Northwire Canada EditionThursday, November 12, 2026
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Gold 4,000.50 −0.7% Silver 52.00 +1.5% Copper 6.27 +0.5% Oil 86.53 +0.6% Palladium 1,030.00 +0.9% TIG 0.800 +0.0% RVG 0.715 −4.0% FNV 354.26 −2.4% FDY 4.30 −0.5% MAU 16.05 −3.2% VOXR 6.78 −0.6% TLO 7.04 −1.0% NICU 1.95 −5.8% VTEN 0.440 +0.0% AWM 0.025 +0.0% OR 50.79 −1.8% AUXX 5.30 −5.5% TNR 0.420 +40.0% ORCL 0.030 +0.0% ELD 47.71 −5.4% OPW 0.140 −6.7% Gold 4,000.50 −0.7% Silver 52.00 +1.5% Copper 6.27 +0.5% Oil 86.53 +0.6% Palladium 1,030.00 +0.9% TIG 0.800 +0.0% RVG 0.715 −4.0% FNV 354.26 −2.4% FDY 4.30 −0.5% MAU 16.05 −3.2% VOXR 6.78 −0.6% TLO 7.04 −1.0% NICU 1.95 −5.8% VTEN 0.440 +0.0% AWM 0.025 +0.0% OR 50.79 −1.8% AUXX 5.30 −5.5% TNR 0.420 +40.0% ORCL 0.030 +0.0% ELD 47.71 −5.4% OPW 0.140 −6.7%

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GR Silver Drill Program Delivers High-Grade Intercepts: 35.45 m at 311 g/t Ag, including 0.4 m at 4,232 g/t Ag in the SE Area, and 2.15 m at 1,164 g/t Ag, 0.6% Cu, and 0.37% W in the Parallel Breccia Target

GR Silver Drill Program Delivers High-Grade Intercepts: 35.45 m at 311 g/t Ag, including 0.4 m at 4,232 g/t Ag in the SE Area, and 2.15 m at 1,164 g/t Ag, 0.6% Cu, and 0.37% W in the Parallel Breccia Target Canada NewsWire VANCOUVER, BC, Nov. 11, 2026 VANCOUVER, BC, Nov. 11, 2026 /CNW/ -- GR Silver Mining Ltd. ("GR Silver Mining" or the "Company") (TSXV: GRSL) (OTCQX: GRSLF) (FRANKFURT: GPE) is pleased to announce continued positive drill results from the current 20,000-metre ("m") drill program at San Marcial, Mexico that confirm the extension of high grade zones in the SE Area, and the continuity of the Parallel Breccia Target located 300 m to the southwest of the 2023 NI 43-101 Resource Area. Highlights Hole SMS26-19 returned 35.45 m true width ("TW") at 311 g/t Ag, including 0.4 m TW at 4,232 g/t Ag and 1.35 TW m at 996 g/t Ag, further confirming the extension of the high-grade silver mineralized system in the SE Area. Hole SMS26-17 returned 2.15 m TW at 1,164 g/t Ag, 0.6 % Cu, 0.37% W in the separate Parallel Breccia Target. This intercept is significant in that it may indicate a multiphase hydrothermal system, potentially reflecting a transition toward a porphyry-related mineralizing environment. The drill program has pivoted to further test the high-grade dilation zone extending from hole SMS26-04, which returned 45.1 m TW at 1,623 g/t Ag, including 8.25 m at 8,579 g/t Ag (see News Release dated May 19, 2026). With the wet season finally winding down and the Durango access road upgrades nearly complete, it is expected that the pace of the ongoing drill program will significantly increase going forward. GR Silver Mining's President & CEO, Eric Zaunscherb, commented, "The systematic approach to exploring the San Marcial mineralized system continues to bear fruit. These results provide important insights into mineralization hosted by the main hydrothermal breccia in the SE Area and the potential extension of the higher-grade dilation zone(s) within. Further, the distinct mineralization and alteration intersected within the separate Parallel Breccia Target continues to support a potential porphyry model, which we plan to test with deeper holes into the central intrusive body later in this program. As we emerge from this year's extensive wet season, our access road upgrade in Durango will allow us to accelerate our drill program, which should enable delivery of our planned MRE update by mid-2027. The safety and security of our employees, contractors, and local communities remain our top priority, as we continuously monitor the security situation in and around the Plomosas Project area. Highlights of Recent 2026 Step-Out Drilling at San Marcial SMS26-19 (Figure 1) intersected a broad zone of chlorite–hematite-rich hydrothermal breccias extending across both the upper Oligocene volcanic sequence and the underlying Jurassic volcano-sedimentary sequence, primarily following the structurally controlled contact between these units. The drill hole also encountered an increased occurrence of dioritic dykes, which become more prominent toward the SE Extension and are interpreted to be associated with the Oligocene subvolcanic intrusive complex. The crosscutting relationships observed between the intrusive dykes and silver–lead–zinc mineralization provide important insights into the timing of the hydrothermal system. These relationships suggest that mineralization developed during a later hydrothermal event, following the emplacement of the Oligocene intrusive complex. Best results (Table 1) include: 35.45 m TW at 311 g/t Ag from 339.85 m down hole including 0.4 m TW at 4,232 g/t Ag and 1.35 m TW at 996 g/t Ag Table 1:        SMS26-16, SMS26-18 and SMS26-19 Drilling Highlights – 2026 Step-Out Drilling Program – SE Area Drill Hole From (m) To (m) Mineralization Type  Apparent width (m) True width (m) Ag Au g/t Pb % Zn % SMS26-19 339.85 376.15 Hydrothermal Bx, Stockwork & Dioritic Dyke 36.3 35.45 311 0.03 0.2 0.4 (Incl) 341.95 342.35 Hydrothermal Bx 0.4 0.4 4,232 0.03 1.6 1.8 (Incl) 356.9 357.25 Hydrothermal Bx 0.35 0.35 1,901 0.18 4.2 2.7 (Incl) 359.5 360.0 Hydrothermal Bx 0.5 0.5 2,017 0.09 0.6 1.2 (Incl) 373.75 375.15 Hydrothermal Bx 1.4 1.35 996 0.24 1.3 2.9 SMS26-16 264.8 272.55 Hydrothermal Bx 7.75 7.6 50 0.04 NA 0.1 SMS26-18 232.2 242.05 Hydrothermal Bx 9.85 9.7 11 NA NA NA 282.85 289.85 Stockwork 7.0 6.9 11 NA NA 0.1 Note: Numbers may be rounded. Results are uncut and undiluted. True sample widths are based on crosscutting angles in core, structural measurements, and intersections for drill holes immediately above and below down dip. NA = no significant result. Bx = breccia. SMS26-17 confirms the continuity of the Parallel Breccia Target, located approximately 300 m southwest of the 2023 NI 43-101 Resource Area (Figure 1). Drilling has now demonstrated mineralization continuity over 300 m along strike and 125 m down-dip, with the system remaining open for further expansion in both directions. Mineralization is primarily associated with quartz–calcite–hematite–tourmaline hydrothermal breccias hosted within the lower Jurassic volcano-sedimentary sequence. These breccias are locally crosscut by stockwork veinlets associated with anomalous silver and gold values, suggesting multiple episodes of hydrothermal activity. The overlapping mineralization styles and alteration assemblages may indicate a multiphase hydrothermal system, potentially reflecting a transition toward a porphyry-related mineralizing environment. Best results (Table 2) include: 2.2 m TW at 1,164 g/t Ag, 0.6% Cu, 0.37% W, from 104.8 m down hole Table 2:        SMS26-11 and SMS26-17, Drilling Highlights – 2026 Step-Out Drilling Program – Parallel Breccia Target Drill Hole From (m) To (m) Mineralization Type Apparent width (m) True width (m) Ag g/t Au g/t Pb % Zn % SMS26-11 20.25 20.75 Fault & Hydrothermal Bx 0.5 0.5 23 0.11 0.5 0.7 Drill Hole From (m) To (m) Mineralization Type Apparent width (m) True width (m) Ag g/t Au g/t Cu % W % SMS26-17 104.80 107.00 Hydrothermal Bx & Stockwork 2.20 2.15 1,164 0.10 0.6 0.37 Note: Numbers may be rounded. Results are uncut and undiluted. True sample widths are based on crosscutting angles in core, structural measurements, and intersections for drill holes immediately above and below down dip. NA = no significant result. Bx = breccia. Drill hole SMS26-19 successfully intersected 35.45 m TW at 311 g/t Ag, including 0.4 m TW at 4,232 g/t Ag, further confirming the continuity of the high-grade silver mineralized system in the SE Area. This mineralized zone was initially identified near surface during the 2022 step-out drilling program in hole SMS22-14 (Figure 2), which returned 10.5 m at 23 g/t Ag and 3.5 m at 118 g/t Ag, including 0.2 m at 1,790 g/t Ag (see News Release dated October 17, 2022). More recently, the same mineralized system was intersected by drill holes SMS26-06 and SMS26-07 as part of the current 20,000 m step-out drilling program, returning significant results of 21.9 m at 168 g/t Ag, including 6.15 m at 447 g/t Ag (see News Release dated July 10, 2026). The SMS26-19 results have now extended the mineralization an additional 80 m down-dip and demonstrate the vertical continuity of high-grade silver mineralization over at least 300 m, reinforcing the exploration potential for further expansion of the mineralized system at depth in the SE Area (Figure 2). As part of the current 20,000-metre step-out drilling program, two additional drill holes are planned on this section to further test the continuity of high-grade silver mineralization at depth and potentially extend the mineralized system to a total down-dip extent of 500 m from surface. Holes SMS26-16 and SMS26-18 did not return encouraging values, requiring further evolution of our exploration model in this area. Drill hole SMS26-17 successfully confirmed the continuity of high-grade silver mineralization within the Parallel Breccia Target, intersecting 2.15 m TW at 1,164 g/t Ag, 0.6% Cu, and 0.37% W hosted in a hydrothermal fault breccia. This distinctive silver-copper-tungsten (Ag-Cu-W) mineralization association was first recognized during the 2025 exploration drilling program in hole SMS25-10A, which returned 9.0 m at 374 g/t Ag, 0.3% Cu, and 0.59% W, including 1.0 m at 1,542 g/t Ag, 1.4% Cu, and 0.62% W (see News Release dated September 24, 2025). The occurrence of sulfide-rich silver mineralization associated with anomalous copper and tungsten values, together with a tourmaline–actinolite–albite–K-feldspar alteration assemblage, suggests a relatively high-temperature hydrothermal environment potentially linked to a porphyry-related mineralizing system. This interpretation is further supported by the location of the Parallel Breccia within a high-chargeability geophysical anomaly in the lower volcano-sedimentary unit surrounding a Cretaceous granodioritic intrusive complex (Figure 1). Additional drilling results have further demonstrated the continuity and exploration potential of the Parallel Breccia. As illustrated in Figure 3, drill hole SMS26-08 intersected 19.9 m grading 206 g/t Ag, including 1.3 m at 932 g/t Ag (see News Release dated August 21, 2025). These results have outlined a mineralized structure extending approximately 300 m along strike and at least 150 m down-dip, highlighting the potential for further expansion of high-grade silver mineralization within the Parallel Breccia system. Mineralization is present in hole SMS26-11 but poorly developed in this location. Discussion The current 20,000-metre step-out drilling program at San Marcial continues to deliver encouraging results, confirming the continuity and expansion potential of high-grade silver mineralization beyond the boundaries of the 2023 NI 43-101 Mineral Resource Estimate ("MRE"), following the chlorite-hematite hydrothermal breccia at the contact between upper Oligocene volcanics and lower volcano-sedimentary units. In the SE Extension, the intersection in drill hole SMS26-19 further supports the continuity of the mineralized system initially identified in 2022 and subsequently intersected during the 2026 drilling campaign. These results demonstrate the vertical continuity of high-grade silver mineralization over at least 300 m vertically. The association of high-grade silver mineralization trends with structural controls suggests a southeast-plunging mineralized system that remains open for further expansion at depth, as illustrated in Figure 4. Drilling at the Parallel Breccia Target, located approximately 300 m southwest of the existing MRE area, has outlined high-grade silver mineralization extending approximately 300 m along strike and at least 150 m down-dip. In addition to the encouraging silver grades intersected in SMS26-17, and the increased size of the mineralized zone at the Parallel Breccia Target, the recent drilling is providing valuable geological insights into the broader mineralizing environment at San Marcial. The association of silver with anomalous copper and tungsten, together with tourmaline–actinolite–albite–K-feldspar alteration, multiple hydrothermal breccia events, and stockwork veining, suggests a complex, multiphase hydrothermal system potentially linked to a deeper porphyry-related environment. These results strengthen confidence in the geological exploration model and highlight the opportunity to expand the known silver mineralization both laterally and at depth, while advancing the understanding of the district-scale mineral potential of San Marcial within the Plomosas Project. Figure 5 illustrates the distribution of Indicated and Inferred Mineral Resources defined in the 2023 MRE, together with high-grade silver intercepts reported from drilling programs conducted since 2023. These results highlight the potential for further resource expansion and the possible conversion of Inferred Mineral Resources to the Indicated category through additional drilling and improved geological confidence. Figures 6 and 7 illustrate the characteristic textures and mineral assemblages associated with high-grade silver mineralization within the hydrothermal breccias intersected in drill hole SMS26-19. The selected core samples provide representative examples of the mineralization styles and hydrothermal textures observed throughout the broader mineralized interval. Table 3 summarizes the progress of the 2026 San Marcial step-out drill program. To date, 7,756 m have been drilled in 25 holes, with assays pending from 6 holes. Table 3:           2026 San Marcial SE Area Step-Out Drill Program – Drill Hole Details Note: all holes drilled from surface; WGS84 Datum. About the Plomosas Project The Plomosas Project, including the recent high-grade silver discovery in the San Marcial SE Area, is emerging in 2026 as a high-grade silver district located on the southwestern edge of the Sierra Madre Occidental, at the border of Durango and Sinaloa, Mexico. The Plomosas Project, covering 7,823 ha and including the historical Plomosas underground mine, benefits from existing mine infrastructure, road access and valid permits associated with past-producing mining sites. The district contains intermediate to low-sulfidation epithermal silver and gold mineralization, hosted in hydrothermal breccias and veins. Wide, high-grade, shallow hydrothermal breccias have been delineated in the San Marcial Area, including the SE Area discovery. Step-out drilling continues in 2026, with continuous resource growth, principally targeting pure silver resources. QA/QC Procedures The Company has implemented QA/QC procedures, which include the insertion of blank, duplicate, and standard samples in all sample lots sent to SGS de México, S.A. de C.V. laboratory facilities in Durango, Mexico, for sample preparation and assaying. For every sample with results above Ag > 100 ppm (over the limit), these samples are re-assayed by SGS de Mexico. Core samples are represented by both HQ and NQ diameters and samples are represented by ½ core split of original core. The analytical methods include four acid Digestion and Inductively Coupled Plasma Optical Emission Spectrometry, with Lead Fusion Fire Assay and a gravimetric finish for silver above over limits. For gold assays, the analytical methods are Lead Fusion and Atomic Absorption Spectrometry, Lead Fusion Fire Assay, and gravimetric finish for gold above over limits (>10 ppm). Qualified Person The Qualified Person under National Instrument 43-101 Standards of Disclosure for Mineral Projects for this news release is Dr. Gilles Arseneau, P. Geo., contractor from Arseneau Consulting Services Inc., who has reviewed and approved its contents. About GR Silver Mining Ltd. GR Silver Mining is a Canadian-based, Mexico-focused mineral exploration company engaged in cost-effective silver-gold resource expansion on its 100%-owned assets, located on the eastern edge of the Rosario Mining District, in the southeast of Sinaloa State, Mexico. GR Silver Mining controls 100% of the Plomosas Project, including both the high-grade silver discovery at the San Marcial Area and the former Plomosas underground mine. Recent discoveries in the 78 km² of highly prospective, advanced-stage exploration concessions position the Company well for resource expansion at the Plomosas Project. Cautionary Statement Regarding Forward-Looking Information This press release contains "forward-looking statements" within the meaning of applicable Canadian securities legislation and information that are based on the beliefs of management and reflect the Company's current expectations. When used in this press release, the words "estimate", "project", "belief", "anticipate", "intend", "expect", "plan", "predict", "may" or "should" and the negative of these words or such variations thereon or comparable terminology are intended to identify forward-looking statements and information. Such statements and information reflect the current view of the Company. Risks and uncertainties may cause actual results to differ materially from those contemplated in those forward-looking statements and information. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this press release. SOURCE GR Silver Mining Ltd. View original content to download multimedia: http://www.newswire.ca/en/releases/archive/November2026/11/c8791.html Contact: GR Silver Mining Ltd., Eric Zaunscherb, President & CEO; For further information, please contact: Telephone: +1 236-270-2057, Email: [email protected]
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