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The Board of Inca Minerals Limited (ASX: ICG) (Inca or the Company) is pleased to provide shareholders a progress report on due diligence associated with the recently announced (ASX 5 February 2025) Binding Implementation Agreement to acquire Stunalara Metals Limited (Stunalara) via an off market takeover bid. Stunalara’s key asset is the high-grade gold & gold- antimony Hurricane Project located approximately 110km west-northwest of Cairns and 75km southwest of Port Douglas in North Queensland. Hurricane boasts multiple undrilled high-grade gold & gold-antimony prospects developed from rock chip and grab sampling.
Inca’s technical team recently conducted a site visit as part of the due diligence process to confirm and replicate historical geochemical data, culminating with the collection and dispatch for assaying of 84 rock chip samples. Assays have now been received for those samples with exceptional results recorded for gold (Au) and antimony (Sb) at multiple prospects including Holmes, Cyclone, Tornado, Hurricane and Bouncer confirming the high-grade prospectivity of the Hurricane Project.
Assay Highlights (Refer to table 1, Appendix 1 for full results)
Assays with gold greater than 5g/t:
- Hurricane South - Sample MC0374: 81.5g/t Au
- Hurricane North - Sample MC0368: 12.95g/t Au
- Hurricane South - Sample MC0379: 11.9g/t Au
- Bouncer - Sample HRX10042: 8.29g/t Au and 12.7% Sb.
- Typhoon - Sample HRX10055: 7.84g/t Au
- Holmes - Sample HRX10083: 6.4g/t Au
- Holmes - Sample MC0392: 6g/t Au
- 2 other samples returned gold greater than 4g/t, three with grades over 3g/t and 12 with grades over 1g/t.
Highly anomalous levels of Antimony (Sb) were also recorded, which included:
- Bouncer - Sample HRX10029 with 35.1% Sb
- Bouncer - Sample HRX10036: 20.8% Sb
- Bouncer - Sample HRX10042: 12.75% Sb
- Bouncer - Sample HRX10037: 9.54% Sb
- Bouncer - Sample HRX10033: 7.78% Sb
- Holmes - Sample MC0393: 5.28% Sb, and
- Holmes - Sample MC0398: 4.89% Sb
29 samples returned highly anomalous arsenic values > 0.1% (>1000ppm As, up to 9840ppm in 1 sample).
“The identification of high-grade gold and antimony in rock chips across different locations which have never been drilled, highlights the significant exploration potential of the Hurricane Project for the discovery of gold and antimony. Inca Minerals is looking forward to progressing follow-up exploration programs to build on this significant rock chip data,” said Inca Exploration Manager, Dr Emmanuel Wembenyui.
In addition to gold, the Hurricane Project results include high levels (up to 35%) of antimony, a critical and new economy metal. Antimony is listed as a critical mineral by the United States, the European Union, Japan, India, the United Kingdom and the Commonwealth of Austalia. New economy metals are pivotal for modern technologies, economies and national security, providing direct support for technologies that are paving the way to the transition from fossil fuels to net zero emmisions , advanced manufacturing and defence technologies/capabilities amongst other applications.
HURRICANE PROJECT
Inca is pleased to report highly encouraging results from a geological reconnaissance field trip to the gold and antimony Hurricane Project. The Hurricane Project is located about 110km west-northwest of Cairns and 75km southwest of Port Douglas in North Queensland, Figure 1.
The Hurricane Project comprises three tenements – EPM 19437, which hosts the Holmes, Porphyry, Monsoon and Cyclone prospects, EPM 25855 in which are located the Hurricane and Tornado Prospects, and EPM 27518, which hosts the Bouncer prospect, Figure 1.
Figure 1: Hurricane Project location map showing all three tenements, prospects and sample locations. The samples have been thematically mapped by gold, demonstrating the widespread occurrence of high-grade gold across the project. The project is sandwiched by 2 major northwest-southeast trending faults being the Hurricane and the Retina Faults. Locally, the project area is dominated by the Hodgkinson Formation and 2 late-stage felsic intrusions located within EPM 19437. Shown in the inset is the location of the Hurricane Project in North Queensland relative to the major towns of Cairns, Townsville and Brisbane.
Geology of the Hurricane Project Regional Geology
The Hurricane Project area falls within the Mossman 1:250,000 and the Mount Mulligan 1:100,000 Queensland Geological map sheets. The regional geology traverses a wide Geological Timescale from the Devonian in the Hodgkinson Formation through granodiorite and rhyolitic Carboniferous and Permian intrusions to Triassic and Quaternary Sandstones. The Hodgkinson Formation comprises dark grey to greenish, fine to medium quartz greywackes interbedded with siltstones, mudstones and conglomerates. The Carboniferous to Permian granitic/granodiorite and rhyolite intrusions comprise a suite of felsic porphyritic intrusions. The main porphyritic bodies comprise medium to coarse-grained mineral crystals including euhedral hornblende- biotite, k-feldspar and quartz, which locally grade into fine-grained silicified granites.
Local Geology
The three tenements which make up the Hurricane Project are structurally set within two major NW-SE trending faults, being the Hurricane Fault and the Retina Fault. The Hodgkinson Formation dominates these tenements and comprises of tightly folded greywackes, siltstones, shales, cherts, conglomerates and limestones. Locally within the Hurricane Project are 2 felsic intrusions, which occur in EPM 19437 and are predominantly porphyritic granites. These intrusions are the major source of heat, which mobilised hydrothermal fluids to interact with surrounding country rock, leading to widespread alteration in the form of silicification, sericite and carbonates, and account for the deposition of epithermal gold, silver, and antimony mineralised veins. Epithermal gold deposits are strongly associated with hydrothermal fluids that are related to calc-alkaline volcanism and magmatism. Plots of La-Y-Nb on the ternary diagram of Cabanis and Lecolle, 1989; shows that the Hurricane Project falls within the Arc Calc-Alkaline geo-tectonic setting, supporting an epithermal exploration model for the project (Figure 2). Epithermal gold could be low or high sulfidation, depending on mineralogy and can occur as veins, stockworks, replacements or disseminations. Mineralisation within the project area is associated with variably altered, silicified and brecciated quartz veins ranging in widths from 2 to >50m and lengths over 700m. The mineralogy of the Hurricane Project which includes gold, antimony, silver, very limited sulphur, +/- lead and zinc, leans towards the low sulfidation model.
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This article includes content from Inca Minerals Limited, licensed for the purpose of publishing on Investing News Australia. This article does not constitute financial product advice. It is your responsibility to perform proper due diligence before acting upon any information provided here. Please refer to our full disclaimer here.
High Grade Gold Intercepts Confirm Kpali Discovery
- Extremely strong gold intercepts from eight-hole RC drilling programme at Kpali Gold Prospect in Ghana’s Upper West Region.
- All eight holes intersected shallow mineralisation with better intercepts including:
- 12m at 8.29g/t Au from 25m (24KPRC010) incl.
- 6m at 11.60g/t Au from 31m and
- a peak 1m intercept of 20.43g/t Au at 36m and
- 4m at 4.16g/t Au from 95m.
- 7m at 2.23g/t Au from 35m (24KPRC011) incl.
- 4m at 3.23g/t Au from 35m and
- 11m at 2.24g/t Au from 50m incl.
- 1m at 8.29g/t Au from 57m.
- 5m at 3.66 g/t Au from 78m (24KPRC012) incl.
- 2m at 7.09g/t Au 79m.
- 13m at 1.58g/t Au from 73m (24KPRC014) incl.
- 1m at 5.62g/t Au from 79m.
- 1m at 8.35g/t Au from 5m (24KPRC015) and
- 9m at 4.81g/t Au from 107m incl.
- 2m at 8.75g/t Au from 109m.
- 1m at 6.64g/t Au from 70m (24KPRC016).
- 7m at 1.67g/t Au from 39m (24KPRC017) and
- 3m at 3.08g/t Au from 78m.
- 12m at 8.29g/t Au from 25m (24KPRC010) incl.
- Status of Kpali Gold Prospect considerably upgraded.
- Broader district containing several other high conviction prospects confirmed as an emerging new exploration frontier.
- Next drilling programme to comprise step-out drilling at Kpali Gold Prospect and testing of other prospects including equally prospective Bundi discovery.
- Results hot on heels of recent Kandia “4000 Zone” RC programme that confirmed good gold continuity and returned strong intercepts including:
- 7m at 3.36g/t Au from 149m within 24m at 1.78g/t Au from 139m (24KARC002) and
- 5m at 3.49g/t Au from 82m within 11m at 2.26g/t Au from 79m (24KARC004).
- Immediate high-level objective is to confirm robust new West African mining camps at Kpali and Kandia and an initial 1.0Moz Au multi-prospect based mineral resource.
Castle Executive Chairman, Stephen Stone, commented “The Kpali Gold Prospect is developing into a robust discovery and is a strong indicator that we may be dealing with a new West African gold mining camp in Ghana’s emerging northern region.
The latest intercepts include some very decent widths and grades at shallow depths with good continuity which can have considerable positive impacts should mining be considered.
Fig 1: Kpali Gold Prospect: Plan showing latest drill results and outline of interpreted multiple mineralised sub-parallel lodes on simplified sub-surface geology.
We have intersected a very impressive 12m at 8.29g/t Au from 25m, including 6m at 11.60g/t Au from 31m and a peak 1m intercept of 20.43g/t Au at 36m in a ‘hangingwall’ lode, and also 4m at 4.16g/t Au from 95m in a lower ‘footwall’ lode.
Apart from these standout results, very strong mineralisation has been encountered within most holes drilled, implying that with additional drilling we may be able to delineate a decent high value deposit.
We are very keen to get back drilling and to extend the Kpali Gold Prospect discovery as well as to follow-up historical drilling at the nearby Bundi discovery, 4km north.
There are also several other enticing prospects in the broader Kpali Gold Project area.
These drilling results follow excellent recent results from four holes at the Kandia Prospect, a second and separate gold discovery associated with a relatively under- explored 16km prospective contact between Birimian metasediments and a granite intrusion. Recent intercepts at Kandia included 7m at 3.36g/t Au from 149m within 24m at 1.78g/t Au from 139m and 5m at 3.49g/t Au from 82m within 11m at 2.26g/t Au from 79m.
These deposits lie in a classic setting for major gold deposits in West Africa and in particular northern Ghana which hosts the Cardinal Resources 5.1Moz gold Namdini deposit and the Azumah Resources 2.8Moz gold Black Volta Gold Project. The latter’s high-grade Julie deposit is immediately along strike from Kandia.
West Africa is where big gold discoveries can be and are still being made. With the gold price now at a level I could only dream of when starting my career, it’s the perfect time to be exploring Castle’s two new discoveries in the very stable, safe and mining friendly jurisdiction of Ghana.”
Fig 2: North-south long-section through mineralised hangingwall and footwall lodes at Kpali highlighting zones of shallow plunging, high-grade gold mineralisation.
Additional intercepts included 7m at 2.23g/t Au from 35m(24KPRC011) including 11m at 2.24g/t Au from 50m, 5m at 3.6g/t Au from 78m (24KPRC012), 9m at 4.81g/t Au from 107m (24KPRC015) and 3m at 3.08g/t Au from 78m (KPRC017).
These results confirm the Kpali Gold Prospect, just one of several prospects within the broader Kpali Gold Project, as a robust discovery in a completely new district within Ghana’s emerging Northern Region exploration frontier.
With several other high conviction prospects yet to be evaluated in the area, including the nearby Bundi, Kpali East, Wa South East and Wa South West prospects, there appears to be present all the hallmarks of a new West African mining camp and the possibility of a considerable gold endowment.
The Kpali Gold Prospect lies within a mineralised corridor associated with a 30m to 50m wide zone of structural deformation immediately west of a granite intrusion. Three drilling programmes have identified near-surface, shallow plunging high-grade lode-style mineralisation to a depth of at least 100m. Multiple, closely-spaced mineralised lodes have been identified over at least 650m strike.
Overall, the geological setting at the broader Kpali Gold Project is of typically structurally-controlled, orogenic style mineralisation within Birimian terrane. This is a similar setting as that hosting several world- class gold mining operations in Ghana and West Africa generally. Orebodies with these characteristics can often extend to considerable depth.
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This article includes content from Castle Minerals Limited, licensed for the purpose of publishing on Investing News Australia. This article does not constitute financial product advice. It is your responsibility to perform proper due diligence before acting upon any information provided here. Please refer to our full disclaimer here.
Top 10 Central Bank Gold Reserves
Central banks added 1,044.6 MT of gold to their vaults in 2024, the third year in a row that gold purchases in this segment surpassed the 1,000 MT mark. In the fourth quarter of 2024 alone, central banks picked up another record 332.9 MT of gold, reported the WGC.
Chart via the WGC.
Twenty-nine percent of the WGC's survey respondents indicated plans to grow their gold reserves, up 5 percent from the previous year. Three percent reported their institution is planning to decrease its gold holdings, which was unchanged from the previous year.
The WGC believes that central bank gold purchases will continue to be a major driver of gold demand in 2025.
Which central banks hold the most gold?
Read on to find out the 10 top countries by central bank gold holdings, as per data from the WGC, including recent Q4 2024 and full-year 2024 reports.
1. United States
Gold reserves: 8,133.46 metric tons
When it comes to the largest gold depository in the world, the American central bank is number one with 8,133.46 metric tons.
A large percentage of US gold is held in “deep storage” in Denver, Fort Knox and West Point. As the US Treasury explains, deep storage is “that portion of the US Government-owned gold bullion reserve which the Mint secures in sealed vaults that are examined annually by the Treasury Department’s Office of the Inspector General and consists primarily of gold bars.”
The rest of US-owned reserves are held as working stock, which the country's mint uses as raw material to mint congressionally authorized coins.
2. Germany
Gold Reserves: 3,351.53 metric tons
The Bundesbank, Germany’s central bank, currently owns 3,351.53 metric tons of gold. Like many of the central banks on this list, the German national bank stores over half of its stock in foreign locations in New York, London and France.
The Bundesbank’s foreign gold reserves came into question in 2012, when the German Federal Court of Auditors, the Bundesrechnungshof, was openly critical of the Bundesbank’s gold auditing.
In response, the German bank issued a public statement defending the security of foreign banks. Privately, the Bundesbank then began the arduous process of repatriating its gold stock back to German soil. By 2016, more than 583 MT of gold had been transferred back to Germany.
Nearly half of Germany’s gold holdings are stored in Frankfurt, while more than a third are in New York, an eighth of its holdings are in London, and a miniscule amount are held in in Paris.
3. Italy
Gold Reserves: 2,451.84 metric tons
Banca d’Italia, the national bank of Italy, began amassing its gold in 1893, when three separate financial institutions merged into one. From there, its 78 MT slowly grew into the 2,451.84 MT the country now owns.
Like Germany, Italy stores parts of its reserves offshore. In total, 141.2 MT are located in the UK, 149.3 are in Switzerland and 1,061 are kept in the US Federal Reserve. Italy houses 1,100 MT of gold domestically.
4. France
Gold Reserves: 2,437 metric tons
The Banque de France has 2,437 MT of gold reserves, all of which it keeps on hand. The precious metal is stored in the bank’s secure underground vault, dubbed La Souterraine, which is located 27 meters below street level.
La Souterraine’s gold vaults are one of the four designated gold depositories of the International Monetary Fund.
According to Investopedia, the collapse of the Bretton Woods gold standard system was in part due to former French President Charles de Gaulle, who “called the U.S. bluff and began actually trading dollars in for gold from the Fort Knox reserves.” At the time, US President Richard Nixon “was forced to take the U.S. off the gold standard, ending the dollar's automatic convertibility into gold.”
5. Russia
Gold Reserves: 2,332.74 metric tons*
The Bank of Russia is the official central bank of the Russian Federation and owns 2,332.74 MT of gold. Like France, Russia’s central bank has opted to store all its physical gold domestically. The Bank of Russia stores two-thirds of its gold reserves in a bank building in Moscow, and the remaining one-third in Saint Petersburg.
The majority of the yellow metal is in the form of large, variable-weight standard gold bars weighing between 10 and 14 kilograms. There are also smaller bars on site weighing as much as 1 kilogram each.
Russia, which is the second largest gold producer by country, has been a steady purchaser of the precious metal since roughly 2007, with sales ramping up significantly between 2015 and 2020. However, Russia’s refineries were banned from selling gold bullion into the London market following the country’s invasion of Ukraine. Sanctions by the west also include a freeze on about half of Russia’s gold reserves.
In early 2022, Russia tied its currency, the ruble, to the yellow metal. "The plan was to shift the currency away from a pegged value and into the gold standard itself so the ruble would become a credible gold substitute at a fixed rate," according to Robert Huish, an Associate Professor in International Development Studies at Dalhousie University.
*This figure does not reflect year-end 2024, including the at least 3.1 MT purchased in 2024, per the WGC, which is awaiting further data to update the 2024 total.
6. China
Gold Reserves: 2,279.56 metric tons
The central bank for Mainland China is the People’s Bank of China (PBoC), located in Beijing. According to the WGC, the national financial institute stores 2,279.56 MT of gold, most which has been purchased since 2000. In 2001, the PBoC had 400 MT of gold in reserve, but in just a little more than two decades that total has climbed by 459 percent.
The PBoC issues the Panda gold coin, which was first created in 1982. The Panda coin is now one of the top five bullion coins issued by a central bank. It is among the ranks of the American Eagle, Canadian Maple Leaf, South African Krugerrand and Australian Gold Nugget.
The PBoC was one of the top gold buyers out the world's central banks for 2024, purchasing another 44 MT of gold during the year. April 2024 marked the 18th consecutive month of gold buying for China's central bank, which paused its purchases afterward until picking them up again in November.
7. Switzerland
Gold Reserves: 1,039.94 metric tons
Holding the seventh largest central bank gold reserves is the Swiss National Bank. Its 1,039.94 MT of gold are owned by the state of Switzerland, but the central bank manages and maintains the reserve.
After years of opaqueness regarding the country’s golden treasure trove, the Swiss Gold Initiative, or Save our Swiss Gold campaign, was launched in 2011.
The publicity culminated in a national referendum in 2014, asking citizens to vote on three proposals. The first was a mandate for all reserve gold to be held physically in Switzerland. The other two dealt with the central bank’s ability to sell its gold reserves, along with a decree that 20 percent of the Swiss bank’s assets be held in gold.
The referendum was unsuccessful, but did prompt the bank to be more transparent. In a 2013 release, the central bank reported that 70 percent of its gold reserve was held domestically, 20 percent was located at the Bank of England and 10 percent was stored with the Bank of Canada.
8. India
Gold Reserves: 876.18 metric tons
The Reserve Bank of India is another central bank that has fervently acted to increase its holdings in recent years. It began adding to its gold assets in 2017; however, the majority of its purchases have taken place in the past four years.
Strikingly, after India's central bank purchased 16 MT of gold in 2023, the institution scooped up another 72 MT of the precious metal in 2024.
While more than half of its gold is held overseas in safe custody with the Bank of England and the Bank of International Settlements, about a third of its gold is held domestically. In June 2024, India repatriated 100 MT of gold from the United Kingdom. This was the first time since 1991 that the Reserve Bank of India moved its overseas gold holdings back home.
9. Japan
Gold Reserves: 845.97 metric tons
Public information about the Bank of Japan’s gold reserves is hard to come by. In 2000, the island nation was holding approximately 753 MT of the yellow metal. By 2004, the Bank of Japan’s gold store had grown to 765.2 MT, and remained at that level until March 2021, when the country purchased 80.76 MT of gold.
10. Netherlands
Gold Reserves: 612.45 metric tons
Rounding out this list of the top central bank gold reserves is the Dutch National Bank (DNB), the central bank of the Netherlands. Like Switzerland, the Dutch central bank stores as much as 38 percent of its gold in Canada’s national reserve. Another 31 percent, in the form of 15,000 gold bars, is held in a domestic vault, while the remaining 31 percent is located in New York’s Federal Reserve bank.
In a report, the DNB describes gold as the supreme safe-haven asset. “Central banks such as DNB have therefore traditionally had a lot of gold in stock. After all, gold is the ultimate nest egg: the trust anchor for the financial system,” it reads. “If the entire system collapses, the gold supply provides collateral to start over. Gold gives confidence in the strength of the central bank’s balance sheet. That gives a safe feeling.”
*11. International Monetary Fund
Gold Reserves: 2,814.1 metric tons
The gold reserve held by the International Monetary Fund is the third largest in terms of size. The large gold reserve was amassed primarily during the founding of the international organization in 1944.
In that inaugural year, it was decided that “25 percent of initial quota subscriptions and subsequent quota increases were to be paid in gold.”
Since 1944, the International Monetary Fund has added gold through the repayment of debts owed by member countries. Nations can also exchange gold for another member country’s currency.
This is an updated version of an article first published by the Investing News Network in 2020.
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Securities Disclosure: I, Melissa Pistilli, hold no direct investment interest in any company mentioned in this article.
1911 Gold
Investor Insight
1911 Gold Corporation offers a unique opportunity for investors seeking exposure to high-grade gold assets with near-term production potential, a fully permitted infrastructure, and significant exploration upside in a world-class mining jurisdiction.
Overview
1911 Gold Corporation (TSXV:AUMB,OTCQX:AUMBF) is a junior mining company focused on the exploration and development of gold resources in Manitoba, Canada. The company holds a dominant, 62,000 hectare land position in the Rice Lake greenstone belt in Manitoba, an underexplored western extension of the prolific Red Lake gold district.
The company’s strategy is focused on de-risking the existing underground mine geology, expanding its mineral resource base through exploration, and advancing towards production on an accelerated time line by leveraging the existing infrastructure in place.
Gold continues to be a preferred safe-haven asset, with strong demand driven by economic uncertainty, inflationary pressures, and global geopolitical tensions. The price of gold has shown resilience, and many analysts project continued strength in the market. 1911 Gold is well-positioned to capitalize on this favorable environment through its fully permitted infrastructure, extensive land package, existing 43-101 resources, and near-term production potential. By advancing its True North project and regional exploration portfolio, the company is strategically placed to benefit from rising gold prices while minimizing jurisdictional risks.
1911 Gold’s leadership team comprises experienced mining executives, geologists and financial professionals with extensive backgrounds in advanced exploration, mine development, corporate finance and strategic planning. Their combined expertise provides the company with the ability to navigate complex operational and financial landscapes, positioning 1911 Gold as a serious contender in the junior mining sector.
Company Highlights
- 1911 Gold Corporation is a junior gold exploration company and near-term producer with more than 1.1 million ounces of gold resource in an established mining district.
- The company’s assets include a permitted 1,300-ton-per-day mill and tailings facility, and underground mine, reducing time and costs to production
- With a large land package in the Rice Lake belt, 1911 Gold boasts multiple high-potential targets, providing significant resource expansion potential.
- The company is led by a seasoned management team and board with a strong track record of advancing mining projects.
- The company operates in a mining-friendly jurisdiction with hydroelectric power and excellent infrastructure.
Key Projects
True North Project
The True North project is 1911 Gold's flagship asset, located in the Rice Lake greenstone belt of southeastern Manitoba, approximately 150 km northeast of Winnipeg. This historically significant mine has produced over 2 million ounces (Moz) of gold and continues to offer substantial exploration upside.
The current mineral resource estimate for True North includes:
- Indicated Resources: 3.52 million tonnes (Mt) at 4.41 grams per ton (g/t) gold, containing 499,000 ounces.
- Inferred Resources: 5.49 Mt at 3.65 g/t gold, containing 644,000 ounces.
These resources remain open for expansion, with multiple high-priority exploration targets identified near existing underground workings.
Geology and Mineralization
The True North deposit is characterized by high-grade, structurally controlled gold mineralization hosted within the Archean Rice Lake greenstone belt. Gold occurs within quartz-carbonate vein systems associated with major regional structures and secondary shear zones. The mineralization extends to significant depths, providing long-term exploration potential.
History
Gold was first discovered at True North in 1911, leading to decades of intermittent mining under various operators. The mine has undergone multiple phases of development, with extensive underground infrastructure, including a shaft extending to a depth of over 1,200 meters. Previous owners, including San Gold Corporation and Klondex Mines, operated the mine until 2017, after which it was acquired by 1911 Gold in mid-2018.
Infrastructure and Geographic Advantages
- A fully permitted 1,300-ton-per-day (tpd) mill, which can be expanded to 2,250 tpd
- A permitted tailings management facility, reducing environmental and permitting risks
- Year-round road access throughout the property with proximity to hydroelectric power
- A 200-person camp and operational support facilities for efficient workforce deployment
Exploration and Development Plans
1911 Gold is focused on expanding the True North resource through an aggressive exploration program. Key initiatives include:
- Drill testing high-priority targets, including San Antonio West and Southeast targets, which have shown strong mineralization potential
- Resource expansion through underground drilling, targeting underexplored areas within the mine lease
- Development of new high-grade zones to support near-term production and long-term operational sustainability
- Geophysical surveys and geochemical sampling to identify additional gold-bearing structures within the broader property
The company will leverage True North’s existing infrastructure to restart mining operations efficiently while continuing to explore the vast untapped potential of the surrounding district.
Regional Exploration Projects
In addition to the True North mine, 1911 Gold controls a large-scale land package within the Rice Lake greenstone belt. The company has identified multiple high-potential targets within this district, including:
- Ogama-Rockland: A past-producing high-grade deposit with significant exploration upside
- Central Manitoba: An area with historical production featuring multiple high-grade vein structures with strong exploration potential
- Gunnar: A historic mine representing an additional potential source of mill feed.
The company aims to leverage its central milling facility as part of a "hub-and-spoke" development model, bringing additional satellite deposits into production.
Management Team
Shaun Heinrichs - President & CEO
With over 20 years of experience in corporate finance, strategic planning, and capital markets, Shaun Heinrichs has held key leadership roles in the mining sector. Before joining 1911 Gold, he served as CFO on various companies, including Group Eleven Resources and Veris Gold, which owned the Jerritt Canyon operation, where he played a pivotal role in corporate development and mergers and acquisitions.
Carmen Amezquita - Chief Financial Officer
A finance professional with over a decade of experience in the resource sector, Carmen has extensive expertise in financial reporting, capital management, and corporate governance for both exploration-stage and producing mining companies.
Michele Della Libera - Vice-president, Exploration
A geologist with over 30 years of experience in mineral exploration, Michele has worked extensively on gold and base metal projects across Canada and internationally and has been closely involved in the development of several mines through to production. He oversees 1911 Gold’s exploration programs, with a focus on expanding the company’s resource base and identifying new discoveries.
Gary O’Connor - Executive Chair
A veteran mining executive with decades of experience in project development and exploration, Gary has held leadership positions at major mining companies, guiding strategic growth initiatives.
Mike Hoffman - Director
A professional engineer with extensive experience in mine development, operations, and corporate strategy. He has played key roles in advancing multiple mining projects from early-stage exploration to production.
Blair Schultz - Director
A finance and investment specialist with a background in institutional asset management and corporate governance. Blair has been instrumental in providing financial oversight and strategic direction for mining companies.
Anna Ladd-Kruger - Director
A highly regarded financial executive in the mining industry, Anna has held senior leadership roles in several resource companies, focusing on financial strategy and corporate growth.
Éric Vinet - Advisor
An expert in mining operations and project development, Éric provides strategic insights on optimizing production, cost management, and operational efficiencies.
Halcones Precious Metals Announces Additional Outcrop Chip Channel Sample Results Extending Mineralized Footprint to the South at Polaris Gold Project, Antofagasta Region Chile
Halcones Precious Metals Corp. (TSX – V: HPM) (the “Company” or “Halcones”) is pleased to announce additional results from the recent field program at the Polaris gold project, Chile (“Polaris” or the “Project”). Polaris is a large, highly prospective gold project that has never been drilled. No modern exploration has been carried out to date other than basic rock sampling and mapping. Surface bedrock sampling performed by Halcones’ geologists has extended the strike length of a trend of assay results, comprising more than 400 rock samples, many grading greater than 1g/t gold, to 3.9 km. This trend remains open for another 2km to the north and 1.5 km to the south before reaching property boundaries.
According to Ian Parkinson, CEO of Halcones, “It is exceedingly rare to see such an extensive and highly mineralized gold trend that has never been drilled. In more than ten years as a senior mining analyst for leading financial institutions, there is not a single project I have seen that shows such extensive mineralization in outcrops and no history of systematic exploration. We are very excited by the prospectivity of this project”.
Halcones’ geologists recent field work was focused on mapping and sampling a priority area within the North Zone (Figure 1) resulting in an expanded priority target. This area has consistently returned high grade results from surface sampling. Several highly prospective drill targets have been outlined through this sampling program in the North Zone (see Figure 2). Sampling completed by the Company has increased the gold mineralized footprint by approximately 210% from the area first observed by the optionors of the Project. Company geologists believe that the North and South Zones may merge into a single large gold anomaly, further increasing the potential of the Project. Sampling is limited in the area between the North and South Zone due to the presence of thin overburden cover. The next phase of exploration will focus on better defining the extension of the anomalous gold in this area to confirm the current geological interpretation of the field team. Additional sampling to explore and expand the anomaly to the north and east will also be done as part of the next stage of exploration.
Highlights:
- Select highlights from the last batch of 44 assays include 29.04, 10.67, and 3.54 g/t Au, hosted primarily in stockwork (see Figures 3 & 4). These results are in addition to the 20.05, 13.08, 8.54 and 6.67 g/t Au previously reported (see February 4th,2025 press release for details). The samples consisted of continuous 1m long chip samples to ensure representative sampling. The program prioritized sampling of stockwork as opposed to larger quartz veins. Gold bearing stockwork (see Figures 3 & 4) at surface has been sampled over approximately a 250m X 500m area and the limits of this mineralized zone are unknown. Several high-grade target areas have been identified. However, the entire area may represent a large, bulk minable target if continuity between bedrock samples is established. See Figure 2 for locations of samples.
- The North Zone sample area with the greatest concentration of high-grade surface samples has been expanded to the South. Sampling by Halcones’ geologists returned values consistent with work done by the optionors of the Project and extended the known area of high-grade mineralization to more than double that previously outlined. The approximate surface area of this target containing multiple surface samples above 1 g/t is 12.3 hectares.
- High grade mineralization continues to exhibit a strong structural control. In the reported sampling area (Figure 2), high grade samples continue to occur on the southwest side of a structural break. Approximately 40% of the surface area in the northwest portion of the Project area has a thin layer of colluvial cover and this has seen limited sampling. The Company plans to expand its sampling through this thin cover when approvals are in place.
- Halcones believes there is potential for a larger tonnage surface deposit of vein and stockwork hosted mineralization within the highly fractured granodioritic rocks adjacent to fault splays associated with the continental scale, Atacama Fault System in the area. Extensive gold mineralization has been identified by surface bedrock sampling over 3.9 km of strike length along these structures on the property to date.
Ian Parkinson, CEO and Director of Halcones:
“We are very excited by the results of our first field program at Polaris. These results have confirmed what we had hoped for at Polaris. In a few weeks of field work we have materially expanded the initial areas of interest and several very clear targets for future drilling have emerged. It is rare to see such broad anomalous gold at surface. Much of the Project area remains sparsely sampled and mapped. Our technical team is currently making plans to get back into the field”.
About The Recent Field Program:
The were two main objectives of the field program.
1) Expand the footprint of the known mineralization in the Northwest corner of the North Zone (See Figure 1).
2) Test and better define the extent of mineralized stockwork as a lower grade bulk tonnage opportunity adjacent to the known vein hosted mineralization.
This first field program has successfully expanded the surface area of mineralization (see Figure 2) and confirmed the presence of extensive stockwork hosted gold mineralization at surface.
Sampling previously performed on Polaris identified the northwest section of the North Zone as a priority area (see Figure 1). In recent field work, Halcones’ geologists increased the density of sampling and expanded the surface footprint of sampling in this priority area (see Figure 2). Halcones’ geologists took a total of 140 samples during the recent field campaign. All assays from this program have been received, of which 31 returned values above 1 g/t Au.
This sampling program has successfully expanded the surface expression of the work completed previously on Polaris. Additionally, stockwork mineralization has been confirmed over a broader area. The presence of mineralized stockwork over an extensive area supports Halcones’ geologist interpretation that bulk tonnage deposit potential exists at Polaris. Sampling has been limited in certain areas due to the presence of a thin layer of colluvial cover. Sampling programs are being planned to test bedrock below this this cover.
Halcones’ geologists have been working with a geological model that Polaris holds potential for a large-scale bulk tonnage open pit operation. The presence of mineralization in stockworks in the wall rocks away from the historically mined, mineralized veins is a crucial component of this model that is present at Polaris. This stockwork is believed to have a similar genesis to the vein hosted mineralization previously exploited by artisanal miners but was never targeted. The stockwork mineralization is not visually obvious due to a general lack of associated sulfide minerals. The 17 known small scale mines in the Project area exploited very high-grade veins with no focus on the stockwork adjacent to the veins.
Figure 1: Polaris Project sampling has identified gold mineralization over a 3.9 km extent in an area that has never been drilled.
Figure 2: Polaris North Zone field program results with recent assays represented.
The stars are Halcones’ samples, the dots are samples by the optionors.
Figure 3: Example of typical mineralized stockwork in outcrop. The rock is highly transected by randomly oriented hairline fractures that commonly contain sub-millimetre to several millimetre quartz veins that are thought to contain the gold. The host is typically tonalite to granodiorite, which has been fractured adjacent to the fault systems in the area. Visually, there are few indications of mineralization.
Figure 4: Example of stockwork mineralization exhibiting larger quartz veinlets. The mineralized rock is characterized by multiple veinlets and fractures at various orientations.
About The Sampling Process
Using a hammer and a rock chisel, a chip sample is carried out uniformly over at least 1 meter sections, ensuring complete collection and homogeneity in order to achieve proper representation of the sample. The sample is collected perpendicular to the dominant strike of the structures and the sample mass must be a minimum of 2 kg. In the event that the outcrop presents some mineralized structure, an independent sample will be taken only from the mineralized structure and an independent sample from the host rock on both sides of the structure. This process is designed to limit bias due to high grading sample collection.
All samples were bagged and sealed on site and delivered directly by the Project Geologist to ANDES ANALITYCAL ASSAY Laboratory in Copiapó, Chile. After sample preparation at ANDES ANALITYCAL ASSAY Laboratory in Copiapó, split pulp samples were shipped to ANDES ANALITYCAL ASSAY in Santiago, Chile for assaying gold by fire assay (AEF_AAS_1E42-FF), and for analyzing 34 other elements, including silver, by four acids (ICP_AES_AR34m1).
ANDES ANALITYCAL ASSAY is an independent laboratory certified with a global quality management system that meets all requirements of International Standards ISO/IEC 17025:2017, includes its own internal quality control samples comprising certified reference materials, blanks, and pulp duplicates.
Qualified Person
The scientific and technical information in this news release has been reviewed and approved by Mr. David Gower, P.Geo., as defined by National Instrument 43-101 of the Canadian Securities Administrators.
About Halcones Precious Metals Corp.
Halcones is focused on exploring for and developing gold-silver projects in Chile. The Company has a team with a strong background of exploration success in the region.
For further information, please contact:
Vincent Chen, CPA
Investor Relations
vincent.chen@halconespm.com
www.halconespreciousmetals.com
Cautionary Note Regarding Forward-looking Information
This press release contains “forward-looking information” within the meaning of applicable Canadian securities legislation. Forward-looking information includes, without limitation, regarding the prospectivity of the Project, the mineralization of the Project, the Company’s exploration program, the Company’s ability to explore and develop the Project and the Company’s future plans. Generally, forward-looking information can be identified by the use of forward-looking terminology such as “plans”, “expects” or “does not expect”, “is expected”, “budget”, “scheduled”, “estimates”, “forecasts”, “intends”, “anticipates” or “does not anticipate”, or “believes”, or variations of such words and phrases or state that certain actions, events or results “may”, “could”, “would”, “might” or “will be taken”, “occur” or “be achieved”. Forward- looking information is subject to known and unknown risks, uncertainties and other factors that may cause the actual results, level of activity, performance or achievements of Halcones, as the case may be, to be materially different from those expressed or implied by such forward-looking information, including but not limited to: general business, economic, competitive, geopolitical and social uncertainties; the actual results of current exploration activities; risks associated with operation in foreign jurisdictions; ability to successfully integrate the purchased properties; foreign operations risks; and other risks inherent in the mining industry. Although Halcones has attempted to identify important factors that could cause actual results to differ materially from those contained in forward-looking information, there may be other factors that cause results not to be as anticipated, estimated or intended. There can be no assurance that such information will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements. Accordingly, readers should not place undue reliance on forward-looking information. Halcones does not undertake to update any forward-looking information, except in accordance with applicable securities laws.
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