Toronto, ON, January 29, 2024 - Kuya Silver Corporation (CSE: KUYA) (OTCQB: KUYAF) (Frankfurt: 6MR1) (the “Company” or “Kuya Silver”) is pleased to present the final assay results from a second diamond drilling program at the Campbell-Crawford and Airgiod target areas, Silver Kings Project, where grassroots drilling in March and April 2023 intersected a new high-grade silver and cobalt discovery. The final results of this second drill campaign, including holes 23-SK-27 to -31, are presented. Kuya Silver has identified several new highly-mineralized veins in this program, including a significant new grassroots drill intersection beneath the adjacent Airgiod property, and has tripled the potential size of the buried target zone area which remains open in all directions.

Highlights:

• High-grade mineralized footprint expanded at the Campbell-Crawford target area
  • Hole 23-SK-31 intersected 12,200 g/t (392 oz/t) Ag, 0.17% Co (12,264 g/t AgEq*) over 0.40 m within a wider zone grading 1,799 g/t Ag, 0.03% Co (1,810 g/t AgEq*) over 3.20 m in the Angus Vein (Figure 1)
  • Kuya has now reported four clustered drilling intersections of >2,000 g/t silver (plus cobalt) on the Angus and Toms Veins (Figure 1, 2)
• New blind discovery made at the Airgiod target area, 250 m northwest of original Angus Vein intersection 
  • Hole 23-SK-30 intersected 249 g/t silver, 1.64% cobalt (863 g/t AgEq*) over 0.40 m, within a wider zone grading 132 g/t silver, 0.35% cobalt (263 g/t AgEq*) over 1.88 m, in a new NW-trending vein named the Moran Vein (Figure 1)
  • This is the first known drill hole in the Airgiod Property targeting the buried lower Nipissing Diabase contact. The new vein was intersected in an identical setting to the Angus Vein at the Campbell-Crawford target area
  • This 250 m step-out triples the tested extent of buried silver-cobalt mineralization between the neighbouring Campbell-Crawford and Airgiod properties

David Lewis, Vice President Exploration, commented: “We are extremely pleased with the results from our fall 2023 drill program at Silver Kings. At the Campbell-Crawford prospect, we expanded the area of high-grade vein mineralization, intersected a number of newly identified silver-cobalt veins, and gained a greater understanding of the potential deposit model. On the Airgiod property, we made a blind vein discovery by stepping out approximately 250 meters from the main Campbell-Crawford vein zone. This new Moran Vein reported our highest-grade cobalt assay to date, as well as silver, and appears to strike in a different orientation to the Clark Vein, which was trenched and mapped on surface.”

David Stein, Kuya Silver’s President and CEO remarked, “The blind discovery of a second highly mineralized vein zone below the Nipissing Diabase north of Kerr Lake establishes a new exploration model for the Cobalt camp which can be repeated to generate multiple targets over Kuya Silver’s expansive and district-scale land package. Adding recent discoveries at Airgiod and Campbell-Campbell to some of the better historical prospects on our properties, we now see four or five distinct, high priority, silver-cobalt targets that demonstrate the potential for a hub-and-spoke business case (ie. multiple mines feeding a centralized plant) for the Silver Kings Project. In addition to expanding the Campbell-Crawford and Airgiod discoveries, Kuya Silver is excited by the potential for other new discoveries on its properties.”

New Vein Discovery on Airgiod Property, 250 Meters Northwest of the Campbell-Crawford Vein Zone

Hole 23-SK-30, collared 220 meters due west of the main Campbell-Crawford vein zone and targeting the neighbouring Airgiod property (Figure 2; Table 1), intersected 249 g/t silver, 1.64% cobalt (863 g/t AgEq*) over 0.40 m from 345.12 m, within a wider 1.88 m zone grading 132 g/t silver, 0.35% cobalt (263 g/t AgEq*) in a newly identified NW-trending vein named the Moran Vein. This new discovery includes Kuya Silver’s highest-grade cobalt assay to date, which is closely associated with silver mineralization in all the largest historical mines in the Cobalt camp. This is the first known drill hole to test the buried and untouched lower Nipissing Diabase contact in the Airgiod Property (where mineralization in the camp is known to cluster), and this new vein was intersected in an identical setting to the Angus Vein at the Campbell-Crawford target area to the east. A second, moderately mineralized vein was also intersected at 370.46 m, potentially corresponding to the ENE-trending Clark Vein on surface. This 250 m step-out drill hole potentially triples the southeast-northwest extent of buried silver-cobalt mineralization in the neighbouring Campbell-Crawford and Airgiod properties.

Drilling At Campbell-Crawford Continues to Expand Silver-Cobalt Discovery Area

While all the drill holes in this batch hit multiple mineralized veins, hole 23-SK-31 reported the best result, intersecting 12,200 g/t (392 oz/t) Ag, 0.17% Co (12,264 g/t AgEq*) over 0.40 m within a wider zone grading 1,799 g/t Ag, 0.03% Co (1,810 g/t AgEq*) over 3.20 m in the Angus Vein. To date, four clustered drilling intersections, ranging from 2,180 to 74,418 g/t silver (plus cobalt) on the Angus and Toms Vein, are now defining a 15+ m wide high-grade mineralized shoot near the intersection of these veins that is open to 70+ m depth (Figure 2). It is becoming clearer that vein intersections and flexures are very important to the formation of these wider mineralized zones or shoots, and which may carry disproportionately more silver and cobalt mineralization than the veins themselves. In that regard, the definition of additional veins in the cluster increases the number of potentially mineralized vein intersections. For example, to date in the Campbell-Crawford area, Kuya Silver has discovered at least seven prominent mineralized veins that can be traced by different drill holes, which could indicate as many as ten vein intersection zones. Several other vein structures have been intersected in single drill holes that could further add to this potential.

23 Meter Mineralized Zone Intersected in Hole 23-SK-29

Silver and cobalt mineralization was also identified in holes 23-SK-27, -28 and -29. Hole 23-SK-29 intersected several mineralized veins and broad sulphide zones, including several veins within a 23.10 m, semi-massive copper-lead-zinc bearing sulphide zone beginning at 193.90 m depth (Figure 3). Highly-anomalous silver-cobalt mineralization occurred throughout this zone, outside of documented veins, and significant mineralization was intersected in four vein structures. This style of mineralization (veins adjacent to massive sulphide zones) was mined at the nearby Beaver-Timiskaming Mine, which produced almost 20 million ounces of silver (Sergiades 1968). Of the mines in the Cobalt and Silver Centre mining camp, the Beaver-Timiskaming Mine has many similarities (host rock, vein association with massive sulphide zones, structural setting, association with Archean volcano-sedimentary rocks, vein position relative to the Nipissing Diabase, lack of Coleman Member sedimentary rocks, proximity; Knight 1922) to the veins drilled at Campbell-Crawford and Airgiod to-date.

Quality Assurance and Quality Control

The drill core samples were logged and sampled with limestone blank material and standard reference material added in sample sequence and/or following visual identification of silver or cobalt mineralization. The samples were cut perpendicular to veining by core saw and were secured in labelled vinyl sample bags. Samples were shipped to AGAT Laboratories in Timmins, Ontario, where they were weighed, crushed and pulverized.

At AGAT Labs (Calgary, Alberta), samples were digested by 4-acid and analyzed by ICP-OES (maximum undiluted detection limit of 500 g/t silver).

At SGS Labs (Lakefield, Ontario), samples were processed by 500 g Screened Metallics. This method is suitable for coarse native metals (e.g. gold, silver, copper, palladium and platinum) with no upper detection limit. Samples were screened to 106 microns and fire assayed.

When samples were analyzed for silver by both ICP-AES and Screened Metallics, the Screened Metallics results are presented. All QA/QC standards were acceptable and within two standard deviations of certified values. 

References

Knight, C.W. 1922. Geology of the Mine Workings of Cobalt and South Lorrain Silver Areas; Ontario Department of Mines, Thirty-first Annual Report, 374p.

Sergiades, A.O. 1968. Silver Cobalt Calcite Vein Deposits of Ontario; Ontario Department of Mines, Mineral Resources Circular No. 10, 498p.

National Instrument 43-101 Disclosure 

The technical content of this news release has been reviewed and approved by Mr. David Lewis, P.Geo., Vice President Exploration of Kuya Silver and a Qualified Person as defined by National Instrument 43-101. 

About Kuya Silver Corporation

Kuya Silver is a Canadian‐based mineral exploration and development company with a focus on acquiring, exploring, and advancing precious metals assets in Peru and Canada. 

For more information, please contact:

David Stein, President and Chief Executive Officer
Telephone: (604) 398‐4493 
info@kuyasilver.com
www.kuyasilver.com 

Reader Advisory

This news release contains statements that constitute "forward-looking information," including statements regarding the plans, intentions, beliefs, and current expectations of the Company, its directors, or its officers with respect to the future business activities of the Company. The words "may," "would," "could," "will," "intend," "plan," "anticipate," "believe," "estimate," "expect," "must," "next," "propose," “new,” “potential,” “prospective,” “target,” “future,” “verge,” “favourable,” “implications,” and “ongoing,” and similar expressions, as they relate to the Company or its management, are intended to identify such forward-looking information. Investors are cautioned that statements including forward-looking information are not guarantees of future business activities and involve risks and uncertainties, and that the Company's future business activities may differ materially from those described in the forward-looking information as a result of various factors, including but not limited to fluctuations in market prices, successes of the operations of the Company, continued availability of capital and financing, and general economic, market, and business conditions. There can be no assurances that such forward-looking information will prove accurate, and therefore, readers are advised to rely on their own evaluation of the risks and uncertainties. The Company does not assume any obligation to update any forward-looking information except as required under the applicable securities laws.

Neither the Canadian Securities Exchange nor the Investment Industry Regulatory Organization of Canada accepts responsibility for the adequacy or accuracy of this release.