The Conversation (0)
Cross River Ventures Corp. (CSE: CRVC) (OTCQB: CSRVF) (FSE: C6R) (the "Company") is pleased to announce results from the Bear Head Zone maiden drill program at the McVicar Project, located 150km northeast of Red Lake Ontario. Highlights include:
- Discovery drill hole BH-02 intersected 0.5m of 41.1 g/t gold with visible gold in core at 153.75 m downhole (See Table 1 for complete results).
- Maiden 8-hole diamond drill program tested a new gold trend (the "Bear Head Zone") that was discovered in 2021 with surface samples grading up to 19.75 g/t Au (Press Release October 5, 2021).
- All 8 holes intercepted anomalous gold mineralization greater than 0.25 g/t Au (See Table 1).
- Planned follow-up work includes geophysics and step-out drill holes
In the summer of 2021, Cross River completed extensive targeted prospecting work on the McVicar Property located in the Archaean Lang Lake greenstone belt, which resulted in the discovery of a new surface gold trend, the "Bear Head Zone", which was drill tested by the company in winter 2022. The Bear Head Zone is a +700-meter long gold trend with surface samples returning up to 19.75 grams-per-tonne (g/t) gold over coincident LiDAR and magnetic features (Press Release October 5, 2021). No previous drilling has ever been completed at the Bear Head Zone target.
Figure 1 shows a map of drillhole locations at the Bear Head Zone.
Figure 1: Bear Head Zone drillholes and high-grade surface samples
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Eight diamond drillholes tested the Bear Head Zone during the winter 2022 program, and all holes intercepted anomalous gold mineralization greater than 0.25 g/t Au. Drilling identified an altered and mineralized corridor >710 m long, open to the east and west along strike.
Notable Drilling Intercepts (>0.5 g/t Au) at Bear Head Zone include:
BH-02:
- 5.23 meters at 0.51 g/t gold from 72.37 m downhole
- including 1.0 meters at 1.17 g/t gold
- 1.0 meters at 0.61 g/t gold from 90.0 m downhole
- 1.2 meters at 0.74 g/t gold from 117.0 m downhole
- 0.5 meters at 0.70 g/t gold from 150.1 m downhole
- 0.5 meters at 41.1 g/t gold (with visible gold in core) from 153.75 m downhole
BH-03:
- 1.0 meters at 0.97 g/t gold from 22 m downhole
- 0.47 meters at 3.23 g/t gold from 43.36 m downhole
- 1.15 meters at 0.97 g/t gold from 47.85 m downhole
BH-04:
- 1.0 meters at 0.90 g/t gold from 125 m downhole
- 1.0 meters at 0.81 g/t gold from 155 m downhole
BH-08:
- 1.0 meters at 1.1 g/t gold from 133 m downhole
Discovery Drillhole: BH-02
Hole BH-02 intersected 0.5m of 41.1 g/t gold in a smoky grey quartz vein with visible gold, chalcopyrite, and pyrrhotite at 153.75m downhole (117m vertical depth). The quartz vein cross-cuts a locally sheared mafic metavolcanic succession, with a feldspar-porphyry dyke cutting host rocks proximal to the vein footwall. The gold interval is located near the east-west trending contact between volcano-sedimentary host rocks and a tonalite intrusive body. The contact area is characterized by damage zones and abundant shearing, various styles of alteration and veining, as well as feldspar porphyry dikes.
Figure 2: a) BH-02 smoky-grey quartz vein (41.1 g/t Au over 0.50m), b) visible gold, chalcopyrite and pyrrhotite in brecciated grey-black quartz
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Geological mapping and 3-D modelling work indicates that this high-grade gold intercept projects to the surface along strike with the 19.75 g/t Au surface sample collected in 2021, as well as the 0.47m sample grading 3.23 g/t Au and 1.185% Cu from BH-03. (Figure 3).
Figure 3: Interpreted projection of high-grade intercepts from surface through BH-03 and BH-02
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Additional smoky grey quartz +/- sulfide veins up to 20 cm wide were intercepted in BH-02 and all other Bear Head Zone drillholes, contributing to a broad, low-grade gold envelope as indicated by the assays. The presence of high-grade mineralization, with visible gold, within a broad low-grade mineralized envelope, is typical in environments where gold is concentrated in plunging chutes. Table 1 shows the significant gold intercepts (>0.25 g/t) in each drill hole.
Table 1: Significant Gold Intercepts >0.25 g/t
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Drillhole Descriptions
BH-01 (Az: 180°, Dip: -50°)
BH-01 is the westernmost hole drilled at the Bear Head Zone and is designed to test an east-west trending quartz vein zone beneath the 1.415 g/t Au sample collected on surface in 2021. BH-01 cut 16 meters of overburden before intersecting chlorite-carbonate altered mafic metavolcanic rocks containing instances of moderate shearing with minor intervals of sericite-silica alteration, with up to 5% grey to white quartz veinlets. The best gold intercept occurs between 16-19 meters downhole and averages 0.356 g/t Au. Pyrite and pyrrhotite are present as fine disseminations and as a stringer veinlet network. At 78m, the hole intersected an intrusive tonalite body to EOH at 185.5m.
BH-02 (Az: 180°, Dip: -50°)
BH-02 was drilled 300m east of BH-01 and targeted an east-west oriented magnetic high feature located north of the quartz-veined topographic ridge system tested by BH-01. After 25 meters of overburden, the hole intersected an intensely sheared clastic sedimentary rock (argillite) that contains smokey quartz veins, disseminated pyrite and pyrrhotite. From 44 -163m downhole, chlorite-calcite altered mafic metavolcanic rocks were intersected, with locally strong shearing, and intermittent zones of moderate sericite and silica alteration. From 62-67m interbedded banded-iron-formations were noted, often with up to 8% banded pyrite and pyrrhotite. The mafic metavolcanic unit (72 to 155 meters downhole) contains narrow smoky grey and white quartz veinlets creating a broad low-grade gold halo (samples up to 1.17 g/t Au, 0.23% Cu over 1m), as well as a 0.5m meter sample with 41.1 g/t Au, where a 20cm (true width unknown) smoky quartz vein contains visible gold, chalcopyrite and pyrrhotite. At 163m the hole intersected tonalite intrusion to EOH at 206 meters.
BH-03 (Az: 180°, Dip: -50°)
BH-03 was drilled 100m east of BH-02 and targeted the quartz-veined ridge topographic high, specifically below the 19.75 g/t Au sample collected in 2021. After 15 meters of overburden the hole intersected chlorite altered mafic metavolcanic rocks to 117 meters downhole. The metavolcanic rocks are moderately sheared (locally) and contain smoky-grey and white quartz veins, quartz breccia, and sulfide stringers with sericite halos. From 20m to 105m downhole, a low-grade gold envelope is present (similar to BH-02). The highest grade sample was taken from a moderately veined interval with foliation-hosted pyrite, pyrrhotite and chalcopyrite, grading 3.23 g/t Au and 1.185% Cu over 0.47m. From 117m to 192m (EOH), the tonalite intrusion was intersected and intermittently cut by fine-grained mafic dykes.
BH-04 (Az: 180°, Dip: -50°)
BH-04 was drilled 100m east of BH-03 and targeted a quartz-vein topographic high ridge with a coincident magnetic anomaly (high). Below 28 meters of overburden the hole cut interbedded clastic metasedimentary rocks (argillite), mafic metavolcanic rocks, and banded iron-formations (locally enriched in arsenopyrite and pyrite) to 97m depth. From 97m to 181m, mafic metavolcanic rocks are present cut locally by fine-grained mafic intrusions (dykes). The mafic metavolcanic rocks are cut by 2-3% smoky-grey to white quartz veinlets which ran up to 0.895 g/t Au & 0.243% Cu over 1m. From 181m to 290m (EOH) the hole intersected tonalite intrusion cut by mafic dykes.
BH-05 (Az: 0°, Dip: -50°)
BH-05 was drilled toward the north and cut a topographic/magnetic low situated between the Bear Head Zone surface exposure and the Chellow Vein (600m to the north). After 26 meters of overburden, the hole intersected sheared argillite to 224m depth. The argillite is locally pyrite +/- pyrrhotite bearing in foliation parallel layering with occasional course arsenopyrite. From 224m to EOH at 449m, the hole intersected foliated chlorite-calcite altered mafic metavolcanic rocks (local argillite interbeds) with narrow zones of sulfides, and minor quartz-carbonate veining. The highest grade gold sample occurred at 63.4m in the sheared argillite, with 0.256 g/t Au, 32.6 g/t Ag, 0.483% Zn, and 0.476% As over 0.5m.
BH-06 (Az: 180°, dip: -50)
BH-06 was drilled 100m east of BH-04 and targeted a quartz-veined topographic high ridge system and coincident magnetic high anomaly. After 20 meters of overburden the hole cut the sheared argillite unit down to 59m, followed by banded iron formation interbedded with mafic metavolcanic rocks down to 67m downhole. From 67-165m, chlorite altered mafic metavolcanic rocks were cut by sparse intermediate to mafic dykes, and local zone of sericite + silica alteration. The mafic metavolcanic unit contains 2-5% smoky-grey to white quartz veins, with increasing sulfide abundance (pyrite + pyrrhotite + chalcopyrite) moving downhole, grading up to 0.42 g/t Au over 2m, and up to 0.16% Cu over 1m. From 165m to 225m the tonalite intrusion was intersected and intermittently cut by fine-grained mafic dykes.
BH-07 (Az: 0°, Dip: -50°)
BH-07 was drilled towards the north to test the topographic/ magnetic low situated between the Bear Head Zone surface exposure and the Chellow Vein (600m to the north). After 21 meters of overburden, the hole intersected the same lithologic sequence as BH-05, with strongly sheared argillite down to 234m, followed by chlorite-altered mafic metavolcanic rocks down to EOH at 489m. Within the mafic metavolcanic unit from 454-488m downhole, quartz + carbonate breccia veins up to 50cm wide with trace chalcopyrite, pyrrhotite and pyrite were intersected. The highest grade gold sample occurred at 429m downhole in the mafic metavolcanic rocks, with 0.267g/t Au over 2m.
BH-08 (Az: 180°, dip: -50)
BH-08 is the easternmost hole drilled at the Bear Head Zone and is designed to test an east-west trending quartz veined topographic ridge system. BH-08 cut 12 meters of overburden before intersecting sheared argillite containing local concentrations of banded sulfides (pyrite, pyrrhotite, and arsenopyrite), with samples in this unit grading up to 0.328% Zn and 0.471% As over 1m. At 74m, the hole intersected mafic metavolcanic rocks, cut by narrow smoky grey-white quartz veinlets and trace sulfides which ran up to 1.1 g/t Au over 1m, and 0.403% Cu and 0.269 g/t over 0.51m. From 185-245m (EOH) the hole intersected tonalite intrusion cut by minor mafic dykes.
Geologic Setting
The geology and mineralization encountered in the drill program are similar to that described at the historic Golden Patricia Mine, located along strike 30km to the SE along the Bear Head Fault Zone. The Golden Patricia Mine produced 619,796 oz at 15.2 g/t Aui, and is hosted in a continuous 40 cm wide smoky quartz vein with visible gold, pyrrhotite, chalcopyrite. Like the Bear Head Zone (McVicar Project), veining at Golden Patricia is also hosted in mafic metavolcanic rocks with feldspar porphyry intrusions, iron formations, and shearing. The Golden Patricia shear zone is interpreted as a splay of the Bear Head Fault.v
Cross River CEO, Alex Klenman stated: "We are pleased with the results of the company's initial drill test on the Bear Head trend. The Cross River technical team identified this area as a priority target for gold mineralization and drilling has now confirmed discovery in this highly prospective zone. We look forward to next steps on the large prospective McVicar property and to follow up drilling at Bear Head. We're also eager to see the results from drilling at the Altered Zone and anticipate receiving those sometime over the next few weeks."
"The discovery of high grade gold during the company's initial drill test at the Bear Head Zone represents a significant step forward for Cross River," said Dan MacNeil, P.Geo, of the Cross River Technical Team. "The Bear Head Zone is on trend with the Golden Patricia Mine, which produced more than half a million ounces of gold at an average grade of 15 grams per ton. The McVicar project is a flagship gold endowed exploration asset, and the presence of high grade gold increases our confidence in the potential of the project," continued Mr. MacNeil.
In addition to drill testing the Bear Head Zone during the winter 2022 drill program, 6 holes were drilled at the Altered Zone target to test strike and plunge continuity of known mineralization. Assays are pending and will be released once received, reviewed, and verified by the technical team.
Table 2: Bear Head Zone Collars
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About The Bear Head Trend
The Bear Head Trend was discovered in summer 2021 by Cross River Ventures field crews. The target is defined by a +700m strike of high-grade surface samples (up to 19.75 g/t Au - see News Release October 5th, 2021) following a prominent WNW trending topographic ridge system with mapped iron formation, sheared mafic meta-volcanics, and mineralized quartz veins. The Bear Head zone is located 600 meters south of the historic Chellow Vein near the southern contact between mafic volcanics and granite along the Bear Head Fault Zone. Drillholes were positioned to target the mineralized ridge system and coincident magnetic anomaly, as well as the topographic low situated between the Bear Head Trend and the Chellow Vein.
The Bear Head Trend is a previously undrilled high-grade gold corridor that is nested within a WNW trending multi-km braided damage zone structure. This geological environment is considered prospective for Archean greenstone gold deposits and contains favorable structural and lithological sites for gold deposition.
About The Altered Zone
The Altered Zone is a complex zone of deformation and intense alteration composed of sheared mafic volcanics, abundant green mica, intermediate intrusive rocks, massive to semi-massive quartz, and a quartz-carbonate-sericite schist.
New geologic modelling by Cross River in 2021 utilizes historic drilling data and suggests that the high-grade gold bearing structure continues at depth, coincident with lithologic breaks and a broader damage zone corridor characterized by an intense hydrothermal alteration overprint. The gold bearing structure at the Altered Zone is open in all directions. 2022 drillholes were positioned to target down-plunge extensions of known mineralization based on 3D modelling, as well as track the continuity of the structure to the south.
About the McVicar Project
Cross River's McVicar gold project is situated in the Superior Province of northern Ontario, Canada. The greenstone belts within the Superior Province contain some of the largest economic gold deposits in the world. McVicar encompasses the geologically significant structural components of the Lang Lake greenstone belt, an underexplored belt located approximately 40 km north of the historic Golden Patricia Mine (619,796 oz at 15.2 g/t Au)*.
The McVicar Gold Project is a district-scale (approximately 12,000 hectares) gold exploration project that contains gold prospective structure and host rocks that transect the entire Lang Lake greenstone belt, located in the Patricia Mining Division, approximately 150 km east of Red Lake, and 80 km west of Pickle Lake, in NW Ontario, Canada.
The property covers all the major fertile structural and lithostratigraphic elements of the greenstone belt, which is bound to the south by the major NW trending Bear Head Fault zone (within which the historic Golden Patricia Mine is situated).
Historic drilling at McVicar Lake in the Altered and North Flexure Zones include:
- 6.46 g/t Au over 10.09 m including 29.86 g/t Au over 1.86 metersii
- 5.5 g/t Au over 3.6 m including 12.2 g/t Au over 0.98 metersiii
The McVicar property also host the Chellow Vein zone, which is a narrow quartz vein that consists of smoky grey to white quartz mineralized with minor pyrite and visible gold. The vein system yielded high grade gold at surface including grab samplesiv that assayed 827.4 g/t Au and 578.1 g/t Auv.
Figure 4: McVicar Gold Project, location of nearby deposits and historical mines, NW Ontario
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Quality Assessment, Quality Control Protocols
Cross River has deployed an industry-standard quality-assurance/quality-control program during the 2022 drill program. This included the insertion of a sequence of standards, blanks, and duplicates into the sample string every tenth sample, in addition to industry standard chain of custody protocols for the samples. Core cutting was completed in Thunder Bay and samples were taken to ALS Global for multi-element analysis in addition to fire-assay of gold using analytical codes ME-MS61 and Au-ICP22. Overlimit analyses of gold (>10 g/t Au) was performed using Au-GRAV22.
Qualified Person
Daniel MacNeil, P.Geo., M.Sc., a Qualified Person as defined under National Instrument 43-101, reviewed, and approved the technical content disclosed in this press release. Historical assay results contained in this press release were not verified by the Company. However, the historical reports referenced were authored by experienced geoscientists and copies of laboratory assay sheets were commonly inserted in the reports.
About Cross River Ventures
Cross River is a gold exploration company focused on the development of top tier exploration properties located in emerging Greenstone Districts of NW Ontario, Canada. The Company controls a 28,000-ha, multiple project portfolio with highly prospective ground in and among prolific, gold bearing greenstone belts. Cross River's common shares trade in Canada under the symbol "CRVC" on the CSE, and in the US under the symbol "CSRVF" on the OTCQB. Please visit www.crossriverventures.com for more information.
On behalf of the Board of Directors of
CROSS RIVER VENTURES CORP.
Alex Klenman
CEO
604-227-6610
aklenman@crossriverventures.com
www.crossriverventures.com
Neither the Canadian Securities Exchange nor its Regulation Services Provider (as that term is defined in the policies of the Canadian Securities Exchange) accepts responsibility for the adequacy or accuracy of this release. This news release may contain forward-looking statements. These statements are based on current expectations and assumptions that are subject to risks and uncertainties. Actual results could differ materially because of factors discussed in the management discussion and analysis section of our interim and most recent annual financial statement or other reports and filings with the Canadian Securities Exchange and applicable Canadian securities regulations. We do not assume any obligation to update any forward-looking statements, except as required by applicable laws.
____________________________________________
i https://thediggings.com/mines/usgs10255075
*https://www.geologyontario.mndm.gov.on.ca/mndmfiles/mdi/data/records/MDI52O06SE00005.html
ii McKay D.B, 2004. Report on the 2003 Overburden Stripping, Geologic Mapping and Sampling Program conducted on the McVicar Lake Property: Continuum Resources Ltd and Prospector Consolidated Resources Inc. www.geologyontario.mndm.gov.on.ca/mndmfiles/afri/data/imaging/52O11SW2003/52O11SW2003.pdf
iii McKay D.B, 2004. Report on the 2003 Overburden Stripping, Geologic Mapping and Sampling Program conducted on the McVicar Lake Property: Continuum Resources Ltd and Prospector Consolidated Resources Inc. www.geologyontario.mndm.gov.on.ca/mndmfiles/afri/data/imaging/52O11SW2003/52O11SW2003.pdf
iv Grab samples are selective by nature and may not represent the true grade or style of mineralization across the property. Dr. Rob Carpenter, P.Geo., Ph.D., a Qualified Person as defined under National Instrument 43-101, reviewed, and approved the technical content disclosed in this press release. Historical assay results contained in this press release were not verified by the Company. However, the historical reports referenced were authored by experienced geoscientists and copies of laboratory assay sheets were commonly inserted in the reports.
v Waldie C.J. Report of Diamond Drilling McVicar Lake Area Patricia Mining Division: BHP Minerals Canada Ltd.
v https://www.geologyontario.mndm.gov.on.ca/mndmfiles/mdi/data/records/MDI52O06SE00005.html
Pinnacle Silver and Gold
Investor Insight
Pinnacle Silver and Gold presents a compelling investment opportunity in the precious metals sector as it continues to advance its flagship high-grade El Potrero project in Mexico and its Red Lake, Ontario assets. The company’s proven business model focuses on rapidly reactivating past-producing mines to generate early cash flow, while simultaneously exploring for district-scale potential, offering a strong value proposition in a bullish gold-silver environment.
Overview
Pinnacle Silver and Gold (TSXV:PINN,OTC:PSGCF,Frankfurt:P9J) is a promising player positioned for growth in the precious metals exploration sector, with its strategic focus on high-potential projects, commitment to responsible mining practices, and experienced leadership team.
Focused on silver and gold projects in the Americas, Pinnacle is strategically placed to capitalize on the growing demand for these valuable resources. Its core projects include the high-grade El Potrero gold-silver project in Mexico, and the Argosy gold mine and North Birch gold project in Ontario’s Red Lake District – each offering near-term development potential and strong exploration upside.
Pinnacle’s current flagship project, El Potrero, is located within the Sierra Madre Gold Silver Trend.
The company's investment appeal stems from several key factors:
- A robust pipeline of projects at various stages of exploration and development
- Strategic focus on high-potential areas in North and South America
- Effective capital management practices
- Aggressive expansion strategy through strategic acquisitions
The company’s business strategy involves the acquisition of past-producing mines that can be put back into production quickly to generate cash flow. By focusing on high-grade, underground mines, Pinnacle can leverage low capex, a smaller operational footprint, easier and faster permitting process and protection against metal price volatility. At the same time, the company conducts brownfield exploration for resource expansion, increasing its potential for district-scale discovery.
Pinnacle's emphasis on creating shareholder value is evident in its approach to project selection and development. The company's portfolio is carefully curated to balance near-term production potential with long-term growth prospects, offering investors exposure to both immediate returns and future upside.
Company Highlights
- Pinnacle Silver and Gold is a Canada-based exploration and development company dedicated to building long-term shareholder value with its silver- and gold-focused assets in North and South America.
- The company’s flagship El Potrero gold-silver project, located in Mexico’s Sierra Madre Belt, has returned exceptional underground sample grades up to 85.1 grams per ton (g/t) gold and 520 g/t silver, with exploration potential across a 1.6 km strike length.
- The 100-percent-owned Argosy gold mine and North Birch project are located in the Red Lake District in Northwestern Ontario, a region famous for gold production and high-grade underground mines.
- The company’s strategy is to generate near-term production from past-producing assets while growing its resource base through modern, brownfields exploration.
- Pinnacle is led by a highly experienced management team with a successful track record in advancing exploration-stage assets through to production.
Key Projects
El Potrero Gold-Silver Project
El Potrero is a high-grade, past-producing gold-silver project located in the prolific Sierra Madre Belt in Mexico, within 35 km of four operating mines, including Fresnillo’s 4,000 tpd Ciénega Mine. The project comprises two concession blocks totaling 1,074 hectares, which include the historic mines and a 100 tpd on-site processing plant.
Recent Developments (as of July 2025):
- Over 600 rock samples have been collected from underground and surface sources for geochemical analysis.
- Channel sampling at the Pinos Cuates mine returned assays of up to 85.1 g/t gold and 520 g/t silver over 0.5 m, and composite intervals of 50.3 g/t gold and 269 g/t silver over 1.7 m.
- Geological interpretation highlights a significant quartz-feldspar porphyry dyke as a structural control on gold-silver mineralization.
- The Dos de Mayo vein system has been mapped over 1.6 km with trench and underground samples showing high-grade mineralization, including 13.2 g/t gold and 2,280 g/t silver from surface grab samples.
- Work is underway to design an underground and surface drill program to define continuity and guide future mine development.
- A site inspection of the 100 tpd plant confirmed that the base infrastructure is sound. Refurbishment of key equipment (crusher, mill, Merrill Crowe circuit) is being planned.
- Permitting efforts are progressing efficiently, aided by the site's historical disturbance. Baseline studies and formal permitting proposals are underway.
Pinnacle can earn an initial 50 percent interest upon production and increase its ownership of El Potrero to 100 percent subject to a 2 percent NSR, primarily through cash flow-funded payments, offering a low-dilution path to full ownership.
Argosy Gold Mine
Located within the Birch-Uchi Greenstone Belt in Ontario’s Red Lake District, and approximately 10 km from First Mining’s Springpole deposit, the Argosy gold mine produced 101,875 ounces at 12.7 g/t gold from 1931 to 1952. Pinnacle owns 100 percent of the project, subject to a 2.5 percent NSR.
Exploration Highlights:
- Past drilling intersected high-grade mineralization, including:
- 14.67 g/t gold over 1.7 m (No. 3 Vein)
- 12.02 g/t gold over 1.29 m (No. 8 Vein)
- 11.75 g/t gold over 1.55 m (No. 2 Vein)
- The project offers strong depth potential, with 2002–2004 drilling intersecting multiple new veins and gold mineralization extending to 400 m vertical depth.
North Birch Gold Project
Located 4 km from the Argosy Mine, North Birch is a 3,850-hectare grassroots project with major upside. The property lies in an underexplored section of the Birch-Uchi Belt and covers a folded and sheared iron formation, interpreted as analogous to Newmont’s Musselwhite Mine.
Exploration Work:
- LiDAR surveys and IP geophysics have revealed 8+ km of structural breaks with multiple drill targets.
- 2022 drilling intersected anomalous gold and copper mineralization within structurally deformed and altered iron formations, confirming the favorable structural setting
Management Team
Robert Archer - President, CEO and Director
Robert Archer has more than 40 years’ experience in the mining industry, working throughout the Americas. After spending more than 15 years with major mining companies, Archer held several senior management positions in the junior mining sector and co-founded Great Panther Mining, a mid-tier precious metals producer, where he served as president and CEO from 2004 to 2017 and director until 2020. He joined Pinnacle as a director in March 2018 followed by his appointment as CEO in January 2019 and president in October 2021. Archer is a professional geologist and holds an Honours BSc from Laurentian University in Sudbury, Ontario.
David Cross - CFO
David Cross is a CPA and CGA with over 21 years’ experience in the junior sector with a focus on finance and corporate governance. He is currently a partner of Cross Davis and Company LLP Chartered Professional Accountant, which specializes in accounting and management services for private and publicly listed companies within the mining industry, and has recently been appointed CFO of Ashburton Ventures.
Colin Jones - Independent Director
Colin Jones is principal consultant for Orimco Resource Investment Advisors in Perth, Australia. He has almost 40 years’ experience as a mining, exploration and consulting geologist in a number of different geological environments on all continents. He has managed large exploration and due diligence projects, and has undertaken numerous bankable technical audits, technical valuations, independent expert reports and due diligence studies worldwide, most of which were on behalf of major international resource financing institutions and banks. Jones holds a Bachelor of Science (Earth Sciences) degree from Massey University, NZ.
David Salari - Independent Director
David Salari has worldwide experience in the design, construction and operation of extractive metallurgical plants. He is an engineer with more than 35 years of experience in the mining and mineral processing field. He is currently the president and CEO of DENM Engineering.
Ron Schmitz - Independent Director
Ron Schmitz is the principal and president of ASI Accounting Services, providing administrative, accounting and office services to public and private companies since July 1995. Schmitz has served as a director and/or chief financial officer of various public companies since 1997, and currently holds these positions with various public and private companies.
Sun Summit Provides Exploration Update from the JD Project in BC's Toodoggone District; Over 3,100 Meters of Drilling Completed at the Creek Zone
- Drilling nearly complete at the Creek zone: Over 3,100 meters of drilling have been completed across ten holes at the Creek zone, with additional drill holes planned. The holes investigated the extent and continuity of near-surface, high-grade and bulk-tonnage gold mineralization. Historical and recent highlight intercepts from 2024 drilling at the Creek zone include:
- 122.53 m of 2.11 g/t Au including 1.5 of 121.0 g/t Au (CZ-24-0047)
- 54.95 m of 2.69 g/t Au including 19.50 m of 7.31 g/t Au (CZ-24-0058)
- 22.0 m of 11.7 g/t Au including 4.0 m of 61.2 g/t Au (CZ97-0085)
- Drilling to follow at the Finn zone where up to 2,000 meters are planned: Holes are designed to evaluate the extent and continuity of high-grade and bulk-tonnage gold-silver mineralization. Historical highlight intercepts (Figure 4) include:
- 35.7 m of 7.26 g/t Au, 94 g/t Ag including 1.0 m of 215.4 g/t Au, 308 g/t Ag (JD95-0472)
- 45.0 m of 3.02 g/t Au, 143 g/t Ag including 5.0 m of 8.18 g/t Au, 918 g/t Ag (JD95-0762)
- 20.85 m of 8.76 g/t Au, 68 g/t Ag including 11.0 m of 15.1 g/t Au,108 g/t Ag (JD95-0972)
- 22.0 m of 6.32 g/t Au, 46 g/t Ag including 12.6 m of 10.8 g/t Au, 66 g/t Ag (JD12-0033)
- Project-wide exploration activities focused on drill target refinement are ongoing, including:
- Over 20 line-km of induced polarization (IP) geophysics has been completed along the JD Porphyry Trend. Infill surveying across the Finn to Creek corridor is set to commence in the coming weeks.
- Over 1,600 soil samples have now been collected across the Belle South grid, the southern extent of the JD Porphyry trend, and the Kadah grid near the Finn to Creek corridor.
- Geological mapping and prospecting are ongoing with a current focus on McClair Creek which transects the JD Porphyry Trend as well as the McClair East area.
"Our fully funded $6 million exploration program designed to systematically advance and expand the gold-silver targets at JD is progressing nicely," said Niel Marotta, CEO of Sun Summit Minerals. "We have made terrific progress at Creek Zone. We are excited about the upcoming drilling at the Finn Zone, where we plan to test the extent of gold mineralization while also investigating a zone of strong silver mineralization, recently modelled through our comprehensive compilation efforts. We expect to begin reporting results from drilling completed at the Creek Zone in the coming weeks, with results from additional targets to follow."
2025 JD Exploration Program
The primary exploration goals at JD in 2025 are to advance and expand the Creek and Finn gold-silver targets and to generate and refine new priority targets across the project. Work is currently focused on the highly prospective 4.5 km long epithermal-related Finn to Creek corridor, as well as the 12 km long JD Porphyry trend (Figure 1).
Drilling update:
Over 3,100 meters of drilling has been completed at the Creek zone with holes collared along a 500-meter northwest-southeast trend. Ten holes investigated the extent and continuity of near-surface, high-grade and bulk-tonnage gold mineralization (e.g., 122.53 m of 2.11 g/t Au including 1.5 of 121.0 g/t Au in CZ-24-0047 and 22.0 m of 11.7 g/t Au including 4.0 m of 61.2 g/t Au in CZ97-0085, Figure 3). Holes were designed to systematically test the vein-controlling structures on 50 to 100 meter pierce-points covering a strike-length of over 500 meters and a down-dip extent of over 200 meters.
Up to 2,000 meters of drilling is planned at the Finn zone with holes designed to investigate the down-dip, strike extent and continuity of near-surface, high-grade and bulk-tonnage gold-silver mineralization (e.g., 35.7 m of 7.26 g/t Au, 94 g/t Ag including 1.0 m of 215.4 g/t Au, 308 g/t Ag in JD95-0472 and 20.85 m of 8.76 g/t Au, 68 g/t Ag including 11.0 m of 15.1 g/t Au,108 g/t Ag in JD95-0972, Figure 4).
Modelling of recently compiled historical Finn zone drill data has outlined a compelling zone of strong silver-gold-base metal mineralization (e.g., 45.0 m of 3.02 g/t Au, 136 g/t Ag including 5.0 m of 8.18 g/t Au, 918 g/t Ag in JD95-0762). Planned drilling at Finn will also be aimed at investigating the structural and/or lithological controls on this gold-associated, silver-rich mineralization.
Target generation update: Project-wide exploration activities aimed at target generation and drill target refinement are ongoing, including:
- Over 20 line km of induced polarization (IP) geophysical surveying has been completed along the JD Porphyry trend east of the Finn Zone. Additional surveying is set to commence in the coming weeks covering parts of the Finn to Creek corridor to infill historical gaps.
- Over 1,600 soil samples have now been collected across the Belle South grid, southern extent of the porphyry trend (Figure 2) and the Kadah grid which covers a highly prospective area south of the Finn to Creek corridor lacking historical soil coverage.
- Geological mapping and prospecting are ongoing with a current focus on McClair Creek which transects the JD Porphyry trend. Mapping has also been completed along the Finn to Creek corridor as well as the Oxide Peak West target. Mapping will continue east towards the East McClair copper target.
Timeline: Drilling and complementary exploration activities are anticipated to continue into early October. Soil and rock samples and drill core samples from the first eight holes at Creek zone have now been submitted to the lab for assay analyses. Results will be released once compiled and interpreted.
Figure 1. Map of the Toodoggone District showing the location of the JD Project in relation to other development and exploration projects. Data sourced from Thesis, TDG and Centerra's corporate websites.
Figure 2. Map of the JD Project showing the broad JD Porphyry trend and the epithermal-related Finn to Creek Corridor. Areas with completed IP and soil surveys are shown in grey. Areas with ongoing and planned geological mapping are shown in orange. Key targets are highlighted.
Figure 3. Map of the Creek Zone showing previous drill collar locations with selected highlights. The area targeted for 2025 drilling is outlined in red. See references below for data sources.
Figure 4. Map of the Finn Zone showing historical drill collar locations with selected highlights. The area targeted for 2025 drilling is outlined in red. See references below for data sources.
National Instrument 43-101 Disclosure
This news release has been reviewed and approved by Sun Summit's Vice President Exploration, Ken MacDonald, P. Geo., a "Qualified Person" as defined in National Instrument 43-101 Standards of Disclosure for Mineral Projects of the Canadian Securities Administrators. Some technical information contained in this release is historical in nature and has been compiled from public sources believed to be accurate. The historical technical information has not been verified by Sun Summit and may in some instances be unverifiable dependent on the existence of historical drill core and grab samples.
Community Engagement
Sun Summit is engaging with First Nations on whose territory our projects are located and is discussing their interests and identifying contract and work opportunities, as well as opportunities to support community initiatives. The Company looks forward to continuing to work with local and regional First Nations with ongoing exploration.
About the JD Project
The JD Project is located in the Toodoggone mining district in north-central British Columbia, a highly prospective deposit-rich mineral trend. The project covers an area of over 15,000 hectares and is in close proximity to active exploration and development projects, such as Thesis Gold's Lawyers and Ranch projects, TDG Gold's Baker-Shasta projects, Amarc Resource's AuRORA project, Centerra's Gold's Kemess East and Underground projects, as well as the past-producing Kemess open pit copper-gold mine.
The project is 450 kilometres northwest of the city of Prince George, and 25 kilometres north of the Sturdee airstrip. It is proximal to existing infrastructure in place to support the past-producing Kemess mine, including roads and a hydroelectric power line.
The JD Project is in a favourable geological environment characterized by both high-grade epithermal gold and silver mineralization, as well as porphyry-related copper and gold mineralization. Some historical exploration, including drilling, geochemistry and geophysics, has been carried out on the property, however the project area is largely underexplored.
About Sun Summit
Sun Summit Minerals (TSXV: SMN) (OTCQB: SMREF) is a mineral exploration company focused on the discovery, expansion and advancement of district scale gold and copper assets in British Columbia. The Company's diverse portfolio includes the JD and Theory projects in the Toodoggone region of north-central B.C., and the Buck Project in central B.C.
Further details are available at www.sunsummitminerals.com.
References
- Krause, R.G. (1995), 1994 Geological and Geochemical Report on the JD Gold Silver Property, Toodoggone River Area, Omineca Mining Division, British Columbia, Assessment Report Indexing System, Report 23663, https://apps.nrs.gov.bc.ca/pub/aris.
- Krause, R.G. (1996), 1995 Geological Report on the JD Gold Silver Property, Toodoggone River Area, Omineca Mining Division, British Columbia, Assessment Report Indexing System, Report 24284, https://apps.nrs.gov.bc.ca/pub/aris.
- McBride, S. (2013), 2012 Geological, geochemical and diamond drilling report on the JD Property, Assessment Report Indexing System, Report 33556, https://apps.nrs.gov.bc.ca/pub/aris.
- McBride, S. and Leslie, C. (2014), 2013 Geological, geophysical and diamond drilling report on the JD Property, Assessment Report Indexing System, Report 34762, https://apps.nrs.gov.bc.ca/pub/aris.
- Hawkins, P.A. (1998), 1997 Exploration Report on the Creek Zone for Antares Mining and Exploration Corporation and AGC Americas Gold Corporation, JD Property, Toodoggone River Area, Omineca Mining Division, Internal Report #98-065-1.
- Davis, J.W., and Jamieson, M.D. (1998), Drilling and Geophysical Report on the M.H. Mineral Clain Group, Toodoggone District, Assessment Report Indexing System, Report 25757, https://apps.nrs.gov.bc.ca/pub/aris.
- Sun Summit Minerals news release October 2, 2024
- Sun Summit Minerals news release October 16, 2024
Link to Figures
Figure 1: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/08/SMN_Figure-1_20250819.jpg
Figure 2: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/08/SMN_Figure-2_20250819-scaled.jpg
Figure 3: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/08/SMN_Figure-3_20250819-scaled.jpg
Figure 4: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/08/SMN_Figure-4_20250819-scaled.jpg
On behalf of the board of directors
Niel Marotta
Chief Executive Officer & Director
info@sunsummitminerals.com
For further information, contact:
Matthew Benedetto, Simone Capital
mbenedetto@simonecapital.ca
Tel. 416-817-1226
Forward Looking Information
Statements contained in this news release that are not historical facts may be forward-looking statements, which involve risks, uncertainties and other factors that could cause actual results to differ materially from those expressed or implied by such forward-looking statements. In addition, the forward-looking statements require management to make assumptions and are subject to inherent risks and uncertainties. There is significant risk that the forward-looking statements will not prove to be accurate, that the management's assumptions may not be correct and that actual results may differ materially from such forward-looking statements. Accordingly, readers should not place undue reliance on the forward-looking statements. Generally forward-looking statements can be identified by the use of terminology such as "anticipate", "will", "expect", "may", "continue", "could", "estimate", "forecast", "plan", "potential" and similar expressions. Forward-looking statements contained in this press release may include, but are not limited to, the timing of and size and scope of the drill program at the JD property; the Company's exploration plans, expectations and forecasts. These forward-looking statements are based on a number of assumptions which may prove to be incorrect which, without limiting the generality of the following, include: the Company's ability to complete the drill program as currently contemplated; risks inherent in exploration activities; volatility and sensitivity to market prices; volatility and sensitivity to capital market fluctuations; and fluctuations in metal prices. The forward-looking statements contained in this news release are made as of the date hereof or the dates specifically referenced in this press release, where applicable. Except as required by applicable securities laws and regulation, Sun Summit disclaims any intention or obligation to update or revise any forward-looking statement, whether as a result of new information, future events or otherwise, except as required by applicable securities laws. All forward-looking statements contained in this press release are expressly qualified by this cautionary statement.
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 release.
