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Rio Grande Resources Announces Positive Assay Results From its Sampling and Field Campaign at the Winston Gold-Silver Project, New Mexico USA

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Rio Grande Resources (RGRLF) has announced significant assay results from its Winston Gold-Silver Project in New Mexico. The sampling program revealed exceptional grades including 66.2 g/t gold and 830 g/t silver along the Paymaster Fault corridor. The campaign, conducted in March 2025, collected 57 samples and confirmed 1.5km of continuous mineralization. Notable discoveries include copper-rich mineralization with one sample assaying 2.76% Cu from a historic shaft. The results identified three key technical advancements: confirmed structural controls for high-grade mineralization, significant depth potential, and diverse mineralization styles including hydrothermal rhyolite breccias, andesite-hosted copper zones, and banded chalcedonic quartz breccias. The company is proceeding with additional geological mapping and geophysical surveys to refine drill targets.
Rio Grande Resources (RGRLF) ha annunciato risultati significativi delle analisi dal suo progetto Winston Gold-Silver nel New Mexico. Il programma di campionamento ha rivelato concentrazioni eccezionali, tra cui 66,2 g/t di oro e 830 g/t di argento lungo il corridoio della faglia Paymaster. La campagna, svolta a marzo 2025, ha raccolto 57 campioni e confermato 1,5 km di mineralizzazione continua. Scoperte rilevanti includono mineralizzazioni ricche di rame, con un campione che ha evidenziato il 2,76% di Cu da un pozzo storico. I risultati hanno individuato tre importanti progressi tecnici: il controllo strutturale confermato per mineralizzazioni ad alta concentrazione, un potenziale significativo in profondità e stili mineralogici diversificati, tra cui brecce idrotermali di riolite, zone di rame ospitate da andesite e brecce di quarzo calcedonico a bande. L'azienda sta proseguendo con ulteriori mappature geologiche e indagini geofisiche per definire meglio gli obiettivi di perforazione.
Rio Grande Resources (RGRLF) ha anunciado resultados significativos de ensayos en su proyecto Winston Gold-Silver en Nuevo México. El programa de muestreo reveló grados excepcionales, incluyendo 66,2 g/t de oro y 830 g/t de plata a lo largo del corredor de la falla Paymaster. La campaña, realizada en marzo de 2025, recolectó 57 muestras y confirmó 1,5 km de mineralización continua. Descubrimientos destacados incluyen mineralización rica en cobre, con una muestra que analizó 2,76% de Cu de un pozo histórico. Los resultados identificaron tres avances técnicos clave: controles estructurales confirmados para mineralización de alta ley, potencial significativo en profundidad y estilos de mineralización diversos, incluyendo brechas hidrotermales de riolita, zonas de cobre alojadas en andesita y brechas de cuarzo calcedónico bandeado. La compañía continúa con mapeos geológicos adicionales y estudios geofísicos para afinar los objetivos de perforación.
Rio Grande Resources(RGRLF)는 뉴멕시코에 위치한 Winston 금-은 프로젝트에서 중요한 분석 결과를 발표했습니다. 2025년 3월에 진행된 샘플링 프로그램에서는 Paymaster 단층 지대에서 금 66.2 g/t, 은 830 g/t의 뛰어난 등급이 확인되었습니다. 총 57개의 샘플이 수집되었으며 1.5km에 걸친 연속 광화대가 확인되었습니다. 주목할 만한 발견으로는 역사적 갱도에서 채취한 샘플이 구리 함량 2.76%를 보인 구리 풍부 광화대가 있습니다. 이번 결과는 고품위 광화에 대한 구조적 제어 확인, 깊이 잠재력의 중요성, 그리고 열수성 리올라이트 브레시아, 안산암 내 구리대, 층상 칼세도니아 석영 브레시아 등 다양한 광화 유형 세 가지 주요 기술적 진전을 밝혀냈습니다. 회사는 시추 목표를 정밀화하기 위해 추가적인 지질 조사 및 지구물리학적 조사를 진행 중입니다.
Rio Grande Resources (RGRLF) a annoncé des résultats significatifs d'analyses sur son projet Winston Gold-Silver au Nouveau-Mexique. Le programme d'échantillonnage a révélé des teneurs exceptionnelles, notamment 66,2 g/t d'or et 830 g/t d'argent le long du corridor de la faille Paymaster. La campagne, menée en mars 2025, a collecté 57 échantillons et confirmé 1,5 km de minéralisation continue. Parmi les découvertes notables figurent une minéralisation riche en cuivre, avec un échantillon affichant 2,76 % de Cu provenant d'un puits historique. Les résultats ont identifié trois avancées techniques clés : la confirmation des contrôles structuraux pour une minéralisation à haute teneur, un potentiel important en profondeur, et des styles de minéralisation diversifiés, comprenant des brèches rhyolitiques hydrothermales, des zones de cuivre encaissées dans l'andésite, et des brèches de quartz calcedonien bandé. La société poursuit des cartographies géologiques supplémentaires et des levés géophysiques afin de préciser les cibles de forage.
Rio Grande Resources (RGRLF) hat bedeutende Analyseergebnisse von seinem Winston Gold-Silber-Projekt in New Mexico bekannt gegeben. Das Probennahmeprogramm ergab außergewöhnliche Gehalte, darunter 66,2 g/t Gold und 830 g/t Silber entlang des Paymaster-Störungskorridors. Die im März 2025 durchgeführte Kampagne sammelte 57 Proben und bestätigte eine 1,5 km lange kontinuierliche Mineralisierung. Bemerkenswerte Entdeckungen umfassen kupferreiche Mineralisierung, wobei eine Probe aus einem historischen Schacht 2,76 % Cu aufwies. Die Ergebnisse identifizierten drei wesentliche technische Fortschritte: bestätigte strukturelle Kontrollen für hochgradige Mineralisierung, signifikantes Tiefenpotenzial und vielfältige Mineralisierungsstile, darunter hydrothermale Rhyolith-Brekzien, andesithostete Kupferzonen und gebänderte chalcedonische Quarzbrekzien. Das Unternehmen setzt weitere geologische Kartierungen und geophysikalische Untersuchungen fort, um Bohrziele zu verfeinern.
Positive
  • Exceptional high-grade assay results with 66.2 g/t gold and 830 g/t silver from sampling
  • Discovery of significant copper mineralization with 2.76% Cu in one sample
  • Confirmation of 1.5km continuous mineralization along Paymaster Fault corridor
  • Multiple mineralization styles identified, suggesting diverse resource potential
  • 100% ownership of the Winston project
Negative
  • Early-stage exploration project with no defined resource estimates yet
  • Limited sample size of only 57 samples collected
  • Narrow mineralization widths in some samples (as small as 0.2m)

Key Highlights include:

  • Assay Results include 66.2 g/t Gold and 830 g/t Silver

  • 1.5km of continuous mineralization confirmed along Paymaster Fault corridor

  • 1 sample assayed 2.76% Cu from a historic 20ft shaft on a copper-oxidized andesite breccia.

VANCOUVER, BC / ACCESS Newswire / June 18, 2025 / Rio Grande Resources Ltd. (CSE:RGR)(OTCPINK:RGRLF) ("Rio Grande" or "RIO" the "Company"), is pleased to announce the results from its geological mapping and sampling program conducted previously announced completed on April 07, 2025, at its 100%-owned Winston project in the Black Range of Sierra County, New Mexico. The program focused on the Paymaster Fault Corridor and identified several new mineralized veins (see figure 1 and Picture 1) and confirmed high-grade gold and silver mineralization across multiple vein systems and returning assays including highlights of 66.2 g/t gold and 830 g/t silver illustrated in Table 1, with full assay illustrated in Table 2. The field campaign conducted from March 24-28, 2025, collected 57 samples and provided the Company geological insights and increased understanding of the high-grade epithermal vein system. These results serve to reinforce the project's exploration potential and indicate that a large, multi-phase hydrothermal system is present.

Figure 1. Property Map with New Results Illustrated as Coloured Triangles.

Jason Barnard, President and CEO of Rio Grande Resources, commented:
"These results underscore the high-grade potential of the Winston project, with gold values up to 66.2 g/t and silver up to 830 g/t. The discovery of new mineralized veins, combined with historic high-grade production from the Ivanhoe, Emporia, and Little Granite mines, reinforces our confidence in the district's potential. We are particularly encouraged by the copper-rich mineralization which adds another dimension to the project's value. These encouraging results continue to expand our knowledge base and further support the district-scale potential we are unlocking at the Winston Project. We look forward to continuing our exploration efforts on the property and increasing value for our shareholders."

Picture 1. Newly Discovered Vein Trend, North Zone

Table 1. Sampling Highlights*

Sample ID

Au (g/t)

Ag (g/t)

Au-Eq* (g/t)

Width (m)

Mineralization Style

1844416

66.2

830

76.6

0.5

Rhyolite breccia

1844444

16.75

746

26.1

0.2

Comb quartz-amethyst

1844419

6.39

23

6.7

2.5

Quartz-rhyolite breccia

1844458

0.005

60.2

0.8

2.0

Cu-oxidized andesite (2.76% Cu)

*See full assay result in table 2 below

Technical Advancements

Building on April's preliminary findings, the latest assay results from the Winston Project reveal three critical advancements in our geological understanding of the system:

Structural Controls Confirmed: High-grade mineralization demonstrates a strong structural control, with the most significant gold and silver values concentrated at vein bends and intersections along the Paymaster Fault corridor. This is particularly evident where ginguro banding (black sulphide-rich layers) is present, a classic indicator of high-grade precious metal deposition in epithermal systems. This sampling phase's highest-grade sample (1844416: 66.2 g/t Au, 830 g/t Ag) occurred precisely at a 340° structural bend in the Paymaster Fault, confirming that these geometric complexities act as primary fluid conduits and metal traps (pic of sample below).

Picture 2. Sample 1844416 (66.2 g/t Au)

Depth Potential Indicated: Quartz textures observed in the field - including colloform banding and crustiform-cockade textures - along with increasing sulphide content in deeper exposures, strongly suggest the mineralized system remains open and potentially expands below historic workings. The highest-grade samples correlate with transitional textures between epithermal and mesothermal regimes, suggesting the valuable elements may represent the upper expressions of a more extensive system. This vertical zonation pattern, where gold values increase with depth until reaching an optimal "precious metal horizon," is characteristic of productive low-sulfidation districts worldwide.

Mineralization Styles: While epithermal quartz veins remain the primary host, the recent results demonstrate significant mineralization occurs in three additional geological domains:

  1. Hydrothermal rhyolite breccias - Sample 1844416 (66.2 g/t Au) came from explosive rhyolite tuff breccia, showing that high-grade mineralization extends beyond simple quartz veins into the surrounding volcanic host rocks.

  2. Andesite-hosted copper zones - The 2.76% Cu value in sample 1844458 demonstrates the presence of additional polymetallic targets. This mineralized andesite breccia runs parallel to the main Paymaster Fault Zone and may have familial relations to the prominent copper signature observed in conjunction with gold mineralization.

  3. Banded chalcedonic quartz breccias - Layered comb, massive, and chalcedonic quartz veins are prominent along surface vein exposures. Higher precious metal grades are observed when clasts are rimmed in chalcedony and the matrix shows patches of platy replacement (boiling textures).

Table 2. Gold & Silver Assay Results (samples returning > 2.0 gpt Au-Equivalent)

Sample ID

Au (g/t)

Ag (g/t)

Description (Mineralization Style)

Location

1844416

66.20

830.0

Quartz breccia with explosive rhyolite tuff clasts, sulphide bands

Northern Trench Area

1844444

16.75

746.0

Coarse comb Amethyst + Qtz-Calcite breccia with oxides

Vein Bend (340°)

1844437

3.46

331.0

Banded Amethystine Vein with vitrophyre matrix

Paymaster Trend

1844419

6.39

23.0

2.5m chip channel - Qtz Rhyolite Breccia with 5% oxides

Pit Exposure

1844415

3.31

23.4

Quartz/Calcite Breccia phase (historic trench)

Northern Trench Area

1844442

4.48

442.0

Qtz vein with ginguro bands + orange oxides

Dozer Cut

1844430

3.36

187.0

0.4m layered Qtz+Cal vein with chalcedony

Paymaster Trend

1844420

4.38

82.8

Composite chip from 1m massive quartz vein

Pit Sampling

1844450

0.90

598.0

Andesite breccia with Cu oxides (chalco/covellite)

Historic Shaft

1844454

0.64

618.0

Qtz+Cal vein with dark sulphide bands

ROM Pile

1844428

0.87

45.1

1.4m calcite vein + stockwork

Stockwork Zone

1844441

1.49

165.0

Layered massive Qtz with red oxide patches

Trench 280°

  1. Detection Limits: Au (<0.005 g/t), Ag (<0.05 g/t)

  2. High-Grade Threshold: Samples >2.0 g/t Au or >100 g/t Ag highlighted

  3. Au-Equivalent = Au (g/t) + [Ag (g/t) ÷ 80]

Picture 3. Various Samples

Dr. Michael Feinstein, Qualified Person, added "The field observations and assay results support our exploration model and provide additional control for drill targeting. At the Winston Project, significant tectonic activity and stretching along the Rio Grande Rift Corridor (RGRC) created a long-lived plumbing system for hydrothermal fluids.

With these encouraging results, additional trenching is recommended to define mineralized shoot geometries at surface. Our upcoming field work is focused on expanding geochemical footprints and approximating the relative vertical position in the exploration model along each vein trace."

Next Steps

Additional geological mapping and geophysical surveys are underway to refine drill targets that will further test the high-grade mineralization along the Paymaster Fault Corridor and other newly identified targets.

All samples were collected by Mineoro Explorations and securely maintained through to submission to the ALS Minerals laboratory in Tucson, an ISO-3000 certified laboratory. Samples were analyzed by Fire Assay and ICP-MS. Internal laboratory QA/QC protocols were followed and 5% external standards are submitted with all sample batches.

Qualified Person

Technical information in this news release has been reviewed and approved by Michael Feinstein, PhD, CPG, who is a Qualified Person as identified by Canadian National Instrument 43-101 Standards of Disclosure for Mineral Projects.

About Rio Grande Resources

Rio Grande Resources (CSE:RGR) is a burgeoning mineral exploration company focused on unlocking the high-grade gold and silver potential within its 3,000-acre drill-ready property in the Black Range of Sierra County, New Mexico. The company holds 100% interest in the Winston project group, which includes the 2 patented historic Ivanhoe & Emporia Claims, and Little Granite mines, all known for their past production of high-grade precious metals. Rio Grande Resources is led by a team of experienced professionals with expertise in mineral exploration and development, who are targeting large-scale precious metal discoveries within the property's well-documented low-sulfidation epithermal setting.

To view the company fact sheet and corporate presentation, please visit our website at www.riogranderesources.ca.

Contact and Information

Company
Jason Barnard, President CEO and Director
(604) 767-6598
jason.barnard@riogranderesources.ca

Investor Relations Contact
Lucas A. Zimmerman & Ian Scargill
MZ Group - MZ North America
(262) 357-2918
RGR@mzgroup.us
www.mzgroup.us

Follow us or contact us on social media
X: @RioGrandeRGR
LinkedIn: https://www.linkedin.com/company/rio-grande-resources-ltd/
Facebook: facebook.com/profile.php?id=61572800435230

Forward-Looking Statements

Except for the statements of historical fact contained herein, the information presented in this news release and oral statements made from time to time by representatives of the Company are or may constitute "forward-looking statements" as such term is used in applicable United States and Canadian laws and including, without limitation, within the meaning of the Private Securities Litigation Reform Act of 1995, for which the Company claims the protection of the safe harbor for forward-looking statements. Such forward-looking statements and forward-looking information include, but are not limited to, the proposed benefits of the Arrangement. These statements relate to analyses and other information that are based on forecasts of future results, estimates of amounts not yet determinable and assumptions of management. Any other statements that express or involve discussions with respect to predictions, expectations, beliefs, plans, projections, objectives, assumptions or future events or performance (often, but not always, using words or phrases such as "expects" or "does not expect," "is expected," "anticipates" or "does not anticipate," "plans," "estimates" or "intends," or stating that certain actions, events or results "may," "could," "would," "might" or "will" be taken, occur or be achieved) are not statements of historical fact and should be viewed as forward-looking statements. Such forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements of the Company to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such risks and other factors include, among others, the availability of capital to fund programs and the resulting dilution caused by the raising of capital through the sale of shares, continuity of agreements with third parties, the satisfaction of the conditions to the Arrangement, risks and uncertainties associated with the environment and delays in obtaining governmental approvals, permits or financing. Although the Company has attempted to identify important factors that could cause actual actions, events or results to differ materially from those described in forward-looking statements, there may be other factors that cause actions, events or results not to be as anticipated, estimated or intended. There can be no assurance that such statements will prove to be accurate as actual results and future events could differ materially from those anticipated in such statements. Although the Company believes that the expectations reflected in such forward-looking statements are based upon reasonable assumptions, it can give no assurance that its expectations will be achieved. Forward-looking information is subject to certain risks, trends and uncertainties that could cause actual results to differ materially from those projected. Many of these factors are beyond the Company's ability to control or predict. Important factors that may cause actual results to differ materially and that could impact the Company and the statements contained in this news release can be found in the Company's filings on SEDAR+. The Company assumes no obligation to update or supplement any forward-looking statements whether as a result of new information, future events or otherwise. Accordingly, readers should not place undue reliance on forward-looking statements contained in this news release and in any document referred to in this news release. This news release shall not constitute an offer to sell or the solicitation of an offer to buy securities. Please refer to the Company's most recent filings under its profile on SEDAR+ at www.sedarplus.ca for further information respecting the risks affecting the Company and its business.

The CSE has neither approved nor disapproved the contents of this news release and accepts no responsibility for the adequacy or accuracy hereof.

SOURCE: Rio Grande Resources



View the original press release on ACCESS Newswire

FAQ

What were the key gold and silver grades from RGRLF's Winston Project sampling?

The sampling revealed exceptional grades of up to 66.2 g/t gold and 830 g/t silver from the Paymaster Fault corridor.

How much copper was discovered in Rio Grande Resources' Winston Project?

One sample from a historic 20ft shaft assayed 2.76% Cu from a copper-oxidized andesite breccia.

What is the extent of mineralization at RGRLF's Winston Project?

The project confirmed 1.5km of continuous mineralization along the Paymaster Fault corridor.

What are the next steps for Rio Grande Resources at the Winston Project?

The company is conducting additional geological mapping and geophysical surveys to refine drill targets along the Paymaster Fault Corridor and other newly identified targets.

What types of mineralization were identified at RGRLF's Winston Project?

Three main types were identified: hydrothermal rhyolite breccias, andesite-hosted copper zones, and banded chalcedonic quartz breccias.
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