ETRUSCUS ADVANCES TOWARD PORPHYRY DISCOVERY AT ZAPPA TARGET, GOLDEN TRIANGLE, B.C.

About this update from Etruscus Resources Corp.

VANCOUVER, BC, Nov. 25, 2025 /CNW/ - Etruscus Resources Corp. (CSE: ETR) (OTC: ETRUF) (FSE: ERR") (the "Company" or "Etruscus") is pleased to report results from its 2025 diamond drill program at the Zappa Porphyry Target, a high-priority copper-gold porphyry prospect located on the Company's 100%-owned Rock & Roll Property (the "Property") in British Columbia's prolific Golden Triangle. The inaugural program totalled 1,311 metres ("m") across three drill holes (See Map 1) and was successful in advancing the Company's understanding of the system, vectoring closer to a potential mineralized porphyry intrusion. Drilling focused on a large surface alteration and chargeability anomaly, intersecting intensely altered volcanic and sedimentary rocks with zones of potassic alteration. Geochemical and alteration patterns indicate that hole RR25-03 was nearest to the heat source, suggesting that the porphyry intrusion may lie to the northeast, beneath the Twin Glacier where further drilling is warranted. The discovery of this alteration extends the Bronson Porphyry Trend onto the Property and greatly increases its prospectivity (See Map 2). Fiore Aliperti, President and CEO of Etruscus commented, "Each step in a porphyry exploration program provides critical data to refine our understanding of the mineralized system. The identification of potassic and QSP alteration is a strong indicator that we're close to the heart of the system, a significant advancement in our exploration. Several nearby discoveries in the Golden Triangle required multiple programs to vector in and locate mineralized zones, and our first-ever drill results at Zappa clearly show we're on the right path." Highlights: Drill Hole Summary: RR25-01 Hole 1 was designed to test a high chargeability anomaly on the western edge of the Zappa target. The hole was drilled steeply to the north and encountered mixed sediments and volcanic units including black shales, andesites and volcanic tuffs. Porphyry alteration predominantly as quartz-sericite-pyrite was prevalent from top of hole to 151 m with total replacement of primary textures (See Graphic 1). This alteration contained up to 5% pyrite as disseminations, stringers and geochemical data confirmed strong hydrothermal alteration. Below this, the hole continued into black...

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