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Hi-View Resources Completes Borealis Property Acquisition
VANCOUVER, BRITISH COLUMBIA – TheNewswire - SEPTEMBER 24th, 2025 – HI-VIEW RESOURCES INC. (“HI-VIEW” OR THE “COMPANY”) (CSE: HVW; OTC: HVWRF; FSE: B63) announce
About this update from Hi-view Resources Inc
[{"type":"text","content":"VANCOUVER, BRITISH COLUMBIA – TheNewswire - SEPTEMBER 24th, 2025 – HI-VIEW RESOURCES INC. (“HI-VIEW” OR THE “COMPANY”) (CSE: HVW; OTC: HVWRF; FSE: B63) announces that, further to it news release dated August 28, 2025, the Company has completed the acquisition of the Borealis Project in the Toodoggone District of north-central British Columbia (the “Acquisition”). The Company acquired the Borealis Project from Coast Copper Corp. (“Coast Copper”) pursuant to the terms and conditions of an asset purchase agreement dated August 27, 2025 (the “APA”) entered into between the Company and Coast Copper. Figure 1. Hi-View Resources Overview Map R. Nick Horsley, Chief Executive Officer of Hi-View, commented: “The acquisition of Borealis has expanded our land package by 9,106 hectares, nearly doubling our fully owned portfolio with no work commitments. When our team first identified the Placer Dome IP target, we were astonished that such a promising site had never been drilled. In 1992, low-grade bulk tonnage porphyry targets were overlooked, yet today, these deposits are highly valued for their consistent mining grades and predictable metallurgy. We have initiated an airborne survey across the entire new holdings and plan to apply for permits to conduct an IP survey, with the goal of advancing to a drill program to test the target.” The Borealis Project: Cas At the Cas area, the 1992 Placer Dome program combined induced polarization (IP), ground magnetometer and VLF-EM surveys with soil and rock geochemistry. The work defined two strong IP chargeability highs (up to 73 msec) with coincident low resistivity within zones of pyritic clay alteration along the margin of a monzonite stock. Ground magnetics showed elevated responses over the intrusion and adjacent alteration, suggesting possible extensions beneath cover and delineating subtle magnetic highs that track pyritic zones. Geochemistry returned sporadic copper and gold anomalies associated with limonitic quartz veins in the alteration footprint—soils up to 138 ppm Cu and 970 ppb Au, and rocks up to 2.3% Cu and 695 ppb Au. Within this setting, Cas 3-9 comprises multi-stage quartz veins hosted by lapilli tuff, including a sample assaying 106 g/t Ag.1Taken together, the datasets outline a possible sulphide-bearing alteration system at an intrusive margin; element-mobility analysis indicate...