as Eskay Creek. Government study just to NE concluded there was VMS potential. Further to the north and south are showings and prospects that suggest VMS activity. Also has presence of gold bearing quartz associated with the Forest Kerr Fault.

Samotua – Trending along successful historic sites

Property Summary – Samotua (Au-Cu)

Property: 3 multi-cell claim totaling 2605 hectares.

Location: 64 km northwest of Telegraph Creek, and just NE of historic Golden Bear Mine.

Owned: Spirit Rock Resources holds a 100% interest in the claims on the property.

Good to Date: All claims are in good standing until 2024.

Target: Carlin Type Gold.

Rock Types: Deformed Permian, limestone and Carboniferous metavolcanic rocks which are intruded by feldspar porphyry dikes.

Historic Assay Results: Features mineralization similar to nearby Golden Bear Mine (major past producer). Several rock samples from a silicified limestone unit in contact with an altered tuff unit have assayed over 1 g/t gold. The silicified limestone outcrops over at least 1.5 kilometers in an approximately 200 m wide zone trending in a NE direction.

Dease Creek – Significant Gold Showings

Property Summary – Dease Creek (Au)

Property: 4 multi-cell claims totaling 2141 hectares.

Location: 22 km Northwest of the town of Dease Lake and accessible by road with good infrastructure.

Owned: Spirit Rock Resources holds a 100% interest in the claims on the property.

Good to Date: All claims are in good standing until 2024.

Target: Orogenic gold.

Rock Types: Permian to Triassic metasediments and volcanics of the Cache Creek Complex. Ultramafics bodies occur throughout the area.

Historic Assay Results: Recorded production from Dease Creek up to 1945 was 126 000 oz Au. Active placer operation at mouth of Dease Creek in summer 2022. A highly anomalous stream sediment sample collected was over the 99.8th percentile for gold regionally. The upper catchment is underlain by a mag high that may indicate ultramafic rocks. Occurrence of placer gold in an area of metasediments and ultramafics, along with a favourable structural regime suggests an orogenic gold target.