The Northern Claims Project

Black Pearl Project Highlights

The Black Pearl Project includes the Moose/Harmon area, where historic grab and float samples reported values of up to 100 g/t Au and 68.4 g/t Ag, alongside multi-percent base metals. Nearby carbonate-hosted systems (NUSKARN, McClair, and BR 794) returned strong polymetallic results, including:
  • 12.8% Cu, 4.25% Zn, and 90.5 g/t Ag
  • 3.8 g/t Ag and 0.42% Cu
  • 56.4 g/t Ag, 0.13 g/t Au, and >1% Cu, Pb, Zn
Epithermal-style veins and breccias also occur in this cluster. At the BR showings, assays include 11.7 g/t Au with 73.8 g/t Ag from a 1 m vein (grab), 12.2 g/t Au with 201 g/t Ag and 0.96% Cu from a 20 cm vein (grab), and a chip sample grading 15.7 g/t Au over 0.20 m. Collectively, these results demonstrate a genetic continuum from porphyry through skarn to epithermal settings within the Black Pearl area.

Oxide Summit Project Highlight

The Oxide Summit Project is defined by epithermal vein systems along the Joanna–Gordonia–Falcon trend. Key results include:
  • Joanna East: Chip sampling of 13.0 g/t Au, 13.6 g/t Ag, and 0.129% Cu over 0.9 m
  • Joanna West: Grab samples up to 5.65 g/t Au, 15.3 g/t Ag, and 0.61% Cu
  • Gulch West: Select quartz vein sample of 14.91 g/t Au, 164.9 g/t Ag, and 1.0% Cu
  • Gordonia: Chip sampling averaging 30 g/t Ag, 1.9% Zn, 0.43% Pb, and 0.11% Cu over 0.91 m, plus a grab of 5.745 g/t Au and 200 g/t Ag
  • Oxide Peak: Quartz–carbonate breccias grading up to 6.85 g/t Au, 282 g/t Ag, and 1.23% Cu (grab); channel sampling of 2.0 m at 1.87 g/t Au and 55 g/t Ag
  • Falcon A1: Chip sample of 0.51% Cu and 5.9 g/t Ag over 2.0 m
  • Falcon A2: Narrow quartz veins up to 2.72% Cu, 118.2 g/t Ag, and 1.05 g/t Au
These occurrences define a well-developed epithermal vein corridor, comparable in style to systems at Shasta, Baker, and Lawyers.

Garnet Project Highlights

The Garnet Project hosts the Garnet porphyry occurrence, where feldspar porphyry with disseminated bornite has been documented. Highlights include:
  • Selected grab sample assaying 0.42% Cu and 9.93 g/t Ag
  • Float samples up to 11.6 g/t Au, 39.2 g/t Ag, and 0.315% Cu
These results confirm the porphyry-style potential of the Garnet target.

Ursus Project Highlights

The Ursus Project contains the Ursus 4 occurrence, where historic grab samples yielded 2.11% Cu and 106 g/t Ag. This mineralization is consistent with skarn-style copper–silver systems developed along intrusive contacts

The Harmon Peak Project

Harmon Peak Project Highlights:

The Harmon Peak Project is a 451.5-hectare property located in the prolific Toodoggone District of north-central British Columbia, approximately 23 kilometers north of the Lawyers deposit. Hi-View Resources holds 100% ownership of the project. The property lies within a proven geological belt that hosts multiple porphyry and epithermal systems, making Harmon Peak a compelling addition to the Company’s exploration portfolio.
The project straddles the unconformity between the Upper Triassic Takla Group and Lower Hazelton Toodoggone Group, overlain by Hazelton volcanics intruded by the Black Lake Intrusive Suite. This setting is analogous to nearby deposits where porphyry systems are associated with intrusive centers and epithermal mineralization is controlled by structural corridors.
Historical Work :
  • 986–1988 (Cove Energy): Airborne magnetic and VLF surveys, soil and rock sampling, and alteration mapping. Assays from nearby zones returned values up to 1.79% Cu, 42.2 ppm Ag, and 2.4 ppm Au.
  • 2005 (Stealth Minerals): Rock sampling in the NW Lake Zone reported grades including 1.00% Cu with 0.965 g/t Au and 0.58% Cu with 0.252 g/t Au, along with several anomalous samples.
  • 2022 (TDG Gold Corp.): Airborne magnetic and radiometric surveys defined magnetic lows rimmed by highs coincident with historic copper and gold samples, highlighting untested porphyry potential.
  • Government Surveys: Regional geochemistry has identified strong anomalies including 355 ppm Cu and silver up to 1,409 ppb in stream sediments. Exploration Potential:
Historic surveys outlined chargeability highs interpreted as pyritic clay alteration halos flanking a monzonite stock. Such features are often indicative of the outer shell of porphyry systems, where surface mineralization may be limited but significant potential exists at depth. Supporting this interpretation, magnetic anomalies suggest extensions beneath cover, while geochemical sampling has returned encouraging results with copper, gold, and silver anomalies. The combination of strong alteration signatures, geophysical anomalies, and favorable geology positions Harmon Peak as a highly prospective target for both porphyry and epithermal mineralization.