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Energy Junior Mining Lion One Metals Precious Metals

Lion One Announces $7.5M Brokered Private Placement

Lion One Metals Ltd.
Lion One Metals Ltd.

NORTH VANCOUVER, British Columbia, July 18, 2024 (GLOBE NEWSWIRE) — Lion One Metals Limited (TSX-V: LIO) (OTCQX: LOMLF) (ASX: LLO) (“Lion One” or the “Company”) is pleased to announce that it has entered into an agreement with Eight Capital as lead agent (the “Agent”) and sole bookrunner in connection with a “best efforts” private placement of up to 20,271,000 units of the Company (the “Units”) at a price of $0.37 per Unit (the “Issue Price”) for aggregate gross proceeds of up to $7,500,270, pursuant to the listed issuer financing exemption available under National Instrument 45-106 – Prospectus Exemptions (the “Offering”), in each of the Provinces of Canada other than Quebec. Each Unit will consist of one common share of the Company (a “Share”) and one common share purchase warrant (a “Warrant”). Each Warrant will entitle the holder thereof to acquire one Share at an exercise price of $0.50 for a period of three years from the date of issuance.

The Company will make available an offering document relating to the Offering (the “Offering Document”) which will be accessible under the Company’s profile at www.sedarplus.ca and at https://liononemetals.com. Prospective investors in the Offering should read the Offering Document before making an investment decision.

The Offering is expected to close on or around July 26, 2024 (the “Closing Date”). Closing of the Offering is subject to certain customary conditions including receipt of all necessary approvals including satisfaction of listing conditions of the TSX Venture Exchange. The Company has granted the Agent an option to offer for sale up to an additional 15% of the Units, at the Issue Price, exercisable in whole or in part at any time for a period of up to 48 hours prior to the Closing Date. The Units issued pursuant to the Offering will not be subject to any hold periods pursuant to applicable Canadian securities laws.

The Company intends to use the net proceeds from the Offering for working capital and general corporate purposes.

This news release does not constitute an offer to sell or a solicitation of an offer to sell any Shares in the United States. The securities to be sold in the Offering have not been and will not be registered under the U.S. Securities Act or any state securities laws and may not be offered or sold within the United States or to U.S. Persons unless registered under the U.S. Securities Act and applicable state securities laws or an exemption from such registration is available.

About Lion One Metals Limited

Lion One Metals is an emerging Canadian gold producer headquartered in North Vancouver BC, with new operations established in late 2023 at its 100% owned Tuvatu Alkaline Gold Project in Fiji. The Tuvatu project comprises the high-grade Tuvatu Alkaline Gold Deposit, the Underground Gold Mine, the Pilot Plant, and the Assay Lab. The Company also has an extensive exploration license covering the entire Navilawa Caldera, which is host to multiple mineralized zones and highly prospective exploration targets.

On behalf of the Board of Directors of
Lion One Metals Limited
Walter Berukoff
Chairman and CEO

For further information
Contact Investor Relations
Toll Free (North America) Tel: 1-855-805-1250
Email: info@liononemetals.com
Website: www.liononemetals.com

Neither 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.

Forward-Looking Information

This news release contains forward‐looking statements and forward‐looking information within the meaning of applicable securities laws. All statements other than statements of historical fact may be forward‐looking statements or information. Forward-looking statements are frequently identified by such words as “may”, “will”, “plan”, “expect”, “anticipate”, “estimate”, “intend” and similar words referring to future events and results. The forward‐looking statements and information are based on certain key expectations and assumptions made by management of the Company. Forward-looking statements made in this news release include statements regarding anticipated completion of the Offering and debt settlement, and the proposed use of proceeds of the Offering. Although management of the Company believes that the expectations and assumptions on which such forward-looking statements and information are based are reasonable, undue reliance should not be placed on the forward‐looking statements and information since no assurance can be given that they will prove to be correct.

Forward-looking statements and information are provided for the purpose of providing information about the current expectations and plans of management of the Company relating to the future. Readers are cautioned that reliance on such statements and information may not be appropriate for other purposes, such as making investment decisions. Actual results could differ materially from those currently anticipated due to a number of factors and risks, including, with respect to the Offering and debt settlement, the conditions of the financial markets, availability of financing, timeliness of completion of the Offering, and the timing of TSX Venture Exchange approval; and with respect to the use of proceeds, the sufficiency of the proceeds, the speculative nature of mineral exploration and development, fluctuating commodity prices, and competitive, as described in more detail in our recent securities filings available at www.sedarplus.ca, including the Offering Document. Accordingly, readers should not place undue reliance on the forward‐looking statements and information contained in this news release. Readers are cautioned that the foregoing list of factors is not exhaustive. The forward‐looking statements and information contained in this news release are made as of the date hereof and no undertaking is given to update publicly or revise any forward‐looking statements or information, whether as a result of new information, future events or otherwise, unless so required by applicable securities laws. The forward-looking statements or information contained in this news release are expressly qualified by this cautionary statement.

Categories
Base Metals Energy Junior Mining Metallic Group Precious Metals Stillwater Critical Minerals

Stillwater Critical Minerals Launches Field Programs Including Property-Wide Geophysical Survey at its Stillwater West Project in Montana, USA

VANCOUVER, BC / ACCESSWIRE / July 18, 2024 / Stillwater Critical Minerals Corp. (TSXV:PGE)(OTCQB:PGEZF)(FSE:J0G) (the “Company” or “Stillwater”) announces it has commenced 2024 field activities including a property-wide airborne electro-magnetic geophysical survey at its flagship Stillwater West Ni-PGE-Cu-Co + Au project in Montana.

The Company has engaged Expert Geophysics Ltd. for a combined time-domain electromagnetic (“EM”) survey using their TargetEM26 system along with a magneto-telluric survey using their MobileMTm system. The survey will utilize the newest technological advancements in airborne EM, building on the success of the first generation DIGHEM airborne EM survey flown over the project in 2000. The total survey will cover approximately 1,069 line-kilometers and provide higher-resolution and improved depth of investigation from the DIGHEM airborne EM survey, as well as VLF coverage. The survey has been designed in collaboration with Glencore plc via the Stillwater West technical committee to fine-tune priority conductive drill targets across the 12-kilometer main resource area, as well as to assist with prioritization and ranking of additional untested conductive targets across the broader 61-square-kilometer property.

Stillwater’s President and CEO, Michael Rowley, said “We are very pleased to kick off our field activities for the season at Stillwater West. This large-scale geophysical survey is part of a larger program that is expected to include an updated mineral resource estimate that will support the commencement of various studies relating to potential production scenarios. These objectives will be important milestones in preparation for continued resource expansion drilling across the nine-kilometer deposit area as well as in developing target areas. In addition, the Company is pursuing a number of other studies and initiatives with strategic partners such as Cornell University and various US Government agencies.”

Vice-President of Exploration, Dr. Danie Grobler, said, “Work has been on-going at our core facility as we ramp up for the year. The technical committee, including Glencore, continues to be focused on the expansion potential of the lower Stillwater Igneous Complex. Detailed geological and structural interpretive work during the past two years added significantly to our understanding of the large Platreef-style mineralized system discovered within the footwall contact zone of the Stillwater Complex. Our geological models now display strong geological control and continuity on mineralized zones. The planned airborne surveys will provide important high-resolution datasets to refine targeting of high-grade nickel-copper-PGE sulphide-hosted mineralization within the multi-kilometer-scale geophysical anomalies that we see across the 32-kilometer-long mineralized system.”

Upcoming Events

Stillwater is pleased to announce that President and CEO Michael Rowley will be presenting at the following events:

  1. Precious Metals Summit, Beaver Creek, Colorado, September 10-13, 2024. For information and registration please click here.
  2. Precious Metals Summit, Zurich, Switzerland, November 11-12, 2024. For information and registration please click here.

About Stillwater Critical Minerals Corp.

Stillwater Critical Minerals (TSXV:PGE)(OTCQB:PGEZF)(FSE:J0G) is a mineral exploration company focused on its flagship Stillwater West Ni-PGE-Cu-Co + Au project in the iconic and famously productive Stillwater mining district in Montana, USA. With the addition of two renowned Bushveld and Platreef geologists to the team and strategic investments by Glencore plc, the Company is well positioned to advance the next phase of large-scale critical mineral supply from this world-class American district, building on past production of nickel, copper, and chromium, and the on-going production of platinum group, nickel, and other metals by neighboring Sibanye-Stillwater. An expanded NI 43-101 mineral resource estimate, released January 2023, positions Stillwater West with the largest nickel resource in an active US mining district as part of a compelling suite of nine minerals now listed as critical in the USA. To date, five Platreef-style nickel and copper sulphide deposits host a total of 1.6 billion pounds of nickel, copper and cobalt, and 3.8 million ounces of palladium, platinum, rhodium, and gold at Stillwater West. All of these deposits remain open for expansion along trend and at depth.

Stillwater also holds the high-grade Black Lake-Drayton Gold project adjacent to Nexgold Mining’s development-stage Goliath Gold Complex in northwest Ontario, currently under an earn-in agreement with Heritage Mining, and the Kluane PGE-Ni-Cu-Co critical minerals project on trend with Nickel Creek Platinum‘s Wellgreen deposit in Canada‘s Yukon Territory.

FOR FURTHER INFORMATION, PLEASE CONTACT:
Michael Rowley, President, CEO & Director – Stillwater Critical Minerals
Email: info@criticalminerals.com Phone: (604) 357 4790
Web: http://criticalminerals.com Toll Free: (888) 432 0075

Quality Control and Quality Assurance

Mr. Mike Ostenson, P.Geo., is the qualified person for the purposes of National Instrument 43-101, and he has reviewed and approved the technical disclosure contained in this news release.

Forward-Looking Statements

This news release includes certain statements that may be deemed “forward-looking statements”. All statements in this release, other than statements of historical facts including, without limitation, statements regarding potential mineralization, historic production, estimation of mineral resources, the realization of mineral resource estimates, interpretation of prior exploration and potential exploration results, the timing and success of exploration activities generally, the timing and results of future resource estimates, permitting time lines, metal prices and currency exchange rates, availability of capital, government regulation of exploration operations, environmental risks, reclamation, title, and future plans and objectives of the company are forward-looking statements that involve various risks and uncertainties. Although Stillwater Critical Minerals believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results or developments may differ materially from those in the forward-looking statements. Forward-looking statements are based on a number of material factors and assumptions. Factors that could cause actual results to differ materially from those in forward-looking statements include failure to obtain necessary approvals, unsuccessful exploration results, changes in project parameters as plans continue to be refined, results of future resource estimates, future metal prices, availability of capital and financing on acceptable terms, general economic, market or business conditions, risks associated with regulatory changes, defects in title, availability of personnel, materials and equipment on a timely basis, accidents or equipment breakdowns, uninsured risks, delays in receiving government approvals, unanticipated environmental impacts on operations and costs to remedy same, and other exploration or other risks detailed herein and from time to time in the filings made by the companies with securities regulators. Readers are cautioned that mineral resources that are not mineral reserves do not have demonstrated economic viability. Mineral exploration and development of mines is an inherently risky business. Accordingly, the actual events may differ materially from those projected in the forward-looking statements. For more information on Stillwater Critical Minerals and the risks and challenges of their businesses, investors should review their annual filings that are available at www.sedar.com.

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.

SOURCE: Stillwater Critical Minerals Corp.

Categories
Base Metals Energy Junior Mining

Copper: Humanity’s first and most important future metal

As the third most-consumed metal behind iron ore and aluminum, copper is all around us. Found naturally in the Earth’s crust, copper was the first metal used by humans, dating back to the 8th century BC. 

Three thousand years later, homo sapiens figured out how to smelt copper from its ore, and to alloy it with tin to create bronze. Bronze was useful for tools and weapons, making it one of the most important inventions in the history of civilization.

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The Copper Age

Nothing happens without copper; as it turns out, not even civilization itself. Beginning around 5,000 BC, the “Chalcolithic”  (from the Greek “khalkos” for copper and “lithos” for stone) or Copper Age was a transitionary period between the Stone Age and the Bronze Age.

It was during this time that copper was introduced as a material that could be worked into metal, paving the way towards the use of bronze later on.

The archeological site of Belovode in present-day Serbia holds the distinction as the world’s oldest copper-smelting location, circa 5,000 BC. Copper was also found in the Near East beginning in the late 5th millennium BC. Later, pockets of copper technology began appearing in northern Italy and along the Mediterranean coast.

Copper was used to shape tools, weaponry, coins and jewelry.

The arrival of metal catapulted early Britain and other societies, including China, which has a long history of using metal objects, into a whole new chapter of civilization.

Copper minerals

According to the Commonwealth Scientific and Industrial Research Organisation (CSIRO), an Australian government agency, there are around 160 naturally occurring copper-bearing minerals. Chalcopyrite, bornite, chalcocite, and native copper (an uncombined form of copper) are four minerals often mined for their copper content.

Chalcopyrite is the most abundant copper-rich mineral.

Azurite is a copper carbonate mineral that forms in the upper oxidized zones of copper ore deposits. It has a deep azure-blue color. When exposed to air and water, it often shows a rainbow-like iridescence. Since ancient times, it has been used as an ore of copper, a gemstone, and a pigment. Michelangelo and Leonardo DaVinci even used it to create blue hues in their paintings. 

Malachite was one of the first ores used to produce copper metal. Often found with azurite, malachite is a mixture of copper, iron and oxygen. It has a deep green color that does not fade over time or when exposed to light. This made malachite a popular pigment for painting. Ancient Egyptians used it for tomb paintings. European painters, especially in the 15th and 16th centuries, loved the palette of greens it gave. Artists in India, Tibet, China, and Japan used it in murals, manuscripts, ceramics and lacquerware. 

‘Conducting change: Why copper is key to a renewable future’ by CSIRO, Oct. 27, 2023.

Uses

Sometimes referred to as “Dr. Copper” for its ability to diagnose the health of the global economy, copper is just as essential to modern society as to ancient civilizations — if not more so.

The Copper Development Association divides its uses into four categories: electrical, construction, transport and other. By far the largest sector for copper usage is electrical, at 65%, followed by construction at 25%.

Source: Natural Resources Canada

Copper is useful for electrical applications because it is an excellent conductor of electricity. The only metal that has higher conductivity is silver, but silver is expensive by comparison. 

Conductivity, combined with durability, malleability and dependability, make it ideal for wiring. Sprott notes that copper’s journey took a historic turn in the 1800s when its exceptional electrical conductivity sparked the revolutionary age of telegraphy and incandescent electric lamps to light homes.

Among electrical devices that use copper, are computers, televisions, circuit boards, semiconductors, microwaves, and fire prevention sprinkler systems.

In telecommunications, copper is used in wiring for local area networks (LAN), modems and routers. The construction industry would not exist without copper; it is essential for wiring in residential and commercial construction. The red metal is also used for potable water and heating systems due to its ability to resist the growth of water-borne organisms, as well as its resistance to heat corrosion.

The transportation industry is reliant on copper for core components of airplanes, trains, cars, trucks and boats. A commercial airliner has up to 190 kilometers of copper wiring, while high-speed trains use up to 10 tonnes of copper per kilometer of track.

Automobiles have used copper and brass radiators and oil coolers since the 1970s. More recent applications include on-board navigation, anti-lock braking systems, heated seats, defrosting wires embedded in windows, hydraulic lines, and wiring for window and mirror controls.

Copper is a critical mineral for our infrastructure, including over 11 million km of electrical wires powering homes, businesses and industry in the United States alone. 

The average home contains more than 90 kg of copper.  

In 2022, the copper market was worth USD$183 billion, making it the third most valuable metals market behind only iron ore and gold.

Copper and electrification

Copper is the heartbeat of the global energy economy.

Millions of feet of copper wiring will be required for strengthening the world’s power grids, and hundreds of thousands of tonnes more are needed to build wind and solar farms. Electric vehicles use triple the amount of copper as gasoline-powered cars. Renewable energies need five times more copper than non-renewables.

According to Bloomberg New Energy Finance (NEF), clean energy currently consumes a quarter of copper demand, a figure that is projected to reach 61% by 2040, given our growing reliance on wind, solar and electric vehicles. (‘Copper: Wired for the Future’ by Sprott, Feb. 27, 2024)

Copper has been designated a critical mineral by several developed countries/ regions including Canada, the US, the European Union, China, Japan and India. Last year at the United Nations’ COP28 climate summit, 118 governments pledged to triple global renewable energy capacity by 2030.

Copper’s role as a critical mineral led to its inclusion in over $30 billion of funding from the Biden administration’s Inflation Reduction Act.

The Sprott report says that, while copper is likely to take center stage as the leading electrification metal, existing copper supplies are dwindling and new mines take up to two decades to develop, which is creating a race to meet increasing copper demand.

Global investment in the energy transition reached $1.8 trillion in 2023; it now exceeds investments in fossil fuels. To reach “net zero” emissions targets by 2050, investments must average $4.8 trillion from 2024 to 2030 (that’s almost $5T every year for the next six years!). In the 2030s, the average annual investment would need to approach $7T.

Sprott makes the following points about copper demanded by electrification and decarbonization:

  • By 2050, it’s projected that the global electric grid will need to double in capacity to meet the 86% increase in electricity demand.
  • Shifting production to greener energy sources is expected to necessitate 427 million tonnes of copper by 2050. Last year, the mining industry only produced 22Mt.
  • The shift toward underground wiring, which requires twice as much metal as overhead lines, is intensifying the demand for copper.
  • Copper is essential in EVs, finding use in electric motors, batteries, inverters, wiring and charging stations. An EV requires 53 kilograms of copper in electric motors, batteries, inverters, wiring and charging stations, about 2.4 times more than a conventional combustion vehicle uses. This volume of wire can extend up to a mile in length. Although efforts are underway to reduce copper in EVs, demand is still projected to hit 2.8 million tonnes by 2030.
  • Renewable energy infrastructure, including solar and wind power, needs 2.5 to 7 times more copper than fossil fuel-based technologies, depending on whether the wind installations are onshore or offshore.
The role of critical minerals in energy transition. Source: IEA, May 2021

A new study suggests that electrifying the global vehicle fleet by 2050 will require an unrealistic ramp-up in copper production.

Researchers at the University of Michigan and Cornell University found that copper can’t be mined fast enough to keep up with current US policy guidelines to make the transition from fossil-fueled power and transportation to electric vehicles and renewable energies.

For example the Inflation Reduction Act calls for 100% of new cars to be electric vehicles by 2035.

“We show in the paper that the amount of copper needed is essentially impossible for mining companies to produce,” said Adam Simon, co-author of the paper, published by the International Energy Forum (IEF).

How impossible? The researchers found between 2018 and 2050, the world will need to mine 115% more copper than has been mined in all human history to 2018. This would meet our current copper needs and support the developing world without considering the green energy transition.

To electrify the global vehicle fleet requires bringing into production 55% more new mines. Between 35 and 195 large new copper mines would have to be built by 2050, at a rate of up to six mines per year. In heavily regulated environments like the United States and Canada, it can take up to 20 years to build one mine from scratch.

The baseline (no green energy transition) scenario supposes a more realistic, but still challenging 35 new copper mines, or one per year from 2018.

Source: International Energy Forum
Source: International Energy Forum

Instead of fully electrifying the US fleet of vehicles, Simon suggests focusing on manufacturing hybrid vehicles, which require far less copper than electric vehicles — 29 kg vs 60 kg.

Going this route would not require major grid improvements and would have almost as large an impact on reducing CO2 emissions, the study found. Also, the likelihood of finding the copper needed to make hybrids is much greater than for electric vehicles.

A final takeaway from the report? There are enough copper resources on planet Earth; the concern is whether these resources can be mined fast enough to support baseline global development, then go beyond towards vehicle electrification and green energy.

The baseline scenario envisions about 1.69 billion tonnes of copper will be mined by 2050, which represents about a quarter (26%) of the total copper resource of 6.6 billion tonnes.

Going deeper underground would grow the resource to 89Bt, and 241BT may be recoverable from the sea floor.

New copper mines that came online between 2019 and 2022 took an average of 23 years to get from discovery to production, the study says.

Copper market

Demand

On the demand side, electrical grids need to be updated, and governments are embarking on large-scale infrastructure investments that are copper-intensive.

Along with the usual applications in construction wiring and plumbing, transportation, power transmission and communications, there is now added demand for copper in electric vehicles, solar panels, wind turbines, and energy storage.

Additional copper is being demanded by the electrification of public transportation systems, 5G and AI.

According to Nikkei Asia, prices are being buoyed by the need for more data centers to support the development of artificial intelligence, all of which will require copper.

The latest copper demand driver comes from the Ukraine, where the war with Russia is consuming tonnes of bullet cartridge casings made of brass, an alloy of copper and zinc.

The European Defense Agency says a NATO 155-mm artillery shell contains half a kilogram of copper, with Ukrainian forces firing up to 7,000 per day.

Supply

Copper may have come off the boil recently due to problems in China but the structural supply deficit is real and keeping prices elevated.

World reserves by country, 2022. Source: Natural Resources Canada

Benchmark Mineral Intelligence (BMI) forecasts global copper consumption to grow 3.5% to 28 million tonnes in 2024, and for demand to increase from 27 million tonnes in 2023 to 38 million tonnes in 2032, averaging 3.9% yearly growth.

Yet the US Geological Survey reports supply from copper mines in 2023 amounted to only 22 million tonnes. If the copper supply doesn’t grow this year, we are looking at a 6Mt deficit.

Mining companies are seeing their reserves dwindle as they run out of ore. Commodities investment firm Goehring & Rozencwajg says the industry is “approaching the lower limits of cut-off grades and brownfield expansions are no longer a viable solution. If this is correct, then we are rapidly approaching the point where reserves cannot be grown at all.”

Effectively, lower grades mean millions of tonnes more rock needs to be moved and processed to get the same amount of copper.

Last week, the vice president of US investment bank Stifel Financial Cole McGill presented data that corroborates Goehring & Rozencwajg, stating “If you look at grades at the top 20 copper mines since 2000, they’ve trended down about 15-20%, and if you take out some of the higher-grade African projects, that’s even lower.”

Sprott agrees that, Chile and Peru, the top copper-producing countries, are grappling with labor strikes and protests, compounded by declining ore grades. Russia, ranked seventh in copper production, faces an expected decline due to the ongoing war in Ukraine. Despite efforts by miners to ramp up production, many analysts anticipate a widening supply imbalance.

Major copper miners aren’t doing much to alleviate the problem. High-quality projects are increasingly rare and major new discoveries are lacking. The time from discovery to production averages 16.5 years.

To meet the increase in copper demand, copper majors are focused on extending the life spans and productivity of existing mines rather than carrying out more expensive, and risky, exploration and development of new (greenfield) projects.

E&MJ Engineering stated in its outlook for copper production to 2050, “The trend toward declining orebody grades and continued development of the pursuit of existing operations to exploit lower grade deposits is likely to continue, in the absence of high-grade project discovery.

A decline in ore grade results in higher operating costs due primarily to the amount and depth of material required to be mined and processed to produce the same amount of copper product. It is no surprise that both GHG emission intensity and energy intensity increase as ore grade decreases. There is a point of inflection, where below an ore grade of around 0.5% copper, the intensity of both metrics rises sharply.”

Given that many mines are fast approaching, if not already tackling, similar grades, this is a pressing problem. In its fiscal year 2020 commodity outlook, BHP, the world’s third largest copper producer, estimated that grade decline could remove about 2 million metric tons per year (mt/y) of refined copper supply by 2030, with resource depletion potentially removing an additional 1.5 million to 2.25 million mt/y by this date.”

Along with technical issues such as falling grades/ deteriorating ore quality, there is also supply pressure from growing resource nationalism.

According to Sprott, capital for the exploration and development of copper mines peaked at $26.13 billion in 2013. Since then, it has almost halved and remains low, with only $14.42 billion spent in 2022.

McGill told Bloomberg that between 2009 and 2016, copper supply grew at a CAGR of 3.5-4%. Since 2016, when copper priced bottomed at around $2-2.20/lb, the CAGR is around 1%.

Without new capital investments, Commodities Research Unit (CRU) predicts global copper mine production will drop to below 12Mt by 2034, leading to a supply shortfall of more than 15Mt. Over 200 copper mines are expected to run out of ore before 2035, with not enough new mines in the pipeline to take their place.

Last year, the government of Panama ordered First Quantum Minerals (TSX:FM) to shut down its Cobre Panama operation, removing nearly 350,000 tonnes from global supply.

A strike at another large copper mine, Las Bambas in Peru, temporarily halted shipments.

Copper specialist Anglo American says it is scaling back output by about 200,000 tons, owing to head grade declines and logistical issues at its Los Bronces mine. Los Bronces production is expected to fall by nearly a third from average historical levels next year as the miner pauses a processing plant for maintenance, Reuters said.

Chile’s copper output has been dented by a long-running drought in the country’s arid north. State miner Codelco’s 2023 production was the lowest in 25 years.

All four of Codelco’s megaprojects have been delayed by years, faced cost overruns totaling billions, and suffered accidents and operational problems while failing to deliver the promised boost in production, according to the company’s own projections.

There are also concerns about Zambia, Africa’s second largest copper producer, where drought conditions have lowered dam levels, creating a power crisis that threatens the country’s planned copper expansion.

Ivanhoe Mines (TSX:IVN) reported a 6.5% Q1 drop in production at the world’s newest major copper mine, Kamoa-Kakula in the DRC.

The Congo last year overtook Peru as the world’s second-largest copper producer, but supply is threatened by ongoing armed conflict.

According to Voice of America

At least 70 people, including nine soldiers and a soldier’s wife, were killed when armed men attacked a village in western Democratic Republic of Congo, local authorities said, as violence intensifies between two rival communities…

The army is also struggling to contain the violence in the eastern part of the country, which has been torn by decadelong fighting between government forces and more than 120 armed groups seeking a share of the region’s gold and other resources.

Violence in the eastern part of the country has worsened in recent months as security forces battle the militias. Earlier this month, a militia attack on a gold mine in northeastern Congo killed six Chinese miners and two Congolese soldiers.

The World Health Organization warns that millions of people in the DRC are facing a health and humanitarian crisis (VOA, July 13, 2024)

As the government collects billions in revenues from new mining operations, like Ivanhoe’s Kamoa-Kakula, we predict the fight over resource rents could lead to internal struggles over who controls the government. How long before Congolese copper, cobalt, diamonds and gold are labeled “blood minerals”?

The forecasted copper supply gap — more than 15Mt by 2034 — was front and center at the Rule Symposium in Florida earlier this month. Mining magnate and Ivanhoe Mines’ founder Robert Friedland said current copper prices “fall woefully short” of supporting the development of new projects.

“We see a crisis coming in physical markets and a requirement for much higher prices to enable most of the copper projects that are in development to have a prayer coming in,” Friedland said via The Northern Miner. . The incentive price to build new mines is $11,000/t.

Higher prices are needed to counteract soaring cost inflation in building new mines, even in cheaper jurisdictions like Chile and Peru.

Friedland produced a surprising statistic, that humanity must mine more copper in the next 20 years than we have in human history to meet surging global demand on the back of the energy transition.

He estimated the global economy needs to find five or six new Kamoa-Kakula-sized projects yearly to maintain a 3% gross domestic product growth rate over the next two decades.

Over the past 10 years, greenfield additions to copper reserves have slowed dramatically. S&P Global estimates that new discoveries averaged nearly 50Mt annually between 1990 and 2010. Since then, new discoveries have fallen by 80% to only 8Mt per year.

There are really only three ways for the industry to get this additional metal. First, they can increase production from existing mines; this often involves “going underground”, digging beneath the existing open pit to access more ore. An expansion to the existing concentrator or building a new one, is sometimes needed.

Second, they can expand their mines laterally, going after resources that weren’t part of the initial mine plan because they were less accessible, or un-economic.

Third, they can explore for new mineral deposits, either internally, or working with junior mining companies, which have the exploration expertise to bring a deposit forward to the point when it can be sold to a major.

Obviously option three, known as greenfield exploration, is more difficult, costly, and carries higher risk than options one and two, called brownfield exploration.

Prices

Crux Investor noted that copper prices have risen significantly, with majors like BHP acquiring copper assets through M&A rather than building new mines. Examples include BHP’s purchase of Oz Minerals and Newmont’s acquisition of Newcrest.

Despite the market’s recognition of copper’s role in the future economy and increasing supply tightness, Crux Investor says analysis shows copper prices still remain below their long-term inflation-adjusted average, suggesting room for further appreciation.

While BMO Capital Markets and Citigroup analysts believe current copper prices may rise past $4.54/lb due to a Chinese smelter supply shortage, and grid investments in China, they say a sustained price gain is needed by copper miners to make investment decisions.

Copper mining is an extremely capital-intensive business for two reasons.

First, mining has a large up-front layout of construction capital called capex – the costs associated with the development and construction of open-pit and underground mines. There is often other company-built infrastructure like roads, railways, bridges, power-generating stations and seaports to facilitate extraction and shipping of ore and concentrate. Second, there is a continuously rising opex, or operational expenditures. These are the day-to-day costs of operation: rubber tires, wages, fuel, camp costs for employees, etc.

The average capital intensity for a new copper mine in 2000 was between US$4,000-5,000 to build the capacity, the infrastructure, to produce a tonne of copper. In 2012 capital intensity was $10,000/t, on average, for new projects. Today, building a new copper mine can cost up to $44,000 per tonne of production.

Capex costs are escalating because:

Declining copper ore grades means a much larger relative scale of required mining and milling operations.

A growing proportion of mining projects are in remote areas of developing economies where there’s little to no existing infrastructure.

Many inputs necessary for mine-building are getting more expensive, as cross-the-board inflation, the highest in 40 years, infiltrates the industry. This includes two of the largest costs, wages and diesel fuel, used to run mining equipment.

The bottom line? It is becoming increasingly costly to bring new copper mines online and run them.

Investors are also demanding a higher return on investment than previously, when there was a greater appetite for risk.

Citigroup is bullish on copper, with the bank’s analysts predicting that prices could surpass $10,000 a tonne ($4.53/lb) this year due to policy support in China.

Mining.com reports Beijing is expected to introduce further stimulus to upgrade its renewable energy infrastructure at the Third Plenum meeting in mid-July:

These additional measures, specifically targeting domestic property and grid investments, are expected to support copper prices in the near term, Citi analysts said in a note.

Conclusion

Copper presents a compelling opportunity for investors. The Sprott report notes that copper prices and miners are likely to benefit from the growing supply-demand gap. It also says that copper’s strategic importance has driven significant M&A in 2023, with BHP and Rio Tinto acquiring copper producers at significant premiums. Automakers concerned about securing future supplies are investing directly in mining companies.

But copper miners buying other copper miners does nothing to alleviate the supply shortage. It only transfers one copper reserve to another. Majors have underinvested in copper exploration and development, preferring M&A to the expense and risk of finding new copper deposits. 

Junior copper explorers provide investors exposure to potential new discoveries that could help narrow the supply gap. These discoveries offer the chance for outsized returns, though obviously with higher risk.

Copper equities have underperformed the copper price, presenting a potential catch-up opportunity.

Extraordinary demand growth, set against a backdrop of constrained supply, is expected to deepen the structural deficit through the end of the decade. Higher copper prices will be needed to incentive new supply. (Crux Investor)

(By Richard Mills)

Ahead of the Herd newsletter, aheadoftheherd.com, hereafter known as AOTH.

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Categories
Base Metals Emx Royalty Energy Junior Mining Precious Metals Project Generators

| EMX Royalty Shareholders | Arizona Sonoran Updates Cactus Project Mineral Resource Estimate to 7.3 B lbs of Copper in M&I and 3.8 B lbs of Copper in Inferred – Updated Parks/Salyer Deposit Amenable as an Open Pit

Casa Grande, AZ and Toronto, ON, July 16, 2024 – Arizona Sonoran Copper Company Inc. (TSX:ASCU) (“ASCU” or the “Company”), releases its updated Mineral Resource Estimate (“MRE”) for the Cactus brownfield copper project, located 45 miles south of Phoenix, Arizona (see FIGURES 1-3). The updated and expanded MRE is inclusive of a seven-month drilling program targeting the MainSpring property, which was completed in April 2024. The Cactus Project is wholly owned and located on private land in Arizona with direct road and rail access, infrastructure onsite, is at an advanced permitting stage, and has permitted access to onsite water wells. Highlights and key changes from the updated MRE are listed below.

Highlights:

  • Updated total Cactus Project Mineral Resource Estimate (“MRE”) including Primary Mineral Resources:
    • Measured and Indicated (“M&I”) 632.6 million short tons @ 0.58% Total Copper (“CuT”) for 7.3 billion pounds (“lbs”) of copper
    • Inferred 474.0 million short tons @ 0.41% CuT for 3.8 billion lbs of copper
  • Key Changes:
    • Confirms Parks/Salyer and MainSpring as one deposit, renamed to “Parks/Salyer”
      • Parks/Salyer mineral resource contains 339.0 million short tons @ 0.71% CuT for 4.8 billion lbs of copper in the M&I category and 299.3 million short tons @ 0.43% CuT for 2.6 billion lbs of copper in the Inferred category
    • Parks/Salyer amenable as an open pit within the pending Preliminary Economic Assessment
      • New Parks/Salyer mineral resource dimensions are 6,400 feet (“ft”)(1,950 meters (“m”) by 3,000 ft (915 m) to a maximum depth of 2,350 ft (716 m) below surface
    • 1,904% increase to the Measured Category with inclusion of initial Measured mineral resources at Parks/Salyer, 26% increase to the total M&I and a 60% increase in total Inferred resource, with no change to cut-off grade criteria or underlying price and cost assumptions
      • 42% increase of M&I mineral resources at Parks/Salyer attributed to success of measured infill drilling program, reporting of open pit resources, and reporting based on total copper pounds
      • Parks/Salyer infill drilling (56,907 ft | 17,345 m) converted 55.9 M short tons @ 1.03% CuT for 1.2 billion lbs of copper reported to the measured category
      • 60% increase to the Inferred mineral resources attributed to expansion of Parks/Salyer mineral resource onto the MainSpring property and reporting based on total copper pounds
      • 7-month drilling program at MainSpring (49,193 ft | 14,994 m) delivered 244.9 M short tons @ 0.39% CuT for 1.9 Billion lbs of copper reported to the Inferred mineral resource

Table 1 below reports the July 11, 2024, Cactus Project MRE, containing the combined Parks/Salyer, Cactus West, Cactus East, and Stockpile mineral resource areas. Each mineral resource area is broken out individually in Table 4. Mineral resources defined within this July 11, 2024, the Cactus Project MRE will be used to form the basis of the ASCU Preliminary Economic Assessment (“PEA”), on track for release in early Q3 2024.

TABLE 1: Cactus Project MRE, Contained Copper Separated into Total Copper and Soluble Copper

Material
Type
Tons
kt
Grade
CuT %
Grade
Cu Tsol %
Contained
Total Cu (k lbs)
Contained
Cu Tsol (k lbs)
Measured
Total Leachable55,2000.940.791,032,200873,800
Total Primary12,3000.510.05124,40013,400
Total Measured67,5000.860.661,156,500887,200
Indicated
Total Leachable414,8000.600.534,965,0004,365,700
Total Primary150,4000.390.041,173,300126,000
Total Indicated565,2000.540.406,138,2004,491,700
M&I
Total Leachable470,0000.640.565.997,2005,239,500
Total Primary162,7000.400.041,297,600139,400
Total M&I632,6000.580.437,294,8005,378,900
Inferred
Total Leachable299,6000.430.382,572,4002,262,800
Total Primary174,5000.360.041,267,500124,700
Total Inferred474,0000.410.253,839,9002,387,500

NOTES:
1. Total soluble copper grades (Cu TSol) are reported using sequential assaying to calculate the soluble copper grade. Tons are reported as short tons.
2. Stockpile resource estimates have an effective date of 1st March, 2022, Cactus mineral resource estimates have an effective date of 29th April, 2022, Parks/Salyer-MainSpring mineral resource estimates have an effective date of 11th July, 2024. All mineral resources use a copper price of US$3.75/lb.
3. Technical and economic parameters defining mineral resource pit shells: mining cost US$2.43/t; G&A US$0.55/t, 10% dilution, and 44°-46° pit slope angle.
4. Technical and economic parameters defining underground mineral resource: mining cost US$27.62/t, G&A US$0.55/t, and 5% dilution. Underground mineral resources are only reported for material located outside of the open pit mineral resource shells. Designation as open pit or underground mineral resources are not confirmatory of the mining method that may be employed at the mine design stage.
5. Technical and economic parameters defining processing: Oxide heap leach (HL) processing cost of US$2.24/t assuming 86.3% recoveries, enriched HL processing cost of US$2.13/t assuming 90.5% recoveries, sulphide mill processing cost of US$8.50/t assuming 92% recoveries. HL selling cost of US$0.27/lb; Mill selling cost of US$0.62/lb.
6. Royalties of 3.18% and 2.5% apply to the ASCU properties and state land respectively. No royalties apply to the MainSpring property.
7. Variable cut-off grades were reported depending on material type, potential mining method, potential processing method, and applicable royalties. For ASCU properties – Oxide open pit or underground material = 0.099% or 0.549% TSol respectively; enriched open pit or underground material = 0.092% or 0.522% TSol respectively; primary open pit or underground material = 0.226% or 0.691% CuT respectively.For state land property – Oxide open pit or underground material = 0.098 % or 0.545% TSol respectively; enriched open pit or underground material = 0.092% or 0.518% TSol respectively; primary openpit or underground material = 0.225% or 0.686% CuT respectively.For MainSpring properties – Oxide openpit or underground material = 0.096% or 0.532% TSol respectively; enriched open pit or underground material = 0.089% or 0.505% TSol respectively; primary open pit or underground material = 0.219% or 0.669% CuT respectively. Stockpile cutoff = 0.095% TSol.
8. Mineral resources, which are not mineral reserves, do not have demonstrated economic viability. The estimate of mineral resources may be materially affected by environmental, permitting, legal, title, sociopolitical, marketing, or other relevant factors.
9. The quantity and grade of reported inferred mineral resources in this estimation are uncertain in nature and there is insufficient exploration to define these inferred mineral resources as an indicated or measured mineral resource; it is uncertain if further exploration will result in upgrading them to an indicated or measured classification.
10. Totals may not add up due to rounding.

George Ogilvie, Arizona Sonoran Copper Company President and CEO commented, “The new Parks/Salyer deposit, inclusive of MainSpring could be transformational for the Company as we foresee the opportunity to right size a larger operation and rescope Parks/Salyer to an open pit mine. The pending result would lead to reduced mining execution risks and lowered operating costs which could manifest themselves in improved Project economics.  The key difference in the larger mineral resource used for the pending PEA, relates to the MainSpring property acquisition and subsequent inferred drilling program identifying the continuation of near surface mineralization south of Parks/Salyer.”

Doug Bowden, Arizona Sonoran Copper Company VP Exploration stated, “Our Cactus Project is a successful copper porphyry growth story resulting from an aggressive exploration program. Our mineral resource journey began with our initial PEA in 2021, and continuously expanded outward from the Cactus Pit area to include Parks/Salyer and most recently MainSpring within the 5.5 km mine trend. The Parks/Salyer discovery includes significant quantities of high-grade (+1.00% CuT) copper, similar to the grades in Cactus East (as shown in FIGURES  2 and 3). Through systematic step out and infill drilling following our first mineral resource in 2021 to today’s update, our Cactus Project MRE indicates an increase to the M&I by an impressive 353%, from 1.61 Billion lbs to 7.29 Billion lbs of copper, while the inferred mineral resources increased 94%, from 1.98 Billion lbs to 3.84 Billion lbs. Lastly, these mineral resource areas have responded favorably and impressively to infill drilling with a consistently high conversion rate into higher resource classifications and will look forward to future infill programs as we move through the technical studies.”

Cactus Mineral Resources Estimate
The Parks/Salyer mineral resources as shown in FIGURE 3, inclusive of MainSpring, indicate 339.0 M short tons @ 0.71% CuT in the M&I category and 299.2 M short tons @ 0.43% CuT in the Inferred Category. Notably, Parks/Salyer is mostly contained within an optimized resource open pit shell indicating the rescoped potential of open pit mining of the deposit with the inclusion of shallower mineralization located on the MainSpring property. Parks/Salyer mineral resources were calculated with a cutoff date of March 31, 2024. There are no material changes to the Cactus East, West and Stockpile deposits as reported within the FEB 21, 2024 PFS.

For the purposes of the MRE, Cactus East reports as open pit mineral resources in compliance with Reasonable Prospects for Eventual Economic Extraction (“RPEEE”). For the purposes of the pending PEA, Cactus East is expected to be exploited as an underground operation.

Table 2 below reports a direct like–for-like comparison of the updated July 11, 2024, MRE, to the MRE comprising the Prefeasibility Study (“PFS”) MRE and illustrates a significant change to the Measured (+1,900%) and Inferred (+60%) categories, as it relates to successful expansion and infill programs at Parks/Salyer, including the MainSpring Property. The Table below calculates a combination of the Soluble Copper grades and Total Copper grades based on the leachable (oxides and enriched) zones, and the primary sulphides, respectively, going forward, mineral resources will calculate both the contained Total Copper and Soluble Copper inventory. Table 2 uses the same notes and assumptions as Table 1.

Table 2: The Cactus Project Mineral Resource Estimate, as of July 11, 2024, as Compared to August 31, 2023

 PREVIOUS MINERAL RESOURCE
(As of August 31, 2023)
UPDATED MINERAL RESOURCE
(As of July 11, 2024)
VARIANCE
Material TypeTons
kt
Grade
Cu%¹
Contained
Cu k lbs
Tons
kt
Grade
Cu%¹
Contained
Cu k lbs
Cu Content
%
Leachable9,1000.23¹41,90055,2000.79¹873,8001,985%
Primary1,3000.328,00012,3000.51124,4001,455%
Total Measured10,4000.2449,80067,5000.74998,2001,904%
Leachable348,5000.63¹4,387,200414,8000.53¹4,365,7000%
Primary86,8000.43737,000150,4000.391,173,30059%
Total Indicated435,3000.595,124,200565,2000.495,539,0008%
Leachable357,6000.62¹4,429,000470,0000.56¹5,239,50018%
Primary88,0000.42745,000162,7000.401,297,60074%
Total M&I445,7000.585,174,000632,6000.526,537,10026%
Leachable107,7000.61¹1,307,900299,6000.38¹2,262,80073%
Primary126,2000.36900,000174,5000.361,267,50041%
Total Inferred233,8000.472,207,900474,0000.373,530,30060%

NOTES: refer to TABLE 1
1 Grade shown is Soluble Copper (Cu TSol)

Drilling programs
The updated Cactus Project MRE is supported by a systematic drilling program targeting MainSpring, the near surface southern extension of the Parks/Salyer deposit, and infill to measured drilling at Parks/Salyer, within the 5.5 kilometre (“km”) (~3.5 mile (“mi”)) mine trend. Mineral resources were classified using data of 125 ft (38 m) drill spacing for Measured, 250 ft (76 m) drill spacing for Indicated and 500 ft (~152 m) drill spacing for Inferred. The in-ground mineral resources were calculated using 435 total drillholes including 161 new holes drilled into the Cactus West and East deposits since 2019 and 159 new holes drilled into the Parks/Salyer deposits since 2020. The Stockpile mineral resource was calculated using 514 new holes drilled into the stockpile on a regular grid since 2021. The isolated MainSpring mineral resource estimate containing 244.9 M short tons @ 0.39% CuT, is shown in TABLE 3 below, while each deposit is broken out separately within TABLE 4.

TABLE 3: MainSpring Property Resource contained within New Parks/Salyer Mineral Resource

Material
Type
Tons
kt
Grade
CuT %
Grade
Cu Tsol %
Contained
Total Cu (k lbs)
Contained
Cu Tsol (k lbs)
Inferred
Total Leachable200,1000.390.341,562,7001,370,300
Total Primary44,8000.380.04344,00033,100
Total Inferred244,9000.390.291,906,7001,403,500

NOTES: refer to TABLE 1

TABLE 4: Cactus Project Mineral Resources by Resource Area

Material
Type
Tons
kt
Grade
CuT %
Grade
Cu Tsol %
Contained
Total Cu (k lbs)
Contained
Cu Tsol (k lbs)
Measured
LeachableParks Salyer O/P45,0001.090.92981,200828,700
Parks Salyer U/G51.300.92100100
Cactus O/P10,2000.250.2250,80045,000
Cactus U/Gn/a
Stockpilen/a
Total Leachable         55,2000.930.79     1,032,100      873,800
 
PrimaryParks Salyer O/P10,9000.530.06115,50012,200
Parks Salyer U/G400.770.07700100
Cactus O/P1,3000.320.048,2001,100
Cactus U/Gn/a
Stockpilen/a
Total Primary12,3000.510.05124,40013,400
Total Measured67,5000.860.661,156,500887,200
Indicated
 LeachableParks Salyer O/P201,3000.750.663,027,0002,671,100
Parks Salyer U/G1,1000.960.8521,40018,900
Cactus O/P131,0000.550.491,446,1001,277,000
Cactus U/G10,2001.040.89213,100181,100
Stockpile71,1000.180.15257,400217,600
Total Leachable414,8000.600.534,965,0004,365,700
 
 PrimaryParks Salyer O/P80,4000.420.04680,60069,200
Parks Salyer U/G1000.770.121,200200
Cactus O/P68,3000.340.03465,80045,100
Cactus U/G1,6000.810.3625,70011,500
Stockpilen/a
Total Primary150,4000.390.041,173,300126,000
Total Indicated565,2000.540.406,138,2004,491,700
Measured & Indicated
 LeachableParks Salyer O/P246,3000.810.714,008,2003,499,800
Parks Salyer U/G1,1000.980.8621,50019,000
Cactus O/P141,2000.530.471,496,9001,322,000
Cactus U/G10,2001.040.89213,100181,100
Stockpile71,1000.180.15257,400217,600
Total Leachable470,0000.640.565,997,2005,239,500
 
 PrimaryParks Salyer O/P91,3000.440.04796,10081,400
Parks Salyer U/G1000.950.151,900300
Cactus O/P69,6000.340.03474,00046,200
Cactus U/G1,6000.800.3625,70011,500
Stockpilen/a
Total Primary162,7000.400.041,297,600139,400
Total M&I632,6000.580.437,294,8005,378,900
Inferred
 LeachableParks Salyer O/P234,5000.420.381,990,2001,767,500
Parks Salyer U/G9,6000.840.76161,200146,300
Cactus O/P50,4000.340.28344,600286,900
Cactus U/G3,9000.940.7772,80059,100
Stockpile1,2000.150.133,6003,000
Total Leachable299,6000.430.382,572,4002,262,800
 
 PrimaryParks Salyer O/P54,1000.390.04427,30041,000
Parks Salyer U/G1,0000.820.2616,7005,300
Cactus O/P117,8000.340.03798,70068,300
Cactus U/G1,5000.820.3324,90010,200
Stockpilen/a
Total Primary174,5000.360.041,267,600124,800
Total Inferred474,0000.410.253,839,9002,387,500

NOTES: refer to TABLE 1

Cactus Project Mineral Resource Modelling
The geological modelling, statistical analysis, and resource estimation in respect of the Cactus Project MRE were prepared by the ASCU resource team and by Allan Schappert – CPG #11758, who is a qualified person as defined by National Instrument 43-101– Standards of Disclosure for Mineral Projects (“NI 43-101”).

The Cactus Project MRE updates are based upon updated drilling data and interpretations. The Cactus Mineral Resource model was developed in Vulcan. Drilling data is supported by industry standard quality assurance and quality control programs, with quality control sampling comprising preparation blanks, certified reference materials, and field and pulp duplicate analyses. Review of the QA/QC data indicates it is of a quality suitable for use in resource estimation.

The mineralized domains are consistent with domaining for porphyry copper systems. Mineralized domains represent combinations of rock type and copper mineral zonation associated with secondary copper enrichment weathering processes. The main mineral zones are leached, oxide, enriched, and primary. Mineral zones are determined by logging and the assay attributes of sequential copper analyses.

Physical density measurements have been undertaken across the deposits, both historically by ASARCO, and more recently by ASCU. Density measurements on inground deposits use the wet / dry weight method and comprise 3,372 samples for Cactus and 143 samples for Parks/Salyer. Due to the unconsolidated nature of the stockpile material, physical bulk density measurements were attained by weight and volume calculations. Four test holes were excavated from which the material removed was dried and weight and the volume of each hole calculated.

Copper grades were estimated using Ordinary Kriging, using 20 ft (6.1 m) composites and top cutting determined by log normal probability plots on a per domain basis. Grade estimates were validated using visual and statistical methods including statistical distribution comparisons, visual comparison against the drilling data on sections, swath plots comparing block grades trends against de-clustered composites, and by smoothing checks using change of support. The effective date of the Cactus Project MRE is July 11, 2024. The Cactus Project MRE will form the basis of a PEA technical report prepared in accordance with NI 43-101, and prepared by M3 Engineering, which will be filed on SEDAR+ under the Company’s issuer profile within 45 days of this news release and will also be available at such time on the Company’s website. The PFS will be superseded in all respects once the Company has publicly disclosed the PEA.

Quality Assurance / Quality Control
Drilling completed on the project between 2020 and 2024 was supervised by on-site ASCU personnel who prepared core samples for assay and implemented a full QA/QC program using blanks, standards, and duplicates to monitor analytical accuracy and precision. The samples were sealed on site and shipped to Skyline Laboratories in Tucson AZ for analysis. Skyline’s quality control system complies with global certifications for Quality ISO9001:2008.

Scientific and technical information contained in this news release have been reviewed and verified by Allan Schappert – CPG #11758, who is a qualified person as defined by NI 43-101.

Links from the Press Release
Figures: https://arizonasonoran.com/projects/cactus-mine-project/press-release-images/
February 21, 2024: https://arizonasonoran.com/news-releases/arizona-sonoran-announces-a-positive-pre-feasibility-study-for-the-cactus-mine-project-with-a-us-509m-post-tax-npv-and-55-kstpa/

Neither the TSX nor the regulating authority has approved or disproved the information contained in this news release.

About Arizona Sonoran Copper Company (www.arizonasonoran.com | www.cactusmine.com)
ASCU’s objective is to become a mid-tier copper producer with low operating costs and to develop the Cactus Project that could generate robust returns for investors and provide a long term sustainable and responsible operation for the community and all stakeholders. The Company’s principal asset is a 100% interest in the brownfield Cactus Project (former ASARCO, Sacaton mine) which is situated on private land in an infrastructure-rich area of Arizona. The Company is led by an executive management team and Board which have a long-standing track record of successful project delivery in North America complemented by global capital markets expertise.

For more information:

Alison Dwoskin, Director, Investor Relations
647-233-4348
adwoskin@arizonasonoran.com

George Ogilvie, President, CEO and Director
416-723-0458
gogilvie@arizonasonoran.com

Forward-Looking Statements
This news release contains certain information that may constitute “forward-looking information” under applicable Canadian securities legislation. All information, other than historical fact, are forward-looking information. Generally, statements containing forward-looking information or statements can be identified by the use of forward-looking terminology such as “plans”, “expect”, “is expected”, “in order to”, “is focused on” (a future event), “estimates”, “intends”, “anticipates”, “believes” or variations of such words and phrases or statements that certain actions, events or results “may”, “could”, “would”, or the negative connotation thereof. Forward looking information includes, but is not limited to, the Company’s future operations, future exploration and development activities or other development plans, the potential of the Cactus Project (including the Parks/Salyer deposit), timing of economic studies and mineral resource estimates including the filing of the technical report in respect of the Cactus Project MRE, the results (if any) of further exploration work to define and or upgrade mineral resources and reserves at the Company’s properties; the anticipated exploration, drilling, development, construction and other activities of ASCU and the result of such activities; the mineral resources and mineral reserves estimates of the Cactus Project including the Cactus Project MRE (and the assumptions underlying such estimates); the ability of exploration work (including drilling) to accurately predict mineralization; the ability of management to understand the geology and potential of the Cactus Project; the completion and timing for the filing of the technical report in respect of the Cactus Project MRE; the timing and ability of the Company to produce a preliminary economic assessment (if at all); the scope of any future technical reports and studies conducted by ASCU; the ability to realize upon mineralization in a manner that is economic; the impact of bringing the Parks/Salyer deposit including the MainSpring property into the mine plan; , and corporate and technical objectives. Forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements of ASCU to be materially different from any future results, performance or achievements expressed or implied by the forward-looking statements. Such risks and uncertainties that could affect the outcome include, among others: future prices and the supply of metals; risks relating to fluctuations in the Canadian dollar and other currencies relative to the US dollar; the results of drilling; the ability to access capital on terms acceptable to the Company necessary to incur the expenditures required to retain and advance the properties; changes in exploration, development or mining plans due to exploration results and changing budget priorities of the Company or its joint venture partners; environmental liabilities (known and unknown); general business, economic, competitive, political and social uncertainties; results of exploration programs or further exploration work; the ability to continue exploration and development of the ASCU properties; changes in any of the assumptions underlying the Cactus Project MRE; accidents, labour disputes and other risks of the mining industry; political instability, terrorism, insurrection or war; or delays in obtaining governmental approvals, projected cash operating costs, failure to obtain any required consents, permits or approvals; and the additional risks described in ASCU’s most recently filed Annual Information Form, annual and interim management’s discussion and analysis, copies of which are available on SEDAR+ (www.sedarplus.ca) under ASCU’s issuer profile.

Although ASCU 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 to differ from those anticipated, estimated or intended. The Company considers its assumptions to be reasonable based on information currently available but cautions the reader that their assumptions regarding future events, many of which may be beyond the control of the Company, may ultimately prove to be incorrect since they are subject to risks and uncertainties that affects the Company and its operations. Accordingly, readers should not place undue reliance on forward-looking information and are urged to carefully consider the foregoing factors as well as other uncertainties and risks outlined in the Company’s public disclosure record. Forward-looking statements contained herein are made as of the date of this news release and ASCU disclaims any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or results or otherwise, except as required by applicable securities laws.

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Energy Junior Mining Project Generators

What Rome’s Currency Debasement Tells us About the Future of the US Dollar…

By David Stockman

July 13, 2024

Well, here’s an interesting historical repeat. Apparently, it took the Roman Empire about 200 years to reduce the value of its currency, the silver Denarius, by 95%. As shown in the chart below, the silver content of the Roman currency had been nearly 100% at the peak of the Empire in 65 AD, but by 268 AD the coin had been clipped and debased so thoroughly that it was comprised of less than 5% silver.

Needless to say, inflation became rampant, causing the financial foundation of the Roman Empire to eventually collapse. In the process, future generations and nations got an unmistakable lesson: Debauching the money is absolutely not the road to sustainable prosperity.

Unfortunately, that has not prevented governments from attempting the currency depreciation route again and again. In our own era, the 111 year history of the Federal Reserve provides a striking case in point. In roughly half the time it took the Romans, the Fed has managed to accomplish the same 95% depreciation of the US dollar.

That’s right. The purchasing power of the consumer dollar as measured by the CPI has dropped from 100 cents when the Fed opened for business in 1914 to barely 3 cents today.

Index of Dollar’s Purchasing Power Since 1914 As Measured By The CPI

And yet and yet. After the most recent surge of inflation, the Fed is at it again. In today’s Congressional testimony, Chairman Powell as much as claimed victory and implied that the next round of rate cuts would soon commence, perhaps as early as September.

Reducing policy restraint too late or too little could unduly weaken economic activity and employment,” Powell said as part of his semiannual update on monetary policy. “More good data would strengthen our confidence that inflation is moving sustainably toward 2 percent.”

Let’s not mince words. What in the hell is he talking about?Schweizer, PeterBest Price: $10.54Buy New $18.15(as of 06:37 UTC – Details)

The implication is that the Fed never has to make amends. If the inflation genie gets out of the bottle and pushes the general price level sharply higher, why the thing to do is to just brake the surge and advise the people to lick their wounds with respect to the depleted value of their savings and the waning purchasing power of their paycheck.

In fact, current Fed policy is simply a one-way ratchet. If inflation exceeds its utterly arbitrary 2.00% target, there is no off-setting correction and restoration of purchasing power. Effectively cumulative inflation is written off as a bad debt.

Unfortunately for main street households and businesses, this embedded inflation-ratchet policy assumes inflation is an equal opportunity cipher. That is to say, even at the Fed’s sacrosanct 2.00% target, the cost of goods and services goes up 2.00% and so, purportedly, wages, rents, profits, interest and all other forms of income rise in lockstep. No one is worse for the inflationary wear—households and businesses just need to keep adjusting both sides of their income statements and balance sheets by the Fed’s preferred PCE deflator and all will be copacetic.

That’s absurd on its face, of course. Right from the get go its obvious that borrowers would get a windfall of depreciated debts and savers would suffer severe confiscation of wealth over even a quarter century—to say nothing of the one and two century debauch of the silver Denarius and dollar shown above. In fact, after 25-years at the Fed’s precise 2.00% target, borrowers would be 40% richer and savers 40% poorer than under a regime of true price stability.

Why in the world today’s central bankers insist upon punishing savers and rewarding borrowers is no mystery. They embrace lock, stock and barrel—whether they acknowledge it or not—the horrid Keynesian fallacy that capitalism is inherently defective because humankind is wont to excessively save and hoard when they should be spending freely and living high on the hog.

It’s really that simple. Even a decent regard for the truism that economic growth and wealth gains are a function of savings and investment would negate the Fed’s pro-inflation policy on its face. Yet as it has happened, the drastic bias of central bank policy in favor of borrowers in all sectors—government, business, households and finance—has essentially extinguished America’s generation of net national savings.

As shown below, the latter measures the entirety of savings in the household and business sectors minus government borrowings. Yet since the Fed began de facto inflation-targeting in the late 1980s, the net national savings rate has headed steadily toward the zero bound. In fact, during Q1 2024 it was actually -0.5% of GDP— a figure on the opposite side of the universe compared to the +7-10% of GDP levels that prevailed during the heyday of middle class prosperity prior to the era of Bubbles Alan Greenspan and his heirs and assigns.

Needless to say, when there is nothing left in the savings till after governments gorge themselves at the borrowing window, where is the investment for productivity and growth supposed to come from?

In truth, the Fed never troubles itself with the question of savings. If the word is even mentioned at all in its post-meeting communiques it’s in the context of a short-run downward blip in household spending levels owing mathematically to what usually amounts to a tiny and transient increase in the savings rate.

Still, seven decades of data do not lie. Systematically and relentlessly, the Fed’s baleful bias against savers and for borrowers has literally dried-up the US economy’s supply of growth oxygen.

Net National Savings Rate. 1955 to 2024

For want of doubt, here is the inflation-adjusted interest rate on a two-years savings instrument, proxied here by the risk-free yield on the two-year UST minus the Y/Y change in the 16% trimmed mean CPI. The chart obviously speaks for itself, but it needs be noted that during the entire 15-year period between July 2008 on the eve of the Great Financial Crisis and July 2023, the geniuses in the Eccles Building had pegged the real yield at negative levels!

Check Amazon for Pricing.Even now after what the acolytes at the Wall Street Journal call the most rapid rise in interest rates in two decades, the real yield in May was just +1.4%. So why in the world is that considered onerous—a threat to the Fed’s alleged twin goal of maximum employment?

Stated differently, if the US economy can’t stand real rates peeking above the zero bound at just 1.4% on two-year instruments and is therefore in dire need of a new round of rate cuts, how in the world can the net national savings rate be lifted out of the economic gutter where it now resides?

Of course, the Fed never mentions real interest rates, either, except for the squirrely extractions it derives by comparing yields on inflation-protected treasuries (TIPS) versus their fixed coupon counterparts. But that has absolutely nothing to do with real yields, and merely reflects trading games played by technicians down in the bond pits.

Inflation-Adjusted Yield On 2-Year USTs, 1984 to 2024

Then again, the Fed subscribes to what amounts to bathtub economics. It thinks growth happens when demand is stimulated up to the brim of potential GDP, and that left to its own devices free market capitalism always whiffs by saving too much and spending too little. So cheap interest rates become the instrument of macro-economic stimulus, purportedly goosing demand until the bathtub of spending is full to the brim and economic growth and employment are maximized.

Alas, in a fully integrated and seamless $110 trillion global economy, the bathtub model of domestic economics is just plain hideous nonsense. Yet here were are again with the Keynesian fools in the Eccles Building itching to restart the printing presses and drive real interest rates and the net national savings rate back into the economic dungeon below the zero bound.

They never learn. Ever.

Reprinted with permission from David Stockman’s Contra Corner.

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Former Congressman David A. Stockman was Reagan’s OMB director, which he wrote about in his best-selling book, . His latest books are The Great Deformation: The Corruption of Capitalism in America and . He’s the editor and publisher of the new David Stockman’s Contra Corner. He was an original partner in the Blackstone Group, and reads LRC the first thing every morning.

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Base Metals Energy Junior Mining Project Generators

One Mile Step-Out at Agate Intercepts Favorable Grades and Thickness

Kelowna, British Columbia–(Newsfile Corp. – July 16, 2024) – Strathmore Plus Uranium Corporation (TSXV: SUU) (OTCQB: SUUFF) (“Strathmore” or “the Company“) is pleased to announce a new discovery of uranium in the Middle sand, one mile south of the company’s expanding northern trend. All previous drilling encountered uranium mineralization only in the Lower sand. The middle sand was the most prolific producer historically in the Shirley Basin. This exciting southern discovery shows increasing grades and above average thickness.

Southeast Mineralized Trend (Middle Sand, Wind River Formation)
Hole IDLatitudeLongitudeDepth (ft)Top (ft)Bottom (ft)Thickness (ft)Grade %
eU
3O8
Grade x
Thickness
AG-135-2442.30389(106.27831)12016.032.516.50.0350.578
AG-137-2442.30365(106.27874)14017.528.010.50.0320.336
AG-138-2442.30446(106.27828)12036.540.54.00.0620.248
AG-143-2442.30500(106.27869)12030.544.514.00.0460.644
AG-147-2442.30580(106.27865)12029.044.515.50.0510.791

Mr. John DeJoia said, “We are excited to hit a mile away. The initial results of the one mile step out to the south has opened a whole new aspect to the agate project. With the discovery of mineralization exhibiting good ISR GT’s (grade thickness), in the middle sand of the Wind River Formation, we now have the potential for a much larger area of mineralization development in an additional sand unit of the Wind River. This is much like the main roll system that was successfully mined to the east. The results of exploration at the Agate Project are responding as our geologic model predicted. We are very excited by this latest step out discovery.”

AGATE PROJECT:

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Mr. Terrence Osier, VP Exploration said, “We are extremely encouraged by the Agate project as we have greatly expanded the length of the northern trend from the 2023 discovery. We encountered uranium mineralization, one mile south, in the Middle sand of the Wind River Formation, the primary sand mined in Shirley Basin. The company had only encountered mineralization in the Lower sand before this. This Middle sand discovery increases our potential to have stacked roll fronts across portions of the property, which will greatly increase our resource potential. I look forward to ongoing work to model the uranium deposits we’ve drilled with results to guide our Phase 2 autumn exploration plans.”

This summer five core holes are planned to compliment groundwater studies from closely located monitor wells. The core will be used for chemical equilibrium studies and by the University of Wyoming for their ongoing geophysical research at the project. In autumn Phase 2 drilling of an additional 100 exploratory holes is scheduled. Planned drilling intends to expand the northern trend into untested ground, including on recently staked claims, and along the newly discovered, shallow Middle zone into deeper ground to the north. The intent of the exploration is to expand the mineralization on the property into a multi-zone deposit, with the potential of stacked roll fronts.

Note: The tabled geophysical results are based on equivalent uranium (eU3O8) of the gamma-ray probes calibrated at the Department of Energy’s Test Facility in Casper, Wyoming. A series E Century Geophysical logging tool with gamma-ray, spontaneous potential, resistivity, and drift detectors was utilized. The reader is cautioned that the reported uranium grades may not reflect actual concentrations due to the potential for disequilibrium between uranium and its gamma emitting daughter products.

About the Agate Property
The Agate property consists of 85 wholly owned lode mining claims covering 1,756 acres. The uranium mineralization is contained in classic Wyoming-type roll fronts within the Eocene Wind River Formation, an arkosic-rich sandstone. Historically, 53 million pounds of uranium were mined in Shirley Basin, including from open-pit, underground, and the first commercial in-situ recovery operation in the USA during the 1960s. At the property, the uranium mineralization is shallow, from 20 to approximately 150 feet deep, much of which appears below the water table and likely amenable to in-situ recovery. Kerr McGee Corporation, the largest US uranium mining company at the time, drilled at least 650 holes across the project area in the 1970s, delineating several targets of potential mineralization. In 2023 and 2024, the Company completed 200 exploration holes on the Project, discovering several areas of potential mineralization. Additional drilling is planned for autumn 2024.

About Strathmore Plus Uranium Corp. Strathmore is focused on discovering uranium deposits in Wyoming, and has three permitted uranium projects including Agate, Beaver Rim, and Night Owl. The Agate and Beaver Rim properties contain uranium in typical Wyoming-type roll front deposits based on historical drilling data. The Night Owl property is a former producing surface mine that was in production in the early 1960s.

Cautionary Statement: “Neither the TSX Venture Exchange nor its Regulation Services Provider (as the term is defined in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.”

Certain information contained in this press release constitutes “forward-looking information”, within the meaning of Canadian legislation. Generally, these forward-looking statements 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”, “be achieved” or “has the potential to”. Forward-looking statements contained in this press release may include statements regarding the future operating or financial performance of Strathmore Plus Uranium Corp. which involve known and unknown risks and uncertainties which may not prove to be accurate. Actual results and outcomes may differ materially from what is expressed or forecasted in these forward-looking statements. Such statements are qualified in their entirety by the inherent risks and uncertainties surrounding future expectations. Among those factors which could cause actual results to differ materially are the following: market conditions and other risk factors listed from time to time in our reports filed with Canadian securities regulators on SEDAR at www.sedar.com. The forward-looking statements included in this press release are made as of the date of this press release and Strathmore Plus Uranium Corp. disclaim any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except as expressly required by applicable securities legislation.

Qualified Person
The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and reviewed on behalf of the company by Terrence Osier, P.Geo., Vice President, Exploration of Strathmore Plus Uranium Corp., a Qualified Person.

Strathmore Plus Uranium Corp.
Contact Information:
Investor Relations
Telephone: 1 888 882 8177
Email: info@strathmoreplus.com

ON BEHALF OF THE BOARD
“Dev Randhawa”
Dev Randhawa, CEO

To view the source version of this press release, please visit https://www.newsfilecorp.com/release/216554

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Base Metals Energy Junior Mining Oil & Gas

Peabody to Announce Results for the Quarter Ended June 30, 2024

ST. LOUIS, July 16, 2024 /PRNewswire/ — On Thursday, August 1, 2024, Peabody (NYSE: BTU) will announce results for the quarter ended June 30, 2024.  A conference call with management is scheduled for 10 a.m. CT on Thursday, August 1, 2024.

Instructions for the conference call participation and accessing a replay, as well as other investor data will be available at PeabodyEnergy.com prior to the call.

Participants may also access the call using the following phone numbers:

U.S. Toll Free                   1 833 816 1387
Canada Toll Free            1 866 284 3684
International Toll            1 412 317 0480

Peabody (NYSE: BTU) is a leading coal producer, providing essential products for the production of affordable, reliable energy and steel.  Our commitment to sustainability underpins everything we do and shapes our strategy for the future.  For further information, visit PeabodyEnergy.com.

Contact:
Karla Kimrey
314.342.7900

Peabody. (PRNewsFoto/Peabody Energy)
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Civil War 2.0

Bob Moriarty
Archives
Jul 15, 2024

I’ve done a number of interviews lately because there are a lot of people talking about things they have no understanding of. Such as war and geopolitics.

If you remember back to the Gulf War reporting, the people on the boob tube were breathlessly commenting on “Daisy Cutters” as if they were some sort of giant bombs. While it is so that the Air Force used giant 10,000-pound bombs to clear landing zones, the term “Daisy Cutter” didn’t refer to the bomb but to the 36-inch-long fuse that detonated the bomb before it reached the earth.

As an F-4B pilot and later an O-1C and O-1G Birddog Forward Air Controller I dropped and controlled hundreds of 500-pound Mark-82 bombs and 750-pound Mark-83 bombs which used the Daisy Cutter fuses to clear landing zones. Daisy Cutter is the fuse, not the bomb.

And every time I hear some talking head mumbling about how Russia is the aggressor in the Ukraine war, I get an urge to gag. Have they all forgotten the $5 billion spent by Victoria Nuland to bring Democracy to Ukraine in 2014 by ridding them of their duly elected President in favor of a thug installed by the Neocons? How about the immortal phrase spoken by Nuland when organizing which thug would the US put into power?

Fuck the EU. I hope that is deeply engraved on her tombstone one day because it perfectly shows the US interest in Democracy.

The MSM has failed to even mention the 14,000 dead from the Ukrainians shelling mostly women and children from 2014 to 2022 in Donbas. And none of them mention the 100,000 NATO trained and armed Ukrainian soldiers poised on the border with Donbas ready to invade. It was scheduled for March 10th 2022.

I think Civil War 2.0 began in a meaningless Trump speech in some Podunk town in Pennsylvania on July 13. The dust has yet to settle but this begins to smell like a long dead fish floating on the top of a swamp.

In what appears to be a credible interview of someone attending the Trump rally we are told that numerous watchers saw a young man carrying a rifle go on top of a building a mere 135 meters or so from where former President Trump was speaking. The watchers attempted to notify the Secret Service and police of the dangerous event of a gunman within easy rifle range of Trump but were ignored.

The shooter managed to aim his rifle and fire a number of rounds towards Trump. From the sound of the rifle to me it appears the sniper was firing a .22 caliber rifle probably with .22 Long Rifle rounds. If you make a head shot, the person hit is going down, likely on a permanent basis. I carried a .22 caliber Colt Woodsman pistol in Vietnam as a survival weapon. I could hit someone at 50 meters in the head and kill them. So, someone basically familiar with a .22 rifle at 135 meters is pretty much point-blank range.

Through a total fluke the shooter missed and only nicked Trump’s ear lobe. An inch or two away from a fatal wound. Clearly there was a giant failure on the part of the Secret Service. Much has been made of the numerous viewers who tried and seemingly failed to garner the attention of either local police or the Secret Service.

There is a very famous picture of two counter snipers on another rooftop about 130 meters or so from the assassin’s position. You may wonder why they didn’t see and take down the shooter.

According to someone calling himself Jonathan Willis, he is one of the two counter snipers on the roof to protect Trump. They had to have seen the assassin but took no action.

Jonathan Willis or someone posting as him says they were forbidden by the head of the Secret Service to shoot until the sniper fired. Willis claims he had the sniper in his sights for at least three minutes and his superiors refused to clear him to shoot.

If you listen to any of the many videos of the attempted assassination you can hear the gunman fire a number of rounds from what would probably be a semi-automatic .22 rifle. A mere second or two after he fired you can hear multiple rounds being fired almost certainly from the counter snipers. Many of the reports call the counter snipers members of the Secret Service but I don’t think they were. I think they were local police snipers. Their uniforms were marked Police and what Jonathan Willis wrote in his entry on X he sounds like a policeman.

Certainly, if the Secret Service refused to allow their own snipers to shoot an assassin and the shooter managed to wound Trump the agent would be told to keep his mouth shut. If Jonathan Willis was in fact one of the counter snipers and was police rather than Secret Service, he wasn’t about to allow the world to think the failure to shoot was his fault.

The timing of the various shots being fired suggests he tells the truth. If the counter snipers didn’t know where the shots were coming from, it would take them a few seconds to determine where the threat originated. They couldn’t have acquired the shooter and manage to kill him a couple of seconds after he fired at Trump and did manage to kill someone attending the rally.

If the top agent of the Secret Service at this rally refused to allow the counter snipers to do their jobs, this was a coup. A deliberate coup on the part of the Secret Service to kill Trump.

We will know on July 15th if it was deliberate or a simple but well-meaning mistake. If the Secret Service agent in charge is fired today it could have been a stupid mistake. If the agent is not fired, it means there is a coverup in progress.

I’ve done ten to fifteen interviews in the last month or so. When asked I made it clear that it is my belief that Biden will not be the Democrat candidate for the Presidential election in November. Lots of viewers didn’t agree with me but clearly there is no chance Biden will be the Democrat choice. He can’t complete a rational sentence. He confuses Zelensky with Putin and believes Trump is his black appointment as Vice President. Biden and the Democrats are destroying what remains of the American attempt at Empire.

And I have made it clear in a number of interviews that Donald Trump terrifies the Democrats to the point that there have been a lot of suggestions that the best way to protect America is to assassinate Trump. They are logically afraid that if Trump is elected, he will do the same thing to them that they have done to him for at least eight years. A mere week ago Biden was calling for Trump to be put in the bullseye. On the 13th of July Biden’s wish came true.

Call it Civil War 2.0 or simply a coup d’état but the Deep State operatives have shown their true colors.

This next week is probably going to be one of the most critical weeks in US history. Millions of military age men have been allowed to enter the US illegally, given money, a cell phone, food and accommodations. Some of them have to be double agents brought in by someone or somebody to create panic and chaos at the right time.

It would be no problem for these young men to be given weapons, ammo and targets. All we need for Martial Law to be imposed would be to have a few dozen random attacks by illegals all across the country. Then the Democrats could do what Zelensky did in Ukraine. When his term expired, he simply ignored the law and stayed in office. Biden/Harris might well conclude that’s just a spiffy idea.

If we don’t have migrants running around shooting people another alternative is for the Deep State to start whacking political candidates for office on both sides. If it works in South America, Mexico and Serbia why can’t it work here? In Mexico alone thirty-seven candidates were killed in this latest election in June of 2024. No doubt we can surpass that number in the US with candidates being whacked by the Deep State on both sides.

I’m not a fan of Alex Jones. As far as I can tell he isn’t dealing with a full deck. But in a short video he put out on Saturday he suggests we have had a coup. He might well be right and if so, we will know shortly.

Call it the intro to Civil War 2.0

###

Bob Moriarty
President: 321gold
Archives

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Energy Junior Mining Precious Metals

Gold79 Announces Trenching Results from the Tyro Main Zone; Trench 1 Returned 39.7m of 1.14 g/t Au Including 9.5m of 2.08 g/t Au

Ottawa, Ontario–(Newsfile Corp. – July 11, 2024) – Gold79 Mines Ltd. (TSXV: AUU) (OTCQB: AUSVF) (“Gold79” or the “Company”) is pleased to announce that it has received the assay results from its recently completed trenching program along the Tyro Main Zone which has confirmed our understanding of the geology, added new potential high-grade targets for the next drill campaign and extended the zone along strike to the northeast.

Highlights from the program include:

  • Confirmed the geologic model where the White Spar Fault intersects the Tyro Main Zone. Trench 1 (T1) returned 39.7m of 1.14 g/t Au including 9.5m of 2.08 g/t Au. In 2023, drilling returned 51.1 g/t Au over 9.1m (GC23-28) about 40 to 50m below these surface exposures.
  • Identified new fault structures intersecting the Tyro Main Zone trending north to northwest (similar to the White Spar fault), providing additional high-grade potential zones.
  • Extended the Tyro Main Zone to the northeast by approximately 40m with Trench 13 (T13) returning 4.7m of 7.64 g/t Au, where it remains open to the northeast.

Derek Macpherson, President and CEO stated, “The data collected in this low-cost exploration effort has improved our understanding of the Tyro Main Zone geology, particularly the impact of the White Spar fault on the SW portion (Decimal Hill Zone) and the high-grades previously drilled at this intersection. With this data, we are starting to plan the next phases of drilling potentially allowing Gold79 to deliver a maiden resource that would be higher-grade and larger than the current deposits in the region.”

A total of 15 trenches were excavated across 358m with a total of 217 chip-channel samples collected. Highlights of the analytical results are presented in Table 1.

Table 1. Summary of the Tyro Main Vein trenching program.

To view an enhanced version of this graphic, please visit:
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In addition to the sampling, all trenches were mapped with the results presented in Figure 1.

Figure 1: Geologic map of the Tyro vein system showing recently completed trenches (T1-T15), Phase 1 and Phase 2 drill hole locations and surface rock sample gold values.

To view an enhanced version of this graphic, please visit:
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Summary

The trenching program has provided Gold79 a combination of better geologic control and a higher sample density. The result is greater confidence that the White Spar fault was active at essentially the same time as the Tyro Main vein but movement continued after the Tyro vein allowing for downward offset of the Decimal Hill zone. This better explains the gold values at Decimal Hill (Table 1: T1, T2, T3 and T3B). Additionally, the results serve to better constrain the limits of gold-bearing veins surrounding the shallow pit; important widths and grades have been documented on 3 sides (Table 1: T4, T5, T6 and T15). In the NE Tyro zone, trenches have exposed broad zones of chalcedony veining and breccia with variable widths and grades (Table 1: T7 thru T12). Most importantly, the northernmost trench, T13, identified beneath alluvial cover a zone of silicification hosting quartz veinlets and breccia with 7.64 g/t Au over 4.7 metres. This brings meaningful gold grades closer to our Frisco Graben target where the suspected gold zone is concealed beneath vapor-dominated alteration.

The Tyro Main Zone is composed of several gold-bearing stages emplaced into a NE-trending, steeply dipping structural corridor which has seen repeated movement. This low sulfidation, epithermal vein system can be divided into 3 zones (SW to NE; Figure 1): 1. Decimal Hill; 2. Tyro Mine Zone; and, 3. The Tyro NE Zone. These zones are essentially defined by north-northwest-trending faults which were likely operative both during and after the Tyro mineralizing events.

Figure 2. Geologic map of the Decimal Hill Zone showing mine workings, drill holes, trenches and surface samples.

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Decimal Hill Zone

The Decimal Hill zone, covering about 300 metres of the Tyro Main vein southwest of the mine, is situated at the intersection of the Tyro and White Spar structural corridors (Figure 2). In addition to the structural intersection, the area hosts the convergence of several rhyolite dikes whose faulted contacts may have provided avenues of ingress to the gold-bearing fluids. This zone is characterized by both north- to northeast-trending veins and breccia and NW-trending veins and breccia. The veins here lack the textural banding, adularia and reveal diminished gold values (i.e. <3 g/t Au; Figure 3).

This trenching campaign, along with the geologic mapping, has confirmed that the Decimal Hill Zone contains both NW- and N-NE-trending veins suggesting that both structural corridors were operative prior to and during the mineralizing stages. The White Spar trend clearly hosted a greater component of post-mineral movement. This later movement is manifested by relatively small offsets of the veins along the Tyro structural corridor resulting in the structural juxtaposition of high-level vein textures and gold grades (Figure 3) with textures and gold grades more indicative of the ‘bonanza’ or boiling zone (i.e. Tyro Mine zone; Figure 4).

Figure 3: Sample No. 0743 (1.15 g/t Au): Hydrothermal breccia composed of Precambrian granite and multi-stage vein fragments including quartz-replaced lattice texture, massive white chalcedony and crustiform-banded chalcedony-adularia rimming massive quartz fragments, Decimal Hill Zone.

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5717/216119_69da767954f31a63_004full.jpg

Tyro Mine Zone

The Tyro Mine Zone, shown in Figure 5, a N30oE-trending zone of sub-parallel and sub-vertical veins, veinlets and hydrothermal breccia, extends from the White Spar fault intersection to the top of Tyro Hill, a distance of about 430 metres (Figure 5). The zone hosts most of the mining activity conducted between 1915 and 1941 and in the 1980s. This includes the Tyro Shaft, reported to be 500 feet deep, the 200 Level and a slot pit developed on the highest-grade portion of the vein. The 200 Level defines the lowest level of selective production although there was some development along the vein to the 300 Level. The 200 Level defines the bottom of the slot pit and hosts a broad zone, 20 to 30 metres wide, of NE-trending chalcedony-adularia-calcite veins (Figure 4). Only two holes have been drilled beneath the Tyro Mine Zone, Hole Nos. GC23-23 (44.4m at 2.01 g/t Au) and GC23-24 (25.9m at 2.27 g/t Au).

Figure 4. Sample No. 0184 – 13.27 g/t Au: Crustiform-banded quartz-chalcedony-adularia vein with internal hydrothermally brecciated vein fragments cemented by olive-green chalcedony, Tyro Mine Zone.

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5717/216119_69da767954f31a63_005full.jpg

Figure 5. Geologic map of the Tyro Mine Zone showing mine workings, drill holes, trenches and surface samples.

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https://images.newsfilecorp.com/files/5717/216119_69da767954f31a63_006full.jpg

Northeast Tyro Zone

The Northeast Tyro Zone extends from the top of Tyro Hill (Figure 1) at N60oE for about 300 metres where it disappears beneath an alluvium filled valley before it intersects the Frisco Mine fault, the southwest margin of the Frisco Graben. This zone commences at the intersection of a NNW-trending post-mineral fault (Figure 5) where the Tyro structural corridor rotates clockwise about 30and flattens slightly to 70-80 degrees southeast. The initial 100 or so metres of the vein is characterized by a zone of silicified amphibolite and granite with weak to moderate chalcedony veinlets and stockwork. Trenches T7 and T8 were cut across this zone (Figure 5) with locally anomalous gold values. Trenches T9, T10 and T11 traverse a broad zone of strong quartz-chalcedony veins, stockwork and vein breccia with variable gold values, i.e. T11 – 7.6m @ 4.43 g/t Au. Between T10 and T11, a 60 metre segment of the vein complex, up to 5m wide, has been stoped to about 20m below the surface. Drilling beneath this zone by Gold79 in 2021 traversed up to 21.3m @ 2.0 g/t Au (GC21-15). The NE extent of the Tyro vein is obscured by dumps and alluvium where T13 was excavated to identify a concealed extension to the vein. Trench 13 traversed a zone of silicified amphibolite and granite containing quartz-chalcedony veinlets and breccia with 4.7m @ 7.64 g/t Au. The Tyro structure remains concealed by alluvial deposits for about 400 metres to the northeast where it intersects the Frisco Mine fault characterized by high-level silica-clay-hematite alteration.

Figure 6. Geologic map of the Northeast Tyro Zone showing mine workings, drill holes, trenches and surface samples.

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5717/216119_69da767954f31a63_007full.jpg

Closing of Private Placement Financing

The Company has closed its non-brokered private placement financing previously announced on April 11, 2024 and May 6, 2024. Gross proceeds of $718,250 was raised through the issuance of 2,873,000 units at $0.25 per unit. Each unit consists of one common share of the Company and one-half common share purchase warrant. A total of 1,436,500 whole warrants were issued, with each warrant entitling the holder to purchase one common share of the Company at a price of $0.30 per share until May 3, 2026. The warrants are callable, at the option of the Company, in the event that the 20-day volume-weighted average price of the Company’s common shares meets or exceeds $0.50 for 10 consecutive trading days based on trades on the TSX Venture Exchange and alternative trading systems. Subscribers will be notified of the call provision being triggered and will have a 30-day period to exercise the warrants.

Cash finder’s fees of $4,200 were paid and 16,800 finder warrants were issued. The finder warrants are exercisable at $0.30 per share and expire May 3, 2026.

This private placement is subject to the final approval of the TSX Venture Exchange. All securities issued in the placement are subject to a statutory hold period until Sept. 4, 2024.

Officers and directors of the Company participated in the private placement and acquired 900,000 units for $225,000. The participation of these insiders in the private placement constitutes a related-party transaction within the meaning of Multilateral Instrument 61-101 — Protection of Minority Security Holders in Special Transactions. The board of directors of the Company, with participating directors abstaining, determined that the transaction is exempt from the formal valuation and minority shareholder approval requirements contained in sections 5.5(a) and 5.7(1)(a) of MI 61-101 for the related-party transaction, as neither the fair market value of securities issued to the insiders nor the consideration paid by the insiders exceeded 25 percent of the Company’s market capitalization. The Company did not file a material change report in respect of the transaction 21 days in advance of the closing of the private placement because insider participation had not been confirmed. The shorter period was necessary in order to permit the Company to close the private placement in a time frame consistent with usual market practice for transactions of this nature.

Qualified Person / Quality Control and Quality Assurance

Robert Johansing, M.Sc. Econ. Geol., P. Geo., the Company’s Vice President, Exploration is a qualified person (“QP”) as defined by NI 43-101 and has reviewed and approved the technical content of this press release. Mr. Johansing has also been responsible for the trenching program including sample collection, labelling, bagging and transport from the project to American Assay Laboratories of Sparks, Nevada. Samples were then dried, crushed and split, and pulp samples were prepared for analysis. Gold was determined by fire assay with an ICP finish, over limit samples were determined by fire assay and gravimetric finish. Silver plus 34 other elements were determined by Aqua Regia ICP-AES, over limit samples were determined by fire assay and gravimetric finish. Gold standards and blanks were inserted into the sample chain along with QAQC procedures conducted by American Assay. Standard sample chain of custody procedures were employed during field work until delivery to the analytical facility.

About Gold79 Mines Ltd.

Gold79 Mines Ltd. is a TSX Venture listed company focused on building ounces in the Southwest USA. Gold79 has four gold projects, two of which are partnered with major gold producers (Kinross at Jefferson Canyon and Agnico at Greyhound). Gold79 is focused on establishing a maiden resource at its Gold Chain project in Arizona and advancing its Tip Top Project in Nevada.

For further information regarding this press release contact:

Derek Macpherson, President & CEO
Phone: 416-294-6713
Email: dm@gold79mines.com
Website: www.gold79mines.com.

Book a 30-minute meeting with our CEO here.

FORWARD-LOOKING STATEMENTS:

This press release may contain forward-looking statements that are made as of the date hereof and are based on current expectations, forecasts and assumptions which involve risks and uncertainties associated with our business including any future private placement financing, the uncertainty as to whether further exploration will result in the target(s) being delineated as a mineral resource, capital expenditures, operating costs, mineral resources, recovery rates, grades and prices, estimated goals, expansion and growth of the business and operations, plans and references to the Company’s future successes with its business and the economic environment in which the business operates. All such statements are made pursuant to the ‘safe harbour’ provisions of, and are intended to be forward-looking statements under, applicable Canadian securities legislation. Any statements contained herein that are statements of historical facts may be deemed to be forward-looking statements. By their nature, forward-looking statements require us to make assumptions and are subject to inherent risks and uncertainties. We caution readers of this news release not to place undue reliance on our forward-looking statements as a number of factors could cause actual results or conditions to differ materially from current expectations. Please refer to the risks set forth in the Company’s most recent annual MD&A and the Company’s continuous disclosure documents that can be found on SEDAR at www.sedar.com. Gold79 does not intend, and disclaims any obligation, except as required by law, to update or revise any forward-looking statements whether as a result of new information, future events or otherwise.

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.

To view the source version of this press release, please visit https://www.newsfilecorp.com/release/216119

Categories
Base Metals Energy Junior Mining Uncategorized

Strathmore Triples Length of Mineralized Trend at Agate

Kelowna, British Columbia–(Newsfile Corp. – July 9, 2024) – Strathmore Plus Uranium Corporation (TSXSUU) (OTCQB: SUUFF) (“Strathmore” or “the Company“) is pleased to announce it has extended the mineralization from the Phase 1 drilling for the 2024 exploration season at the Agate project in Wyoming. The Company completed 100 exploration holes across the project area, resulting in the extension of the Lower sand’s northern trend to 3,700 feet in length.

Highlights for the drilling along this trend included holes:

*AG-175-24 (7.5 feet of 0.128% eU3Ofrom 103.5-110.0 feet)
*AG-200-24 (15 feet of 0.116% eU3O8 from 82.5-97.5 feet).
*AG-162-24 (16 feet of 0.067% eU3Ofrom 87.5-103.5 feet)

In addition, five piezometer wells were completed for groundwater testing and five holes were prepared for core recovery this summer.

Phase 1 of the 2024 drilling explored the Eocene Wind River Formation, an arkosic-rich sandstone which is noted for its high porosity and permeability, and high groundwater transmissivity. In addition to continued exploration of the Lower sand, the recent drilling discovered shallow mineralization within the overlying Middle sand, which is thicker than the Lower sand, and historically produced most of the uranium in the Shirley Basin district.

Dev Randhawa, CEO commented:

The BOD and I, along with our new Director, Mr. Marion Loomis, and technical advisors Ray Ashley and Sam Hartmann, toured both our Agate and Beaver Rim properties on June 26 & 27th.

We are excited to see the higher-grade intercepts as we move further SW. at Agate. The drill results are validating our prediction of the Wyoming roll front model as applied to our Agate property. With continued exploration by our field team and geophysical modeling by the University of Wyoming personnel, I expect Strathmore to further define the east side of the mineralized tongue at Agate and move towards a draft ISR resource assessment.

Agate Exploration:

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/3282/215737_ae406299f46f3955_002full.jpg

Hole IDLatitudeLongitudeDepth (ft)Top (ft)Bottom (ft)Thickness (ft)Grade % eU3O8Grade x Thickness
AG-101-2442.30469(106.29538)12080.586.05.50.0170.094
AG-102-2442.30502(106.29534)12084.598.013.50.0260.351
AG-103-2442.30474(106.29495)12074.582.58.00.0350.280
AG-104-2442.30447(106.29533)10081.087.06.00.0190.114
AG-105-2442.30500(106.29573)12086.598.512.00.0140.168
AG-106-2442.30472(106.29573)10079.083.04.00.0370.148
86.589.02.50.0460.115
AG-107-2442.30446(106.29579)12080.583.53.00.0340.102
88.592.54.00.0440.176
AG-108-2442.30529(106.29531)12088.090.02.00.0230.046
AG-109-2442.30558(106.29533)12084.587.02.50.0310.078
89.599.510.00.0320.320
AG-110-2442.30531(106.29493)12082.592.510.00.0190.190
AG-111-2442.30477(106.29610)12083.092.09.00.0260.231
AG-112-2442.30505(106.29608)12081.585.03.50.0230.081
AG-113-2442.30505(106.29493)12083.093.010.00.0220.219
AG-114-2442.30528(106.29573)12084.595.511.00.0140.154
AG-115-2442.30566(106.29493)12088.089.51.50.0310.047
AG-116-2442.30561(106.29456)12083.087.54.50.0270.122
AG-117-2442.30590(106.29494)12075.087.512.50.0150.188
AG-118-2442.30589(106.29459)12087.0100.513.50.0240.324
AG-119-2442.30553(106.29558)12087.5105.518.00.0330.594
AG-120-2442.30293(106.29702)140BARREN
AG-121-2442.30318(106.29700)120BARREN
AG-122-2442.30346(106.29699)12089.594.55.00.0220.110
AG-123-2442.30322(106.29739)14090.092.02.00.0240.048
94.0101.07.00.0140.098
AG-124-2442.30349(106.29736)14090.095.05.00.0170.085
AG-125-2442.30373(106.29697)12091.094.03.00.0270.081
AG-126-2442.30319(106.29662)12084.088.54.50.0190.086
AG-127-2442.30374(106.29738)14097.099.02.00.0150.030
AG-128-2442.30320(106.29744)14092.098.06.00.0130.078
AG-129-2442.30370(106.29668)12086.588.52.00.0130.026
AG-130-2442.30402(106.29697)12090.094.54.50.0590.266
AG-131-2442.30360(106.27836)13019.027.08.00.0300.242
31.534.02.50.0220.055
41.043.02.00.0280.056
AG-132-2442.30414(106.27911)10037.542.04.50.0290.131
48.550.52.00.0120.024
63.565.52.00.0120.024
AG-133-2442.30417(106.27866)10037.539.52.00.0130.026
41.563.522.00.0130.288
68.071.03.00.0150.045
AG-134-2442.30387(106.27872)12042.550.58.00.0130.105
56.058.52.50.0130.033
62.564.52.00.0110.022
AG-135-2442.30389(106.27831)12016.032.516.50.0350.578
34.036.52.50.0130.033
44.048.54.50.0250.113
AG-136-2442.30335(106.27836)1009.513.03.50.0130.046
20.024.04.00.0120.048
35.542.57.00.0140.095
45.049.04.00.0140.056
AG-137-2442.30365(106.27874)14017.528.010.50.0320.336
32.536.03.50.0270.095
AG-138-2442.30446(106.27828)12036.540.54.00.0620.248
Hole IDLatitudeLongitudeDepth (ft)Top (ft)Bottom (ft)Thickness (ft)Grade % eU3O8Grade x Thickness
AG-139-2442.30417(106.27832)12043.549.05.50.0180.099
AG-140-2442.30387(106.27802)12033.536.53.00.0160.048
40.044.04.00.0130.052
AG-141-2442.30445(106.27869)12035.041.56.50.0130.085
67.069.02.00.0120.024
AG-142-2442.30469(106.27872)12034.036.02.00.0350.070
62.565.02.50.0150.038
70.072.02.00.0140.028
AG-143-2442.30500(106.27869)12030.544.514.00.0460.644
51.056.05.00.0100.052
64.571.06.50.0120.076
AG-144-2442.30503(106.27821)12016.023.07.00.0130.094
30.532.52.00.0410.082
36.540.54.00.0380.152
AG-145-2442.30559(106.27820)12018.020.02.00.0120.024
23.028.05.00.0110.055
33.536.02.50.0120.030
44.048.54.50.0140.063
53.057.04.00.0140.056
61.064.53.50.0130.044
71.073.52.50.0120.030
AG-146-2442.30535(106.27869)12020.523.53.00.0130.038
25.548.022.50.0140.304
AG-147-2442.30580(106.27865)12029.044.515.50.0510.791
57.068.011.00.0130.143
AG-148-2442.30610(106.27818)12028.031.53.50.0110.037
35.048.013.00.0130.165
54.056.52.50.0110.027
AG-149-2442.31234(106.29066)140101.0104.53.50.0460.161
110.5116.56.00.0110.068
AG-150-2442.31252(106.29057)140103.5107.54.00.0100.042
AG-151-2442.31322(106.29053)14095.0106.011.00.0790.869
AG-152-2442.31321(106.29016)160101.0105.54.50.0490.221
AG-153-2442.31352(106.29048)140BARREN
AG-154-2442.31353(106.29015)14093.095.52.50.0270.068
AG-155-2442.31353(106.28978)14090.593.02.50.0390.098
94.5100.05.50.0600.330
AG-156-2442.31321(106.28978)16098.5108.09.50.0560.532
AG-157-2442.31293(106.29090)140100.5103.02.50.0370.093
104.5106.52.00.0250.050
AG-158-2442.31321(106.29090)14092.597.04.50.0120.054
AG-159-2442.31321(106.28945)160107.0109.02.00.0280.056
AG-160-2442.31351(106.28942)14095.099.54.50.0440.198
AG-161-2442.31364(106.28944)14091.5102.511.00.0210.231
AG-162-2442.31295(106.29128)14077.579.52.00.0360.072
87.5103.516.00.0671.072
AG-163-2442.31269(106.29129)140107.0108.51.50.0130.020
AG-164-2442.31266(106.29090)14099.5105.05.50.0330.182
AG-165-2442.31266(106.29168)140105.0107.52.50.0130.033
AG-166-2442.31298(106.29164)14083.586.02.50.0370.093
AG-167-2442.31295(106.29201)14080.583.02.50.0290.073
Hole IDLatitudeLongitudeDepth (ft)Top (ft)Bottom (ft)Thickness (ft)Grade % eU3O8Grade x Thickness
85.587.52.00.0400.080
89.591.52.00.0270.054
AG-168-2442.31251(106.29198)14078.580.52.00.0680.136
91.594.02.50.0110.028
97.5104.06.50.0140.088
AG-169-2442.31230(106.29179)14096.0100.54.50.0140.063
102.0107.05.00.0140.070
AG-170-2442.31241(106.29229)140101.0104.53.50.0130.046
AG-171-2442.31270(106.29229)14090.092.52.50.0150.038
94.5101.06.50.0130.085
105.5107.52.00.0110.021
AG-172-2442.31216(106.29212)14097.0107.010.00.0140.138
AG-173-2442.31213(106.29257)140101.5107.05.50.0680.374
AG-174-2442.31246(106.29262)140BARREN
AG-175-2442.31191(106.29215)140103.5111.07.50.1280.960
AG-176-2442.31196(106.29282)140BELOW CUTOFF
AG-177-2442.31175(106.29253)14059.563.03.50.0120.042
108.5112.03.50.0200.070
AG-178-2442.31162(106.29217)14051.053.02.00.0110.022
69.572.53.00.0130.040
109.5113.54.00.0100.041
AG-179-2442.31186(106.29178)140109.0112.03.00.0450.135
AG-180-2442.31231(106.29144)14085.091.56.50.1220.793
95.099.04.00.0380.152
AG-181-2442.31135(106.29262)14080.586.05.50.0230.127
101.5113.011.50.0150.172
AG-182-2442.31129(106.29219)140100.0112.012.00.0140.168
AG-183-2442.31209(106.29182)140100.0102.52.50.0370.093
105.0108.53.50.0140.050
112.0114.02.00.0120.024
AG-184-2442.31204(106.29146)14096.099.53.50.0550.193
100.0110.510.50.0140.147
AG-185-2442.31220(106.29104)14084.586.52.00.0120.024
93.596.02.50.0150.038
98.0103.05.00.0180.090
105.0107.02.00.0100.020
AG-186-2442.31108(106.29362)140112.0121.09.00.0620.558
AG-187-2442.31076(106.29367)140115.0117.02.00.0330.066
117.0129.012.00.0120.141
AG-188-2442.31065(106.29429)140110.5129.018.50.0120.221
AG-189-2442.31040(106.29429)140109.0111.52.50.0230.058
116.5121.55.00.0120.062
AG-190-2442.31080(106.29329)140108.5113.55.00.0930.465
AG-191-2442.31046(106.29470)160124.5132.07.50.0150.113
AG-192-2442.31022(106.29472)140111.0116.05.00.0120.062
117.5127.09.50.0170.162
AG-193-2442.31029(106.29502)14096.0101.05.00.0120.058
113.5122.59.00.0140.122
124.0130.06.00.0160.096
AG-194-2442.31015(106.29529)140112.5120.58.00.0160.128
AG-195-2442.31095(106.29429)160130.0133.53.50.0160.056
Hole IDLatitudeLongitudeDepth (ft)Top (ft)Bottom (ft)Thickness (ft)Grade % eU3O8Grade x Thickness
AG-196-2442.31353(106.28906)14096.0100.04.00.0290.116
AG-197-2442.31352(106.28869)14097.0103.06.00.0130.078
AG-198-2442.31373(106.28866)14097.0105.08.00.0330.266
AG-199-24-MW42.31395(106.28670)125NOT LOGGED
AG-200-24-MW42.31502(106.28512)13082.597.515.00.1161.740

Note: The geophysical results are based on equivalent uranium (eU3O8) of the gamma-ray probes calibrated at the Department of Energy’s Test Facility in Casper, Wyoming. A series E Century Geophysical logging tool with gamma-ray, spontaneous potential, resistivity, and drift detectors was utilized. The reader is cautioned that the reported uranium grades may not reflect actual concentrations due to the potential for disequilibrium between uranium and its gamma emitting daughter products.

  • Mineralized holes with thicker, higher-grade intercepts are interpreted to be in the Near Interface, Nose (main front), or Near Seepage ground located within the projected roll front system.
  • Mineralized holes with thinner, below cutoff grade intercepts are interpreted to be in the Limb/Tails or Remote Seepage ground located behind (altered) or ahead (reduced) of the projected roll front system, respectively.
  • Non-mineralized holes are interpreted to be in the Barren Exterior ground located ahead of the projected roll front system in reduced ground.
  • The drill results were determined using thickness and grade % cutoffs of 2-feet and 0.01% eU3O8.

The 2024 drilling was completed by Single Water Services utilizing a mud-rotary rig and the geophysical logging was completed by Hawkins CBM Logging, both of Wyoming with extensive experience in the uranium industry. Mr. Terrence Osier, PG, VP Exploration for Strathmore, was the supervising Geologist and oversaw the drilling activities and lithologic descriptions of the drilled cuttings which were sampled at 5-foot intervals. The drilling was completed on budget (US$275,000) and in a timely manner over a month’s time. The results of the exploration will be analyzed and assist in the layout of additional drill sites proposed for the Phase 2 drilling in autumn 2024.

New Claims Staked

In addition to exploration, the Company has expanded the project area by staking 18 new mining claims continuous to the current claim group, bringing the project total to 85 mining claims. The new claims cover ground where mineralization is anticipated to be on trend with recent and historical drilling. Strathmore plans to amend the drill permit following the Phase 1 drilling to include the new mining claims and anticipates exploration of the acquired ground in Phase 2 drilling later this year.

About the Agate Property

The Agate property consists of 85 wholly owned lode mining claims covering 1,756 acres. The uranium mineralization is contained in classic Wyoming-type roll fronts within the Eocene Wind River Formation, an arkosic-rich sandstone. Historically, 53 million pounds of uranium were mined in Shirley Basin, including from open-pit, underground, and the first commercial in-situ recovery operation in the USA during the 1960s. At the property, the uranium mineralization is shallow, from 20 to approximately 150 feet deep, much of which appears below the water table and likely amenable to in-situ recovery. Kerr McGee Corporation, the largest US uranium mining company at the time, drilled at least 650 holes across the project area in the 1970s, delineating several targets of potential mineralization.

About Strathmore Plus Uranium Corp. Strathmore is focused on discovering uranium deposits in Wyoming, and has three permitted uranium projects including Agate, Beaver Rim, and Night Owl. The Agate and Beaver Rim properties contain uranium in typical Wyoming-type roll front deposits based on historical drilling data. The Night Owl property is a former producing surface mine that was in production in the early 1960s.

Cautionary Statement: “Neither the TSX Venture Exchange nor its Regulation Services Provider (as the term is defined in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release”.

Certain information contained in this press release constitutes “forward-looking information”, within the meaning of Canadian legislation. Generally, these forward-looking statements 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”, “be achieved” or “has the potential to”. Forward looking statements contained in this press release may include statements regarding the future operating or financial performance of Strathmore Plus Uranium Corp. which involve known and unknown risks and uncertainties which may not prove to be accurate. Actual results and outcomes may differ materially from what is expressed or forecasted in these forward-looking statements. Such statements are qualified in their entirety by the inherent risks and uncertainties surrounding future expectations. Among those factors which could cause actual results to differ materially are the following: market conditions and other risk factors listed from time to time in our reports filed with Canadian securities regulators on SEDAR at www.sedar.com. The forward-looking statements included in this press release are made as of the date of this press release and Strathmore Plus Uranium Corp. disclaim any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except as expressly required by applicable securities legislation.

Qualified Person

The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and reviewed on behalf of the company by Terrence Osier, P.Geo., Vice President, Exploration of Strathmore Plus Uranium Corp., a Qualified Person.

Strathmore Plus Uranium Corp.

Contact Information:
Investor Relations
Telephone: 1 888 882 8177
Email: info@strathmoreplus.com

ON BEHALF OF THE BOARD
“Dev Randhawa”
Dev Randhawa, CEO

Neither 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.

To view the source version of this press release, please visit https://www.newsfilecorp.com/release/215737