20-F 1 form20-f.htm

 

 

 

UNITED STATES

SECURITIES AND EXCHANGE COMMISSION

Washington, D.C. 20549

 

FORM 20-F

 

☐ REGISTRATION STATEMENT PURSUANT TO SECTION 12(b) OR 12(g) OF THE SECURITIES EXCHANGE ACT OF 1934

 

OR

 

☒ ANNUAL REPORT PURSUANT TO SECTION 13 OR 15(d) OF THE SECURITIES EXCHANGE ACT OF 1934

 

For the fiscal year ended January 31, 2022

 

OR

 

☐ TRANSITION REPORT PURSUANT TO SECTION 13 OR 15(d) OF THE SECURITIES EXCHANGE ACT OF 1934

 

For the transition period from __________to__________

 

OR

 

☐ SHELL COMPANY REPORT PURSUANT TO SECTION 13 OR 15(d) OF THE SECURITIES EXCHANGE ACT OF 1934

 

Date of event requiring this shell company report ___________

 

Commission file number 000-52055

 

RED METAL RESOURCES LTD. 

(Exact name of Registrant as specified in its charter)

 

Not Applicable

(Translation of Registrant’s name into English)

 

British Columbia, Canada

(Jurisdiction of incorporation or organization)

 

1130 West Pender Street, Suite 820, Vancouver, BC V6E 4A4

(Address of principal executive offices)

 

Caitlin Jeffs, Telephone: 1.866.907.5403, Facsimile: 604-684-0517,

102-278 Bay St. Thunder Bay, ON P7B 1R8

(Name, Telephone, E-mail and/or Facsimile number and Address of Company Contact Person)

 

Securities registered or to be registered pursuant to Section 12(b) of the Act.

 

Title of each class   Name of each exchange on which registered
Not Applicable   Not Applicable

 

Securities registered or to be registered pursuant to Section 12(g) of the Act.

 

Common Shares Without Par Value

(Title of Class)

 

Securities for which there is a reporting obligation pursuant to Section 15(d) of the Act.

 

Not Applicable

(Title of Class)

 

Indicate the number of outstanding shares of each of the issuer’s classes of capital or common stock as of the close of the period covered by the annual report.

 

51,557,959 Common Shares without par value issued and outstanding as at January 31, 2022.

 

Indicate by check mark if the registrant is a well-known seasoned issuer, as defined in Rule 405 of the Securities Act. ☐ YES ☒ NO

 

If this report is an annual or transition report, indicate by check mark if the registrant is not required to file reports pursuant to Section 13 or 15(d) of the Securities Exchange Act of 1934. ☐ YES ☒ NO

 

Note - Checking the box above will not relieve any registrant required to file reports pursuant to Section 13 or 15(d) of the Securities Exchange Act of 1934 from their obligations under those Sections.

 

Indicate by check mark whether the registrant (1) has filed all reports required to be filed by Section 13 or 15(d) of the Securities Exchange Act of 1934 during the preceding 12 months (or for such shorter period that the registrant was required to file such reports), and (2) has been subject to such filing requirements for the past 90 days. ☒ YES ☐ NO

 

Indicate by check mark whether the registrant has submitted electronically and posted on its corporate website, if any, every Interactive Data File required to be submitted and posted pursuant to Rule 405 of Regulation S-T (232.405 of this chapter) during the preceding 12 months (or for such shorter period that the registrant was required to submit and post such files). ☒ YES ☐ NO

 

Indicate by check mark whether the registrant is a large accelerated filer, an accelerated filer, a non-accelerated filer or an emerging growth company. See definition of “accelerated filer”, “large accelerated filer”, and “emerging growth company” in Rule 12b-2 of the Exchange Act. (Check one):

 

Large accelerated filer ☐ Accelerated filer ☐
Non-accelerated filer ☒ Emerging growth company ☐

 

If an emerging growth company that prepares its financial statements in accordance with U.S. GAAP, indicate by check mark if the registrant has elected not to use the extended transition period for complying with any new or revised financial accounting standards† provided pursuant to Section 13(a) of the Exchange Act. ☐

 

† The term “new or revised financial accounting standard” refers to any update issued by the Financial Accounting Standards Board to its Accounting Standards Codification after April 5, 2012.

 

Indicate by check mark which basis of accounting the registrant has used to prepare the financial statements included in this filing:

 

U.S. GAAP ☐   International Financial Reporting Standards as issued
by the International Accounting Standards Board ☒
  Other ☐

 

If “Other” has been checked in response to the previous question, indicate by check mark which financial statement item the registrant has elected to follow. ☐ Item 17 ☐ Item 18

 

If this is an annual report, indicate by check mark whether the registrant is a shell company (as defined in Rule 12b 2 of the Exchange Act). ☐ YES ☒ NO

 

(APPLICABLE ONLY TO ISSUERS INVOLVED IN BANKRUPTCY PROCEEDINGS DURING THE PAST FIVE YEARS)

 

Indicate by check mark whether the registrant has filed all documents and reports required to be filed by Sections 12, 13 or 15(d) of the Securities Exchange Act of 1934 subsequent to the distribution of securities under a plan confirmed by a court.

☐ YES ☐ NO 

 

 

 

 
 

 

TABLE OF CONTENTS

 

GLOSSARY OF TECHNICAL TERMS 3
   
FORWARD-LOOKING STATEMENTS 6
   
CAUTIONARY NOTE TO UNITED STATES INVESTORS 7
   
PART I 8
   
Item 1 Identity of Directors, Senior Management and Advisers 8
Item 2 Offer Statistics and Expected Timetable 8
Item 3 Key Information 8
Item 4 Information on the Company 15
Item 4A Unresolved Staff Comments 49
Item 5 Operating and Financial Review and Prospects 50
Item 6 Directors, Senior Management and Employees 53
Item 7 Major Shareholders and Related Party Transactions 60
Item 8 Financial Information 62
Item 9 The Listing 64
Item 10 Additional Information 65
Item 11 Quantitative and Qualitative Disclosures About Market Risk 71
Item 12 Description of Securities Other than Equity Securities 72
   
PART II 73
   
Item 13 Defaults, Dividend Arrearages and Delinquencies. 73
Item 14 Material Modifications to the Rights of Security Holders and Use of Proceeds. 73
Item 15 Controls and Procedures 73
Item 16 [Reserved] 74
   
PART III 77
   
Item 17 Financial Statements 77
Item 18 Financial Statements 77
Item 19 Exhibits 77
   
SIGNATURE 78

 

2
 

 

GLOSSARY OF TECHNICAL TERMS

 

Term   Meaning   Term   Meaning
AEM   Airborne Electromagnetic   Na   sodium
Ag   Silver   Na2O   sodium oxide
Al   Aluminum   NE   northeast
Al2O3   aluminum oxide   NI   National Instrument
AW   apparent width   Ni   nickel
As   Arsenic   NSR   net smelter return
Au   Gold   NTS   National Topographic System
Ba   Barium   P   phosphorous
Be   Beryllium   P2O5   phosphorous oxide
Bi   Bismuth   Pb   Lead
C   carbon dioxide   Pd   Palladium
Ca   Calcium   pH   Acidity
CaO   calcium oxide   Pt   platinum
Cd   Cadmium   QA/QC   Quality Assurance/Quality Control
Co   Cobalt   S   south
CO2   carbon dioxide   S   sulfur
Cr   Chromium   Sb   antimony
Cr2O3   chromium oxide   SE   southeast
Cu   Copper   Se   selenium
DDH   diamond drill hole   SiO2   silicon oxide
DW   drilled width   Sn   tin
E   East   SO2   sulphur dioxide
EM   electromagnetic   Sr   strontium
Fe   Iron   Sum   summation
Fe2O3   iron oxide (ferric oxide-hematite)   SW   southwest
Fe3O4   iron oxide (ferrous oxide-magnetite)   Ti   titanium
HLEM   horizontal loop electromagnetic   TiO2   titanium oxide
H2O   hydrogen oxide (water)   Tl   thallium
IP   induced polarization   TW   true width
K   Potassium   U   uranium
K2O   potassium oxide   U3O8   uranium oxide (yellowcake)
Li   Lithium   UTM   Universal Transverse Mercator
LOI   loss on ignition (total H2O, CO2 and SO2 content)   V   vanadium
Mg   Magnesium   V2O5   vanadium oxide
MgO   magnesium oxide   VLF   very low frequency
Mn   Manganese   VLF-EM   very low frequency-electromagnetic
MnO   manganese oxide   W   west
Mo   Molybdenum   Y   yttrium
Mt   millions of tonnes   Zn   zinc
N   North        
NE   Northeast        
NW   Northwest        
S   South        

 

3
 

 

Units of Measure

 

Units of Measure   Abbreviation   Units of Measure   Abbreviation
Above mean sea level   amsl   Litre   L
Ampere   A   Litres per minute   L/m
Annum (year)   a   Megabytes per second   Mb/s
Billion years ago   Ga   Megapascal   MPa
British thermal unit   Btu   Megavolt-ampere   MVA
Candela   cd   Megawatt   MW
Carat   ct   Metre   m
Carats per hundred tonnes   cpht   Metres above sea level   masl
Carats per tonne   cpt   Metres per minute   m/min
Centimetre   cm   Metres per second   m/s
Cubic centimetre   cm3   Metric ton (tonne)   t
Cubic feet per second   ft3/s or cfs   Micrometre (micron)   μm
Cubic foot   ft3   Microsiemens (electrical)   μs
Cubic inch   in3   Miles per hour   mph
Cubic metre   m3   Milliamperes   mA
Cubic yard   yd3   Milligram   mg
Day   d   Milligrams per litre   mg/L
Days per week   d/wk   Millilitre   mL
Days per year (annum)   d/a   Millimetre   mm
Dead weight tonnes   DWT   Million   M
Decibel adjusted   dBa   Million tonnes   Mt
Decibel   dB   Minute (plane angle)  
Degree   °   Minute (time)   min
Degrees Celsius   °C   Month   mo
Degrees Fahrenheit   °F   Newton   N
Diameter   ø   Newtons per metre   N/m
Dry metric ton   dmt   Ohm (electrical)   Ω
Foot   ft   Ounce   oz
Gallon   gal   Parts per billion   ppb
Gallons per minute (US)   gpm   Parts per million   ppm
Gigajoule   GJ   Pascal   Pa
Gram   g   Pascals per second   Pa/s
Grams per litre   g/L   Percent   %
Grams per tonne   g/t   Percent moisture (relative humidity)   % RH
Greater than     Phase (electrical)   Ph
Hectare (10,000 m2)   ha   Pound(s)   lb
Hertz   Hz   Pounds per square inch   psi
Horsepower   hp   Power factor   pF
Hour   h (not hr)   Quart   qt
Hours per day   h/d   Revolutions per minute   rpm
Hours per week   h/wk   Second (plane angle)  
Hours per year   h/a   Second (time)   s
Inch    “(symbol, not “ )   Short ton (2,000 lb)   st
Joule   J   Short ton (US)   t
Joules per kilowatt-hour   J/kWh   Short tons per day (US)   tpd
Kelvin   K   Short tons per hour (US)   tph
Kilo (thousand)   k   Short tons per year (US)   tpy
Kilocalorie   kcal   Specific gravity (g/cm3)   SG
Kilogram   kg   Square centimetre   cm2

 

4
 

 

Units of Measure   Abbreviation   Units of Measure   Abbreviation
Kilograms per cubic metre   kg/m3   Square foot   ft2
Kilograms per hour   kg/h   Square inch   in2
Kilograms per square metre   kg/m2   Square kilometre   km2
Kilojoule   kJ   Square metre   m2
Kilometre   km   Thousand tonnes   kt
Kilometres per hour   km/h   Tonne (1,000kg)   t
Kilonewton   kN   Tonnes per day   t/d
Kilopascal   kPa   Tonnes per hour   t/h
Kilovolt   kV   Tonnes per year   t/a
Kilovolt-ampere   kVA   Total dissolved solids   TDS
Kilovolts   kV   Total suspended solids   TSS
Kilowatt   kW   Volt   V
Kilowatt hour   kWh   Week   wk
Kilowatt hours per short ton (US)   kWh/st   Weight/weight   w/w
Kilowatt hours per tonne (metric ton)   kWh/t   Wet metric ton   wmt
Kilowatt hours per year   kWh/a   Yard   yd
Kilowatts adjusted for motor efficiency   kWe   Year (annum)   a
Less than     Year   yr

 

The term grams/tonne (g/t) is expressed as “grams per tonne” where 1 gram/tonne = 1 ppm (parts per million) = 1000 ppb (parts per billion). Other abbreviations include oz/t = ounce per short ton; Moz = million ounces; Mt = million tonnes; t = tonne (1000 kilograms); SG = specific gravity; lb/t = pound/ton; and st = short ton (2000 pounds).

 

5
 

 

FORWARD-LOOKING STATEMENTS

 

Except for statements of historical fact relating to the Company, certain statements in this Annual Report, including the documents incorporated by reference herein, may constitute forward-looking information, future oriented financial information, or financial outlooks (collectively, “forward-looking information”) within the meaning of Canadian securities laws. Forward-looking information may relate to this Annual Report, the Company’s future outlook and anticipated events or results and, in some cases, can be identified by terminology such as “may”, “could”, “should”, “expect”, “plan”, “anticipate”, “believe”, “intend”, “estimate”, “projects”, “predict”, “potential”, “targeted”, “possible”, “continue” or other similar expressions concerning matters that are not historical facts and include, but are not limited in any manner to, those with respect to commodity prices, mineral resources, mineral reserves, realization of mineral reserves, existence or realization of mineral resource estimates, the timing and amount of future production, the timing of construction of any proposed mine and process facilities, capital and operating expenditures, the timing of receipt of permits, rights and authorizations, and any and all other timing, development, operational, financial, economic, legal, regulatory and political factors that may influence future events or conditions, as such matters may be applicable. In particular, this Annual Report contains forward-looking statements pertaining to the following:

 

expenditures for general and administrative expenses;
expectations regarding revenue, expenses and operations;
the Company having sufficient working capital and being able to secure additional funding necessary for the continued exploration of the Company’s mineral interests;
expectations regarding the potential mineralization, geological merit and economic feasibility of the Company’s projects;
expectations regarding drill programs and potential impacts thereof;
mineral exploration and exploration program cost estimates;
expectations regarding any environmental issues that may affect planned or future exploration programs and the potential impact of complying with existing and proposed environmental laws and regulations;
treatment under applicable governmental regimes for permitting and approvals; and
key personnel continuing their employment with the Company. See “Risk Factors”.

 

Such forward-looking statements are based on a number of material factors and assumptions, and include the ultimate determination of mineral reserves, if any, the availability and final receipt of required approvals, licenses and permits, sufficient working capital to develop and operate any proposed mine, access to adequate services and supplies, economic conditions, commodity prices, foreign currency exchange rates, interest rates, access to capital and debt markets and associated costs of funds, availability of a qualified work force, and the ultimate ability to mine, process and sell mineral products on economically favourable terms. While the Company considers these assumptions to be reasonable based on information currently available to it, they may prove to be incorrect. Actual results may vary from such forward-looking information for a variety of reasons, including but not limited to risks and uncertainties disclosed in this Annual Report. Forward-looking statements are based upon management’s beliefs, estimates and opinions on the date the statements are made and, other than as required by law, the Company does not intend, and undertakes no obligation to update any forward-looking information to reflect, among other things, new information or future events.

 

Investors are cautioned against placing undue reliance on forward-looking statements.

 

6
 

 

CAUTIONARY NOTE TO UNITED STATES INVESTORS

 

Unless otherwise indicated, all mineral resource estimates included in this Annual Report on Form 20-F have been prepared in accordance with Canadian National Instrument 43-101 - Standards of Disclosure for Mineral Projects (“NI 43-101”), and the Canadian Institute of Mining, Metallurgy and Petroleum Definition Standards for Mineral Resources and Mineral Reserves (“CIM Definition Standards”). NI 43-101 is a rule developed by the Canadian Securities Administrators which establishes standards for public disclosure an issuer makes of scientific and technical information concerning mineral projects. NI 43-101 permits the disclosure of a historical estimate made prior to the adoption of NI 43-101 that does not comply with NI 43-101 using the historical terminology if the disclosure: (a) identifies the source and date of the historical estimate; (b) comments on the relevance and reliability of the historical estimate; (c) states whether the historical estimate uses categories other than those prescribed by NI 43-101 and, if so, includes an explanation of the differences; and (d) includes any more recent estimates or data available.

  

Canadian standards, including NI 43-101, differ significantly from the requirements of the Securities and Exchange Commission (the “SEC”), and reserve and resource information contained in this Annual Report on Form 20-F may not be comparable to similar information disclosed by U.S. companies. In particular, and without limiting the generality of the foregoing, the term “resource” does not equate to the term “reserves”. Under U.S. standards, mineralization may not be classified as a “reserve” unless the determination has been made that the mineralization could be economically and legally produced or extracted at the time the reserve determination is made. The SEC’s disclosure standards normally do not permit the inclusion of information concerning “measured mineral resources”, “indicated mineral resources” or “inferred mineral resources” or other descriptions of the amount of mineralization in mineral deposits that do not constitute “reserves” by U.S. standards in documents filed with the SEC. U.S. investors should also understand that “inferred mineral resources” have a great amount of uncertainty as to their existence and great uncertainty as to their economic and legal feasibility. It cannot be assumed that all or any part of an “inferred mineral resource” will ever be upgraded to a higher category. Under Canadian rules, estimated “inferred mineral resources” may not form the basis of feasibility or pre-feasibility studies except in rare cases. Investors are cautioned not to assume that all or any part of an “inferred mineral resource” exists or is economically or legally mineable. Disclosure of “contained ounces” in a resource is permitted disclosure under Canadian regulations; however, the SEC normally only permits issuers to report mineralization that does not constitute “reserves” by SEC standards as in-place tonnage and grade without reference to unit measures. The requirements of NI 43-101 for identification of “reserves” are also not the same as those of the SEC, and reserves reported by our company in compliance with NI 43-101 may not qualify as “reserves” under SEC standards. Accordingly, information concerning mineral deposits set forth herein may not be comparable with information made public by companies that report in accordance with U.S. standards.

 

Foreign Private Issuer Filings

 

We are considered a “foreign private issuer” pursuant to Rule 405 promulgated under the Securities Act of 1933, as amended (the “Securities Act”). In our capacity as a foreign private issuer, we are exempt from certain rules under the Exchange Act that impose certain disclosure obligations and procedural requirements for proxy solicitations under Section 14 of the Exchange Act. In addition, our officers, directors and principal shareholders are exempt from the reporting and “short-swing” profit recovery provisions of Section 16 of the Exchange Act and the rules under the Exchange Act with respect to their purchases and sales of our common shares. Moreover, we are not required to file periodic reports and financial statements with the SEC as frequently or as promptly as United States companies whose securities are registered under the Exchange Act. In addition, we are not required to comply with Regulation FD, which restricts the selective disclosure of material information.

 

For as long as we are a “foreign private issuer” we intend to file our annual financial statements on Form 20-F and furnish our quarterly financial statements on Form 6-K to the SEC for so long as we are subject to the reporting requirements of Section 13(g) or15(d) of the Exchange Act. However, the information we file or furnish will not be the same as the information that is required in annual and quarterly reports on Form 10-K or Form 10-Q for U.S. domestic issuers. Accordingly, there may be less information publicly available concerning us than there is for a company that files as a domestic issuer. We will continue to file our Forms 20-F or 6-K until we are no longer a foreign private issuer. We are required to determine our status as a foreign private issuer on an annual basis at the end of our second fiscal quarter. We would cease to be a foreign private issuer at such time as more than 50% of our outstanding voting securities are held by United States residents and any of the following three circumstances applies: (1) the majority of our executive officers or directors are United States citizens or residents; (2) more than 50% of our assets are located in the United States; or (3) our business is administered principally in the United States. If we lose our “foreign private issuer status” we will be required to comply with Exchange Act reporting and other requirements applicable to U.S. domestic issuers, which are more detailed and extensive than the requirement for “foreign private issuers”.

 

7
 

 

PART I

 

FINANCIAL INFORMATION AND ACCOUNTING PRINCIPLES

 

The financial statements and summaries of financial information contained in this Annual Report on Form 20-F are reported in Canadian dollars (“$”) unless otherwise stated. A “tonne” is one metric ton or 2,204.6 pounds.

 

Item 1Identity of Directors, Senior Management and Advisers

 

Not applicable.

 

Item 2Offer Statistics and Expected Timetable

 

Not applicable.

 

Item 3Key Information

 

A.[Reserved]

 

B.Capitalization and Indebtedness

 

Not applicable.

 

C.Reasons for the Offer and Use of Proceeds

 

Not applicable.

 

D.Risk Factors

 

General

 

The Company is in the business of exploring and, if warranted, developing mineral properties, which is a highly speculative endeavor. A purchase of any of the Common Shares involves a high degree of risk and should be undertaken only by purchasers whose financial resources are sufficient to enable them to assume such risks and who have no need for immediate liquidity in their investment. An investment in the Common Shares should not constitute a significant portion of an individual’s investment portfolio and should be made only by persons who can afford a total loss of their investment. Prospective shareholders should evaluate carefully the following risk factors associated with an investment in the Common Shares.

 

The following risks and uncertainties could materially adversely affect the Company’s business, financial condition and results of operations. Additional risks and uncertainties not presently known to management of the Company or that are currently deemed immaterial may also impair the Company’s operations and financial condition.

 

Risks Relating to our recent Conversion and Continuation

 

We may still be treated as a U.S. corporation and taxed on our worldwide income after the conversion and continuation.

 

The conversion and continuation of our company from the State of Nevada to the Province of British Columbia, Canada is considered a migration of our company from the State of Nevada to the Province of British Columbia, Canada. Certain transactions whereby a U.S. corporation migrates to a foreign jurisdiction can be considered by the United States Congress to be an abuse of the U.S. tax rules because thereafter the foreign entity is not subject to U.S. tax on its worldwide income. Section 7874(b) of the Internal Revenue Code of 1986, as amended (the “Code”), was enacted in 2004 to address this potential abuse. Section 7874(b) of the Code provides generally that certain corporations that migrate from the United States will nonetheless remain subject to U.S. tax on their worldwide income unless the migrating entity has substantial business activities in the foreign country to which it is migrating when compared to its total business activities.

 

8
 

 

If Section 7874(b) of the Code applied to the migration of our company from the State of Nevada to the Province of British Columbia, Canada, our company would continue to be subject to United States federal income taxation on its worldwide income. Section 7874(b) of the Code could apply to our migration unless we had substantial business activities in Canada when compared to our total business activities.

 

We may be classified as a Passive Foreign Investment Company as a result of the merger and continuation.

 

Sections 1291 to 1298 of the Code contain the Passive Foreign Investment Company (“PFIC”) rules. These rules generally provide for punitive treatment of “U.S. holders” of PFICs. A foreign corporation is classified as a PFIC if more than 75% of its gross income is passive income or more than 50% of its assets produce passive income or are held for the production of passive income.

 

Because most of our assets after the conversion and continuation are in cash or cash equivalents and shares of our wholly-owned subsidiary, Minera Polymet SpA, we may in the future be classified as a PFIC. If we are classified as a PFIC, then the holders of shares of our company who are U.S. taxpayers may be subject to PFIC provisions which may impose U.S. taxes, in addition to those normally applicable, on the sale of their shares of our company or on distribution from our company.

 

Holders of shares of the Company who are U.S. taxpayers should consult their own tax advisors with respect to the application of the PFIC rules in their particular circumstances.

 

Negative Operating Cash Flow

 

During the years ended January 31, 2022 and 2021 the Company earned no revenue while the net loss from operations totaled $1,622,000 and $210,654, respectively. If the Company does not find sources of financing as and when needed, it may be required to cease its operations.

 

Mineral exploration and development are very expensive. During the fiscal year ended January 31, 2022, the Company had no revenue from its operations and its operating expenses totaled $1,520,118 (2021 - $357,570). These expenses were further increased by $118,144 (2021 - $105,766) in interest we accrued on our notes payable. These expenses were in part offset by $2,404 gain from foreign exchange fluctuation (2021 - $2,811 loss) and by $13,858 gain we recorded on forgiveness of debt (2021 - $255,493). Since inception, we have supported our operations through equity and debt financing and, to a minor extent, through option payments received on our option or joint venture agreements, and royalty payments from third-party vendors, who we allowed to mine our claims. Our ability to continue our operations, including exploring and developing our properties, will depend on our ability to generate operating revenue, obtain additional financing, or enter into joint venture agreements. Until we earn enough revenue to support our operations, which may never happen, we will continue to be dependent on loans and sales of our equity or debt securities to continue our development and exploration activities. If we do not find sources of financing as and when we need them, we may be required to severely curtail, or even to cease, our operations.

 

Insufficient Capital

 

The Company was incorporated on January 10, 2005, and to date has been involved primarily in organizational activities, acquiring and exploring mineral claims and obtaining financing. The Company’s financial statements have been prepared assuming that it will continue as a going concern. From the Company’s inception on January 10, 2005, the Company has accumulated losses of $12,144,764. As a result, the Company’s management has expressed substantial doubt about the Company’s ability to continue as a going concern. The continuation of the Company’s operations depends on its ability to complete equity or debt financings as needed or generate capital from profitable operations. Such financings may not be available or may not be available on reasonable terms. The Company’s financial statements do not include any adjustments that could result from the outcome of this uncertainty. Whether the Company will be successful as a mining company must be considered in light of the costs, difficulties, complications and delays associated with its proposed exploration programs. These potential problems include, but are not limited to, finding claims with mineral deposits that can be cost-effectively mined, the costs associated with acquiring such properties and the unavailability of human or equipment resources. The Company cannot provide assurance it will ever generate significant revenue from its operations or realize a profit. The Company expects to continue to incur operating losses during the next 12 months.

 

9
 

 

Effects of COVID-19 Outbreak

 

In March of 2020, the World Health Organization declared an outbreak of COVID-19 Global pandemic. The COVID-19 has impacted vast array of businesses through the restrictions put in place by most governments internationally, including the USA, Canadian and Chilean governments, as well as provincial and municipal governments, regarding travel, business operations and isolation/quarantine orders. At this time, it is unknown to what extent the impact of the COVID-19 outbreak may have on the Company as this will depend on future developments that are highly uncertain and that cannot be predicted with confidence. These uncertainties arise from the inability to predict the ultimate geographic spread of the disease, and the duration of the outbreak, including the duration of travel restrictions, business closures or disruptions, and quarantine/isolation measures that are currently, or may be put, in place worlds-wide to fight the virus. While the extent of the impact is unknown, the COVID-19 outbreak may hinder the Company’s ability to raise financing for exploration or operating costs due to uncertain capital markets, supply chain disruptions, increased government regulations and other unanticipated factors, all of which may also negatively impact the Company’s business and financial condition.

 

Debt Owing to Related Parties

 

As of January 31, 2022, the Company owed $57,254 to related parties that were due in the next 12-month period for the services and reimbursable expenses they have provided; in addition, the Company owed its related parties $1,715,016 on account of long-term notes payable and for services provided, which are payable on or after January 31, 2023 (as amended). The Company does not have the cash resources to pay the long-term debt; therefore it may decide to partially pay these individuals by issuing shares of the Company’s common stock to them. Because of the low market value of the Company’s common stock, the issuance of shares will result in substantial dilution to the percentage of the outstanding common stock owned by current shareholders.

 

Financing Risks

 

The Company has no history of significant earnings and, due to the nature of its business, there can be no assurance that the Company will be profitable. The Company has paid no dividends on its shares since incorporation and does not anticipate doing so in the foreseeable future. The only present source of funds available to the Company is through the sale of its securities. Even if the results of any future exploration are encouraging, the Company may not have sufficient funds to conduct the further exploration that may be necessary to determine whether or not a commercially mineable deposit exists on the Properties. While the Company may generate additional working capital through equity offerings or through the sale or possible syndication of the Properties, there is no assurance that any such funds will be available. If available, future equity financing may result in substantial dilution to shareholders

 

Speculative Nature of Mineral Exploration

 

Resource exploration is a speculative business, characterized by a number of significant risks including, among other things, unprofitable efforts resulting not only from the failure to discover mineral deposits but also from finding mineral deposits that, though present, are insufficient in quantity and quality to return a profit from production. The marketability of minerals acquired or discovered by the Company may be affected by numerous factors which are beyond the control of the Company and which cannot be accurately predicted, such as market fluctuations, the proximity and capacity of milling facilities, mineral markets and processing equipment and such other factors as government regulations, including regulations relating to royalties, allowable production, importing and exporting of minerals and environmental protection, the combination of which factors may result in the Company not receiving an adequate return of investment capital.

 

There is no assurance that the Company’s mineral exploration and development activities will result in any discoveries of commercial bodies of ore. The long-term profitability of the Company’s operations will, in part, be directly related to the costs and success of its exploration programs, which may be affected by a number of factors. Substantial expenditures are required to establish reserves through drilling and to develop the mining and processing facilities and infrastructure at any site chosen for mining. Although substantial benefits may be derived from the discovery of a major mineralized deposit, no assurance can be given that minerals will be discovered in sufficient quantities to justify commercial operations or that funds required for development can be obtained on a timely basis.

 

10
 

 

No Known Mineral Reserves

 

It is unknown whether the Properties contain viable mineral reserves. If the Company does not find a viable mineral reserve, or if it cannot exploit the mineral reserve, either because the Company does not have the money to do it or because it will not be economically feasible to do so, the Company may have to cease operations and you may lose your investment. Mineral exploration is a highly speculative endeavor. It involves many risks and is often non-productive. Even if mineral reserves are discovered on the Properties, the Company’s production capabilities will be subject to further risks and uncertainties including:

 

Costs of bringing the property into production including exploration work, preparation of production feasibility studies, and construction of production facilities, all of which the Company has not budgeted for;
Availability and costs of financing;
Ongoing costs of production; and
Environmental compliance regulations and restraints.

 

Market Factors May Affect Ability to Market Any Minerals Found

 

Even if the Company discovers minerals that can be extracted in a cost-effective manner, it may not be able to find a ready market for its minerals. Many factors beyond the Company’s control affect the marketability of minerals. These factors include market fluctuations, the proximity and capacity of natural resource markets and processing equipment, government regulations, including regulations relating to prices, taxes, royalties, land tenure, land use, importing and exporting minerals and environmental protection. The Company cannot accurately predict the effect of these factors, but any combination of these factors could result in an inadequate return on invested capital.

 

Mineral Exploration is Hazardous

 

The search for minerals is hazardous. In the course of exploration, development and production of mineral properties, the Company could incur liability or damages as it conducts its business due to the dangers inherent in mineral exploration, including pollution, cave-ins, fires, flooding, earthquakes and other hazards. It is not always possible to fully insure against such risks or against which the Company may elect not to insure. The Company has no insurance for these types of hazards, nor does it expect to obtain such insurance for the foreseeable future. Should such liabilities arise, they could reduce or eliminate any future profitability and result in increasing costs and a decline in the value of the securities of the Company.

 

Government Regulations

 

The mining business is subject to various levels of government control and regulation, which are supplemented and revised from time to time. The Company cannot predict what legislation or revisions might be proposed that could affect its business or when any such proposals, if enacted, might become effective. The Company’s exploration activities are subject to laws and regulations governing worker safety, and, if it explores within the national park that is part of its Farellón property, protection of endangered and other special status species as well as protection of significant archeological remains, if there are any, will likely require compliance with additional laws and regulations. The cost of complying with these regulations has not been burdensome to date, but if the Company mines the Properties and processes more than 5,000 tonnes of ore monthly, it will be required to submit an environmental impact study for review and approval by the federal environmental agency. The Company anticipates that the cost of such a study will be significant and, if the study were to show too great an adverse impact on the environment, the Company might be unable to develop the property or it might have to engage in expensive remedial measures during or after developing the property, which could make production unprofitable. This requirement could materially adversely affect the Company’s business, the results of its operations and its financial condition if it were to proceed to mine a property or process ore on the property. The Company has no immediate or intermediate plans to process ore on any of the Properties.

 

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If the Company does not comply with applicable environmental and health and safety laws and regulations, it could be fined, enjoined from continuing its operations, and suffer other penalties. Although the Company makes every attempt to comply with these laws and regulations, it cannot provide assurance that it has fully complied or will always fully comply with them.

 

Environmental and Safety Regulations and Risks

 

Environmental laws and regulations may affect the operations of the Company. These laws and regulations set various standards regulating certain aspects of health and environmental quality. They provide for penalties and other liabilities for the violation of such standards and establish, in certain circumstances, obligations to rehabilitate current and former facilities and locations where operations are or were conducted. The permission to operate can be withdrawn temporarily where there is evidence of serious breaches of health and safety standards, or even permanently in the case of extreme breaches. Significant liabilities could be imposed on the Company for damages, clean-up costs or penalties in the event of certain discharges into the environment, environmental damage caused by previous owners of acquired properties or noncompliance with environmental laws or regulations. In all major developments, the Company generally relies on recognized designers and development contractors from which the Company will, in the first instance, seek indemnities. The Company minimizes risks by taking steps to ensure compliance with environmental, health and safety laws and regulations and operating to applicable environmental standards. There is a risk that environmental laws and regulations may become more onerous, making the Company’s operations more expensive.

 

Competition

 

The mining industry is intensely competitive in all its phases. The Company competes for the acquisition of mineral properties, claims, leases and other mineral interests as well as for the recruitment and retention of qualified employees with many companies possessing greater financial resources and technical facilities than the Company. The competition in the mineral exploration and development business could have an adverse effect on the Company’s ability to acquire suitable properties or prospects for mineral exploration in the future.

 

Stress in the Global Economy

 

Negative fluctuations in a state of global economy may cause general tightening in the credit markets, lower levels of liquidity, increases in the rates of default and bankruptcy, and lower business spending, all of which may have a negative effect on the Company’s business, results of operations, financial condition and liquidity. The Company’s suppliers may not be able to supply it with needed raw materials on a timely basis, may increase prices or go out of business, which could result in the inability of the Company to carry out its planned exploration programs. Furthermore, it may become difficult to locate other mineral exploration companies with available funds willing to engage in risky ventures such as the exploration of the Properties.

 

Such conditions may make it very difficult to forecast operating results, make business decisions and identify and address material business risks. As a result, the Company’s operating results, financial condition and business could be adversely affected.

 

The Company conducts operations in a foreign jurisdiction and is subject to certain risks that may limit or disrupt its business operations.

 

The Company’s head office is in Canada and its mining operations are in Chile. Mining investments are subject to the risks normally associated with the conduct of any business in foreign countries including uncertain political and economic environments; wars, terrorism and civil disturbances; changes in laws or policies, including those relating to imports, exports, duties and currency; cancellation or renegotiation of contracts; royalty and tax increases or other claims by government entities, including retroactive claims; risk of expropriation and nationalization; delays in obtaining or the inability to obtain or maintain necessary governmental permits; currency fluctuations; restrictions on the ability of local operating companies to sell gold, copper or other minerals offshore for US dollars, and on the ability of such companies to hold US dollars or other foreign currencies in offshore bank accounts; import and export regulations, including restrictions on the export of gold, copper or other minerals; limitations on the repatriation of earnings; and increased financing costs.

 

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These risks could limit or disrupt the Company’s exploration programs, cause it to lose its interests in its mineral claims, restrict the movement of funds, cause it to spend more than it expected, deprive it of contract rights or result in its operations being nationalized or expropriated without fair compensation, and could materially adversely affect the Company’s financial position or the results of its operations. If a dispute arises from the Company’s activities in Chile, the Company could be subject to the exclusive jurisdiction of courts outside North America, which could adversely affect the outcome of the dispute.

 

While the Company takes steps it believes are necessary to maintain legal ownership of its claims, title to mineral claims may be invalidated for a number of reasons, including errors in the transfer history or acquisition of a claim the Company believed, after appropriate due diligence investigation, to be valid, but in fact, wasn’t. If ownership of the Company’s claims was ultimately determined to be invalid, the Company’s business and prospects would likely be materially and adversely affected.

 

The Company’s ability to realize a return on its investment in mineral claims depends upon whether it maintains the legal ownership of the claims. Title to mineral claims involves risks inherent in the process of determining the validity of claims and the ambiguous transfer history characteristic of many mineral claims. The Company takes a number of steps to protect the legal ownership of its claims, including having its contracts and deeds notarized, recording these documents with the registry of mines and publishing them in the mining bulletin. The Company also reviews the mining bulletin regularly to determine whether other parties have staked claims over its ground. However, none of these steps guarantees that another party could not challenge the Company’s right to a claim. Any such challenge could be costly to defend and, if the Company lost its claim, its business and prospects would likely be materially and adversely affected.

 

No Anticipation of Payment of Dividends

 

A dividend has never been declared or paid in cash on the Common Shares. The Company does not anticipate such a declaration or payment for the foreseeable future. The Company intends to retain any earnings to develop, carry on, and expand its business.

 

Price Volatility of Publicly Traded Securities

 

In recent years, the securities markets in Canada have experienced a high level of price and volume volatility, and the market prices of securities of many companies have experienced wide fluctuations in price which have not necessarily been related to the operating performance, underlying asset values or prospects of such companies. There can be no assurance that continual fluctuations in price will not occur. It may be anticipated that any quoted market for the Common Shares will be subject to market trends generally, notwithstanding any potential success of the Company in creating revenues, cash flows or earnings. The value of Common Shares will be affected by such volatility.

 

Fluctuating Mineral Prices and Currency Risk

 

The Company’s revenues, if any, are expected to be in large part derived from the extraction and sale of precious and base minerals and metals. Factors beyond the control of the Company may affect the marketability of metals discovered, if any. Metal prices have fluctuated widely, particularly in recent years. Consequently, the economic viability of any of the Company’s exploration projects cannot be accurately predicted and may be adversely affected by fluctuations in mineral prices.

 

The Company sometimes holds a significant portion of its cash in US dollars. Currency exchange rate fluctuations can result in conversion gains and losses and diminish the value of its US dollars. If the US dollar declined significantly against the Canadian dollar or the Chilean peso, its US dollar purchasing power in Canadian dollars and Chilean pesos would also significantly decline and that could make it more difficult for the Company to conduct its business operations. The Company has not entered into derivative instruments to offset the impact of foreign exchange fluctuations.

 

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Management

 

The success of the Company is currently largely dependent on the performance of its directors and officers. The loss of the services of any of these persons could have a materially adverse effect on the Company’s business and prospects. There is no assurance the Company can maintain the services of its directors, officers or other qualified personnel required to operate its business.

 

Key Person Insurance

 

The Company does not maintain key person insurance on any of its directors or officers, and as result the Company would bear the full loss and expense of hiring and replacing any director or officer in the event the loss of any such persons by their resignation, retirement, incapacity, or death, as well as any loss of business opportunity or other costs suffered by the Company from such loss of any director or officer.

 

Difficulty for United States Investors to Effect Services of Process Against the Company.

 

The Company is incorporated under the laws of the Province of British Columbia, Canada. Consequently, it will be difficult for United States investors to affect service of process in the United States upon the directors or officers of the Company, or to realize in the United States upon judgments of United States courts predicated upon civil liabilities under the Exchange Act. The majority of the Company’s directors and officers are residents of Canada and all of the Company’s material assets are located outside of the United States. A judgment of a United States court predicated solely upon such civil liabilities would probably be enforceable in Canada by a Canadian court if the United States court in which the judgment was obtained had jurisdiction, as determined by the Canadian court, in the matter. There is substantial doubt whether an original action could be brought successfully in Canada against any of such persons or the Company predicated solely upon such civil liabilities.

 

Conflicts of Interest

 

Some of the directors and officers are engaged and will continue to be engaged in the search for additional business opportunities on behalf of other corporations, and situations may arise where these directors and officers will be in direct competition with the Company. Conflicts, if any, will be dealt with in accordance with the relevant provisions of the Business Corporations Act (British Columbia). Some of the directors and officers of the Company are or may become directors or officers of other companies engaged in other business ventures. In order to avoid the possible conflict of interest which may arise between the directors’ duties to the Company and their duties to the other companies on whose boards they serve, the directors and officers of the Company have agreed to the following:

 

Participation in other business ventures offered to the directors will be allocated between the various companies and on the basis of prudent business judgment and the relative financial abilities and needs of the companies to participate;
No commissions or other extraordinary consideration will be paid to such directors and officers; and
Business opportunities formulated by or through other companies in which the directors and officers are involved will not be offered to the Company except on the same or better terms than the basis on which they are offered to third party participants.

 

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“Penny Stock” Rules May Make Buying or Selling Our Common Stock Difficult, and Severely Limit its Marketability and Liquidity

 

Because the Company’s securities are considered a penny stock, shareholders will be more limited in their ability to sell their shares. The SEC has adopted rules that regulate broker-dealer practices in connection with transactions in penny stocks. Penny stocks are generally equity securities with a price of less than USD$5.00, other than securities registered on certain national securities exchanges or quoted on the NASDAQ system, provided that current price and volume information with respect to transactions in such securities is provided by the exchange or quotation system. Because the Company’s securities constitute “penny stocks” within the meaning of the rules, the rules apply to the Company and to its securities. The rules may further affect the ability of owners of shares to sell the Company’s securities in any market that might develop for them. As long as the trading price of the Common Shares is less than USD$5.00 per share, the Common Shares will be subject to Rule 15g-9 under the Exchange Act. The penny stock rules require a broker-dealer, prior to a transaction in a penny stock, to deliver a standardized risk disclosure document prepared by the SEC, that:

 

Contains a description of the nature and level of risk in the market for penny stocks in both public offerings and secondary trading;
Contains a description of the broker’s or dealer’s duties to the customer and of the rights and remedies available to the customer with respect to a violation to such duties or other requirements of securities laws;
Contains a brief, clear, narrative description of a dealer market, including bid and ask prices for penny stocks and the significance of the spread between the bid and ask price;
Contains a toll-free telephone number for inquiries on disciplinary actions;
Defines significant terms in the disclosure document or in the conduct of trading in penny stocks; and
Contains such other information and is in such form, including language, type, size and format, as the SEC shall require by rule or regulation.

 

The broker-dealer also must provide, prior to effecting any transaction in a penny stock, the customer with: (a) bid and offer quotations for the penny stock; (b) the compensation of the broker-dealer and its salesperson in the transaction; (c) the number of shares to which such bid and ask prices apply, or other comparable information relating to the depth and liquidity of the market for such shares; and (d) a monthly account statement showing the market value of each penny stock held in the customer’s account. In addition, the penny stock rules require that prior to a transaction in a penny stock not otherwise exempt from those rules; the broker-dealer must make a special written determination that the penny stock is a suitable investment for the purchaser and receive the purchaser’s written acknowledgment of the receipt of a risk disclosure statement, a written agreement to transactions involving penny stocks, and a signed and dated copy of a written suitably statement. These disclosure requirements may have the effect of reducing the trading activity in the secondary market for the Common Shares.

 

Tax Issues

 

Income tax consequences in relation to the Common Shares will vary according to circumstances of each investor. Prospective investors should seek independent advice from their own tax and legal advisers prior to investing in Common Shares of the Company.

 

Other Risks and Uncertainties

 

Although the Company has tried to identify all significant risks, it may not have identified all risks. There may be other risks.

 

The Company has sought to identify what it believes to be the most significant risks to its business, but it cannot predict whether, or to what extent, any of such risks may be realized nor can it guarantee that it has identified all possible risks that might arise. Investors should carefully consider all of such risk factors before making an investment decision with respect to the Company’s Common Shares.

 

Item 4Information on the Company

 

A.History and Development of the Company

 

Company Name

 

The legal and commercial name of the company is Red Metal Resources Ltd.

 

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Principal Office

 

The Company’s head office is located at 1130 West Pender Street, Suite 820, Vancouver, British Columbia, V6E 4A4. Its registered office address is 595 Burrard Street, Suite 700, Vancouver, British Columbia, V7X 1S8.We do not have an agent in the United States. The Company’s mailing address is 278 Bay Street, Suite 102, Thunder Bay, Ontario, P7B 102

 

Corporate Information and Important Events

 

Red Metal Resources Ltd. was incorporated under the Nevada Business Corporations Act on January 10, 2005, as Red Lake Exploration, Inc. On August 27, 2008, the name of the Company was changed to Red Metal Resources Ltd. On February 10, 2021, the Company changed its corporate jurisdiction from the State of Nevada to the Province of British Columbia by means of a process called a “conversion” under the Nevada Revised Statutes and a “continuation” under the Business Corporations Act (British Columbia). Upon the Company’s continuation to British Columbia, the Articles of Incorporation and Bylaws of the Company, under the Nevada Revised Statutes, were replaced with the Articles of the Company, under the Business Corporations Act (British Columbia). The authorized capital of the Company was amended to an unlimited number of common shares without par value.

 

On November 18, 2021, the Company filed a final non-offering prospectus with the B.C. Securities Commission and became a reporting issuer in the province of British Columbia. The common shares of the Company were approved for listing on the Canadian Securities Exchange (the “CSE”) and began trading under the symbol “RMES” as of market open on November 25, 2021, and the Company consequently became a reporting issuer in the province of Ontario. The Company’s common shares continue to trade on the OTC Link alternative trading system on the OTC PINK marketplace under the symbol “RMESF”.

 

On August 21, 2007, the Company formed Minera Polymet Limitada (“Polymet”) as a limited liability company, under the laws of the Republic of Chile. On September 28, 2015, the Company changed Polymet’s incorporation from Limited Liability Company to a Closed Stock Corporation (“SpA”). As of the date of this Form 20-F the Company owns 100% of Polymet, which holds its Chilean mineral property interests.

 

The Company is engaged in the business of mineral exploration in Chile with the objective to explore and, if warranted, develop mineral properties. All of the Company’s mineral concessions are located in the Candelaria iron oxide copper-gold (IOCG) belt of the coastal cordillera, in the Carrizal Alto Mining District, III Region of Atacama, Chile. The Company has three active copper-gold projects on two properties, namely the Farellón and Perth Projects both located on the Carrizal Property, and the Mateo Project located on the Mateo Property. In addition to holding these active properties, as an exploration company, the Company periodically stakes, purchases or options claims to allow time and access to fully consider the geological potential of claims.

 

The Company’s flagship project, the Farellón Project, is an early-stage exploration property consisting of eight mining concessions totaling 1,234 hectares.

 

Consistent with the Company’ historical practices, the Company’s management continues to monitor its costs in Chile by reviewing the Company’s mineral claims to determine whether they possess the geological indicators to economically justify the capital to maintain or explore them. As at the time of this Form 20-F, Polymet has six employees and engages independent consultants on as needed basis. Most of the Company’s support - such as vehicles, office, and equipment - is supplied under short-term contracts. The only long-term commitments that the Company has are for royalty payments on four of its mineral concessions - Farellón Alto 1 - 8, Quina 1 - 56, Exeter 1 - 54, and Che. These royalties are payable once exploitation begins. The Company is also required to pay property taxes that are due annually on all the concessions that are included in its properties.

 

The cost and timing of all planned exploration programs are subject to the availability of qualified mining personnel, such as consulting geologists, geo-technicians and drillers, and drilling equipment. Although Chile has a well-trained and qualified mining workforce from which to draw and few early-stage companies such as Red Metal are competing for the available resources, if the Company is unable to find the personnel and equipment needed at the prices that were budgeted for the programs, the Company might have to revise or postpone its exploration plans.

 

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Capital Expenditures

 

Due to a lack of operating capital, during the fiscal years ended January 31, 2021 and 2020, the Company conducted no material exploratory operations on any of its mineral properties; and it also did not increase its land holdings in Chile.

 

During the year ended January 31, 2022, the Company raised sufficient capital to continue exploration work on its Farellón Property, In the short to medium term, based on the positive results from multiple past exploration programs on the Farellón Project, the Company planned to carry out a two-phase drill program. The first phase of the drill program commenced on January 25, 2022, and was completed in the early March of 2022; it consisted of a drilling that tested the primary mineralization at depth that has, thus far, only been intersected in a few drill holes, and determine the potential of the cobalt mineralization in the sulfide zone.

 

The highlights of the first phase included the following:

 

  First hole on new zone intercepted six meters of vein with strong visible copper sulphides; further 1.5 km of untested strike length;
  All holes have intercepted visible copper sulphide mineralization and alteration associated with IOCG deposits; and
  Diamond drill core provided valuable alteration and structural information not seen in previous RC drilling.

 

As of the date of this Annual Report on Form 20-F sampling is ongoing for drillholes and no visual estimates of grade have been made.

 

During the year ended January 31, 2022, the Company spent a total of $232,569 on the Farellón Property Project.

 

If the first phase continues to return positive results, a second phase drilling program would be conducted in order to complete an initial mineral resource estimate.

 

Takeover Offers

 

The Company is not aware of any indication of any public takeover offers by third parties in respect of our common shares during our last and current financial years.

 

The U.S. Securities and Exchange Commission (SEC) maintains an internet site that contains reports, proxy and information statements, and other information regarding issuers that file electronically with the SEC. The address of that site is http://www.sec.gov.

 

Additional information can be found at the Company’s website at http://www.redmetalresources.com/

 

B.Business Overview

 

Nature of Operations and Principal Activities

 

The Company is engaged in the business of mineral exploration in Chile with the objective to explore and, if warranted, develop mineral properties. All of the Company’s mineral claims are located in the Candelaria iron oxide copper-gold (IOCG) belt of the coastal cordillera in the Carrizal Alto Mining District, III Region of Atacama, Chile. The Company has three active copper-gold projects on two properties, namely the Farellón and Perth Projects both located on the Carrizal Property, and the Mateo Project located on the Mateo Property. In addition to holding these active properties, as an exploration company, the Company periodically stakes, purchases or option claims to allow time and access to fully consider the geological potential of claims.

 

The Company’s flagship project, the Farellón Project, is a mid-stage exploration project consisting of eight exploitation concessions totaling 1,234 hectares.

 

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The Company acquired the initial mining claim for the Farellón Project pursuant to an assignment agreement between Polymet and Minera Farellón Limitada (“Minera Farellón”) dated September 25, 2007, and amended on November 20, 2007. Under the terms of the assignment agreement, Minera Farellón agreed to assign to Polymet its option to buy the Farellón 1 Al 8 mining concession. Polymet acquired the option on April 25, 2008, and concurrently assumed all of Minera Farellón’s rights and obligations under the Farellón option agreement. Polymet exercised the option and bought the property from the vendor on April 25, 2008. The patented mining concessions are registered in the name of and owned 100% by Polymet.

 

On September 17, 2008, the Company acquired the Cecil 1 - 49, Cecil 1 - 40 and Burghley 1 - 60 claims for an aggregate purchase price of $27,676. On December 1, 2009, the Company initiated the manifestacion process by applying to convert the Cecil 1 - 40 and Burghley 1 - 60 exploration (pedimento) claims to mining (mensura) claims. In January 2013, the Company abandoned the manifestacion process for the Cecil 1-40 and Burghley 1-60 claims as the Company discovered that the most prospective ground, as outlined in the Company’s prospecting and mapping program completed in April 2012, was covered by several mensuras underlying both claims.

 

On August 21, 2012, the Company acquired four mineral claims - Azucar 6-25, Kahuna 1-40, Stamford 61-101, and Teresita - through the government auction for a total price of $19,784.

 

On December 15, 2014, the Company entered into an option agreement with David Marcus Mitchell to earn 100% interest in a Quina 1-56 clam (the “Quina Claim”). The Quina Claim covers 251 hectares and is centered at 310,063 east and 6,890,435 south UTM PSAD56 Zone 19 and is contiguous to the Farellón Property. Acquisition of the Quina Claim added approximately 2 kilometers of strike length of the Farellón Veins. In order to acquire the 100% interest in the Quina Claim the Company paid a total of $150,000 in combined stock and cash payments and completed the acquisition on December 15, 2018.

 

On June 3, 2015, the Company entered into an option agreement, made effective on June 15, 2015, with Minera Stamford S.A., to earn 100% interest in a mining claim known as “Exeter 1-54” (the “Exeter claim”). The Exeter claim totals 235 hectares and is contiguous to the Farellón Property, which is located in the Carrizal Alto mining district, located approximately 75 kilometers northwest of the city of Vallenar, 150 kilometers south of Copiapo and 20 kilometers west of the Pan American Highway. In order to acquire 100% interest in the Exeter claim, the Company paid a total of $150,000 and completed the transaction on May 12, 2019.

 

These properties form substantial land holdings in a historical mining district, which was a prolific past producer, shut down due to economic conditions, rather than exhaustion of deposits. The Company’s Carrizal Property, adjacent and contiguous to the Carrizal Alto Mine, has undergone only limited modern exploration, which has so far demonstrated the potential of the property to host a mineralized deposit.

 

The Company’s Perth and Mateo Projects are both early-stage exploration projects. The Perth Project is composed of 13 mining concessions covering 2,044 hectares and the Mateo Project is composed of 5 mineral concessions covering 182 hectares. Both projects are 100% owned by Polymet.

 

To date the Company has not determined whether its claims contain mineral reserves that are economically recoverable and it has not produced revenues from its principal business.

 

Principal Market and Revenues

 

The Company does not currently have any market, as it has not yet identified any mineral resource on any of the Company’s properties that is of a commercially exploitable quantity. If the Company’s succeeds in identifying a mineral resource in commercially exploitable quantities, its principal markets would consist of metals refineries and base metal traders and dealers. The Company’s first customer likely will be ENAMI, the Chilean national mining company, which refines and smelts copper from the ore that it buys from Chile’s small- and medium-scale miners. ENAMI is located in Vallenar. The Company could also sell its ore to the Dos Amigos heap leach facility located approximately fifty kilometers south of Vallenar in Domeyko.

 

To date the Company has not generated any revenues from any of its properties.

 

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Seasonality of our Business

 

The Company’s mineral exploration activities are not subject to seasonal variation due to the year-round favorable weather conditions in Chile.

 

Sources and Availability of Raw Materials

 

The raw materials for our exploration programs include camp equipment, hand exploration tools, sample bags, first aid supplies, groceries and propane. All of these types of materials are readily available from a variety of local suppliers.

 

Marketing Channels

 

We do not currently have any market, as we have not yet identified any mineral resource on any of our properties that is of a commercially exploitable quantity, and therefore do not currently engage in marketing activities.

 

Patents and Licenses; Industrial, Commercial and Financial Contracts; and New Manufacturing Processes

 

In conducting our business operations, we are not dependent on any patented or license processes, technology, industrial, commercial or financial contract or new manufacturing processes.

 

Competitive Conditions

 

The mineral exploration business is an extremely competitive industry. We are competing with many other exploration companies looking for minerals. We are one of the smallest exploration companies and a very small participant in the mineral exploration business. Being a junior mineral exploration company, we compete with other similar companies for financing and joint venture partners, and for resources such as professional geologists, camp staff, helicopters and mineral exploration contractors and supplies. We do not represent a competitive presence in the industry.

 

Governmental Regulations

 

The mining business is subject to various levels of government control and regulation, which are supplemented and revised from time to time. The Company cannot predict what legislation or revisions might be proposed that could affect its business or when any such proposals, if enacted, might become effective. The Company’s exploration activities are subject to laws and regulations governing worker safety, and, if it explores within the national park that is part of its Farellón property, protection of endangered and other special status species as well as protection of significant archeological remains, if there are any, will likely require compliance with additional laws and regulations. The cost of complying with these regulations has not been burdensome to date, but if the Company mines the Properties and processes more than 5,000 tonnes of ore monthly, it will be required to submit an environmental impact study for review and approval by the federal environmental agency. The Company anticipates that the cost of such a study will be significant and, if the study were to show too great an adverse impact on the environment, the Company might be unable to develop the property or it might have to engage in expensive remedial measures during or after developing the property, which could make production unprofitable. This requirement could materially adversely affect the Company’s business, the results of its operations and its financial condition if it were to proceed to mine a property or process ore on the property. The Company has no immediate or intermediate plans to process ore on any of the Properties.

 

If the Company does not comply with applicable environmental and health and safety laws and regulations, it could be fined, enjoined from continuing its operations, and suffer other penalties. Although the Company makes every attempt to comply with these laws and regulations, it cannot provide assurance that it has fully complied or will always fully comply with them.

 

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Environmental and Safety Regulations and Risks

 

Environmental laws and regulations may affect the operations of the Company. These laws and regulations set various standards regulating certain aspects of health and environmental quality. They provide for penalties and other liabilities for the violation of such standards and establish, in certain circumstances, obligations to rehabilitate current and former facilities and locations where operations are or were conducted. The permission to operate can be withdrawn temporarily where there is evidence of serious breaches of health and safety standards, or even permanently in the case of extreme breaches. Significant liabilities could be imposed on the Company for damages, clean-up costs or penalties in the event of certain discharges into the environment, environmental damage caused by previous owners of acquired properties or noncompliance with environmental laws or regulations. In all major developments, the Company generally relies on recognized designers and development contractors from which the Company will, in the first instance, seek indemnities. The Company minimizes risks by taking steps to ensure compliance with environmental, health and safety laws and regulations and operating to applicable environmental standards. There is a risk that environmental laws and regulations may become more onerous, making the Company’s operations more expensive.

 

C.Organizational Structure

 

The Company owns 100% of Minera Polymet SpA (“Polymet”), a corporation organized under the laws of the Republic of Chile on August 21, 2007. Polymet holds the Company’s Chilean mineral property interests and, to comply with Chilean legal requirements, Polymet has appointed a legal representative in Chile. Polymet’s head office is located in Vallenar, III Region of Atacama, Chile.

 

D.Property, Plant and Equipment

 

The Company’s executive office is located at 1130 West Pender Street, Suite 820, Vancouver, British Columbia V6E 4A4, Canada. The Company rents this location from its CFO at no cost. This space accommodates our finance and administrative department.

 

The Company’s secondary office is located at 278 Bay Street, Suite 102, Thunder Bay, ON P7B 1R8. The Company rents this location from Fladgate Exploration Consulting Corporation (“Fladgate”), a company owned by Ms. Caitlin Jeffs and Mr. Michael Thompson, who each hold 33% of Fladgate. During the nine-month period ended October 31, 2021, the Company paid $1,000 per month for this office. At October 31, 2021, Fladgate agreed to forgive the accrued office rent fees, and as of the date of this Annual Report on Form 20-F, the Thunder Bay office is provided to the Company free of charge. This space acts as the Company’s mailing address, and accommodates our CEO and VP of Exploration, as well as provides geological support to the Chilean operations.

 

Our Chilean office is located in Vallenar, III Region of Atacama, Chile. This office is provided to the Company free of charge by Mr. Jeffs, the Company’s major shareholder and father of our CEO, Caitlin Jeffs.

 

The Company believes that the existing space is adequate for the Company’s current needs. Should the Company require additional space, the Company believes that such space can be secured on commercially reasonable terms.

 

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Overview of Mineral Properties

 

Active Properties

 

Through a number of transactions since 2007, the Company has assembled its active mineral properties identified and further detailed in Figure 1 and Table 1, respectively, below as the Farellón Property, the Perth Property, and the Mateo Property:

 

 

 

Figure 1: Location and access to active properties (accessible by road from Vallenar)

 

21
 

 

Table 1 - Active Properties

 

    Percentage,   Hectares
Property   type of claim   Gross area   Net area(a)
Farellón            
Farellón Alto 1 – 8   100%, mensura   66    
Quina 1 – 56   100%, mensura   251    
Exeter 1 – 54   100%, mensura   235    
Cecil 1 – 49   100%, mensura   228    
Teresita   100%, mensura   1    
Azucar 6 – 25   100%, mensura   88    
Stamford 61 – 101   100%, mensura   165    
Kahuna 1 – 40   100%, mensura   200    
        1,234   1,234
             
Perth            
Perth 1-36   100%, mensura   109    
Rey Arturo 1-30   100%, mensura   276    
Lancelot 1 1-27   100%, mensura   260    
Galahad IA 1 44   100%, mensura   217    
Camelot 1 53   100%, mensura   227    
Percival 4 1 60   100%, mensura   300    
Tristan II A 1 55   100%, mensura   261    
Galahad IB 1 3   100%, mensura   10    
Tristan II B 1 4   100%, mensura   7    
Merlin IB 1 10   100%, mensura   38    
Merlin A 1 48   100%, mensura   220    
Lancelot II 1 23   100%, mensura   115    
Galahad IC   100%, mensura   4    
        2,044   2,044
Mateo            
Margarita   100%, mensura   56    
Che 1 and Che 2   100%, mensura   76    
Irene and Irene II   100%, mensura   60    
        192    
Overlapped claims(a)       (10)   182
            3,460

 

(a) Irene and Irene II overlap each other; the net area of both claims is 50 hectares.

 

Carrizal Property – Farellón And Perth Projects

 

Technical Report

 

The information in this Annual Report on Form 20-F with respect to the Carrizal Property is derived from the report titled “Independent Technical Report on the Carrizal Cu-Co-Au Property” dated August 31, 2021 with an effective date of August 1, 2021, written by Scott Jobin-Bevans, Ph.D., PMP, P. Geo of Caracle Creek International Consulting Inc. (the “Technical Report”). The Technical Report has been prepared in accordance with the requirements of National Instrument 43-101 – Standards of Disclosure for Mineral Projects (“NI 43-101”). Mr. Jobin-Bevans is an independent “Qualified Person” for purposes of NI 43-101. The full text of the Technical Report is available for review at the mailing address of the Company at 278 Bay Street, Suite 102, Thunder Bay, Ontario, P7B 102, and may also be accessed online under the Company’s SEDAR profile at www.sedar.com and on the Company’s website http://www.redmetalresources.com.

 

22
 

 

Property Description and Location

 

The Carrizal Property is located approximately 700 km north of Chile’s capital city of Santiago, in Region III, referred to as the “Region de Atacama”. The Carrizal Property lies within the Carrizal Alto Mining District, straddling the border between Huasco and Copiapo provinces, approximately 75 km northwest of the City of Vallenar, 150 km south of Copiapo, and 20 km west of the Pan-American Highway (Figure 1). The centre of the Carrizal Property is situated at coordinates 308750 mE and 6895000 mN (PSAD56 UTM Zone 19, Southern Hemisphere).

 

The Carrizal Property has historically been subdivided into two separate projects, namely the Perth and Farellón project areas, representing roughly the northern and southern halves of the Carrizal Property, respectively. The Carrizal Property consists of 21 exploitation concessions (‘mensuras’). The Carrizal Property covers a total area of 3,278 hectares (2,044 ha in the Perth Project and 1,234 ha in the Farellón Project) (Figures 2, 3 and 4).

 

 

  

Figure 2 - Location of the Farellón and Perth projects claim blocks of the Carrizal Property, Region III, Region de Atacama, northern Chile

 

23
 

  

 

 

Figure 3 - Claims in the southern portion of the Carrizal Property referred to as the Farellón Project area

 

 

 

Figure 4 - Claims in the northern portion of the Carrizal Property referred to as the Perth Project area

 

24
 

 

Accessibility

 

The Carrizal Property is readily accessible from the City of Vallenar, Chile, via both paved and well-maintained dirt roads. Access is primarily gained by taking the Pan-American highway (Ruta 5) north from Vallenar to the Carrizal turn-off (approximately 20 km north). From the turn-off, a well-maintained dirt road runs to the CMP Cerro Colorado iron mine and continues to Canto del Agua and towards Carrizal Alto. From this route, a dirt side road then leads directly to the Carrizal Property (Figure 1).

 

Title/Interest

 

The Company owns all of the concessions in the Carrizal Property, through right of title.

 

Surface Rights and Legal Access

 

The surface rights of the Carrizal Property are owned by the Chilean government; however, if the Carrizal Property is developed and mined at a later date, the surface rights will need to be secured as part of the permitting process. Surface rights are rented to mines for the life of the mine by the Chilean government and claim holders have legal unimpeded access to their pedimentos and mensuras.

 

Other Land Tenure Agreements

 

There are pre-existing Net Smelter Return Royalties (“NSR”) on the properties as outlined in Table 2 below and there are no other known land tenure agreements regarding the Carrizal Property. To date, only the existing mensuras and mensuras that are in progress have been surveyed by the Chilean government. The remaining concessions which are exploration pedimentos do not require a survey until an application has been made to transfer them to mensuras.

 

Table 2 - Pre-existing NSRs on various concessions, Carrizal Property

 

Concession Name   Concession Type   Concession Number   NSR
(%)
  Buy Back
USD$
  NSR2*
(%)
Southern claim block (Farellón)
Farellón Alto 1 - 8   Mensura   033030156-2   1.5*   600,000   1.5
Cecil 1 - 49   Mensura   033030329-8           2.5
Azúcar 6 - 25   Mensura   033030342-5           2.5
Kahuna 1 - 40   Mensura   033030360-3           2.5
Stamford 61 - 101   Mensura   033030334-4           2.5
Teresita   Mensura   033030361-1           2.5
Quina 1 - 56   Mensura   033030398-0   1.5*   1,500,000   1.5
Exeter 1 - 54   Mensura   033030336-0   1.5*   750,000   1.5
Northern claim block (Perth)
Perth 1 - 36   Mensura   033030383-2           2.5
Rey Arturo 1 - 30   Mensura   033030638-6           2.5
Lancelot 1 1 - 27   Mensura   033022832-6           2.5
Galahad IA 1 - 44   Mensura   03201D252-K           2.5
Camelot 1 - 53   Mensura   03201D253-8           2.5
Percival 4 1 - 60   Mensura   03201D256-2           2.5
Tristan II A 1 - 55   Mensura   03201D264-3           2.5
Galahad IB 1 - 3   Mensura   03201D55-4           2.5
Tristan II B 1 - 4   Mensura   03201D251-1           2.5
Merlin IB 1 - 10   Mensura   033030691-2           2.5
Merlin A 1 - 48   Mensura   033030692-0           2.5
Lancelot II 1 - 23   Mensura   033030690-4           2.5
Galahad IC   Mensura   03201D254-6           2.5

 

Pursuant to Mining Royalty Agreements dated July 29, 2020 (“Mining Royalty Agreements’), Polymet offered royalties to each of Richard Jeffs, Caitlin Jeffs and Joao (John) da Costa (each a “Royalty Holder”) for total aggregate consideration of USD$5,000. The Mining Royalty Agreements have not been finalized in accordance with Chilean law in part due to the current COVID restrictions preventing the parties from executing the agreement under applicable Chilean Law. Upon finalization according to Chilean law, any future royalties arising from the sale of mineral and other materials from the mining properties listed in the table below located in Chile (collectively, the “Carrizal Property”) will be payable to each of the Royalty Holders in accordance with the terms of their respective Mining Royalty Agreements. The royalty payments are only payable as soon as Polymet initiates or restarts the operation, exploitation, and consequent sale of mineral and other materials from the Properties.

 

25
 

 

Table 3 – Net Smelter Returns Royalty to be paid (%)

 

Property  

Richard Jeffs,

Major Shareholder(1)

 

Caitlin Jeffs,

CEO and

Director(1)

 

Joao da Costa,

CFO and

Director(1)

  Cecilia Alday   David Mitchell   Minera Stamford S.A.
Farellón Alto 1 - 8 (2)   0.75   0.45   0.30   1.5        
Cecil 1 - 49   1.25   0.75   0.50            
Azúcar 6 - 25   1.25   0.75   0.50            
Kahuna 1 - 40   1.25   0.75   0.50            
Stamford 61 - 101   1.25   0.75   0.50            
Teresita   1.25   0.75   0.50            
Quina 1 - 56 (3)   0.75   0.45   0.30       1.5    
Exeter 1 - 54(4)   0.75   0.45   0.30           1.5
Perth 1 - 36   1.25   0.75   0.50            
Rey Arturo 1 - 30   1.25   0.75   0.50            
Lancelot II 1 - 40   1.25   0.75   0.50            
Lancelot 1 1 - 27   1.25   0.75   0.50            
Merlin IB 1 - 10   1.25   0.75   0.50            
Merlin I A 1 - 48   1.25   0.75   0.50            
Tristan II B 1 - 4   1.25   0.75   0.50            
Galahad IA 1 - 44   1.25   0.75   0.50            
Camelot 1 - 60   1.25   0.75   0.50            
Galahad I C 1 - 60   1.25   0.75   0.50            
Tristan II A 1 - 60   1.25   0.75   0.50            
Galahad I B 1 - 3   1.25   0.75   0.50            
Percival 4 1 - 60   1.25   0.75   0.50            

 

Notes:

 

(1) Each of the NSR’s to Richard Jeffs, Caitlin Jeffs and Joao da Costa will be paid quarterly once commercial exploitation begins and will be paid on gold, silver, copper and cobalt sales. If, within two years, the Company does not commence commercial exploitation of the mineral properties, an annual payment of USD$10,000 per Royalty Holder will be paid. Pursuant to Chilean law, this agreement is not fully complete until registered against the land title in Chile.
(2) Farellón Alto 1 – 8 is subject to a royalty in favor of Cecilia Alday Limitada equal to 1.5% of the net smelter return that Polymet receives from the property to a maximum of USD$600,000. The royalty is payable monthly and is subject to a monthly minimum of USD$1,000 when Red Metal starts selling any minerals it extracts from the property.
(3) Red Metal has the right to buy out the royalty for a one-time payment of USD$1,500,000.
(4) Red Metal has the right to buy out the royalty for a one-time payment of USD$750,000.

 

Mineral Tenure

 

Chile’s current mining and land tenure policies were incorporated into laws in 1982 and amended in 1983. The laws were established to secure the property rights of both domestic and foreign investors to stimulate mining development in Chile. While the state owns all mineral resources, exploration and exploitation of these resources is permitted by acquiring mining concessions which are granted by the courts according to the law.

 

Concessions are defined by UTM coordinates representing the centre-point of the concession and dimensions (in metres) in north-south and east-west directions. There are two kinds of concessions, mining and exploration, and three possible stages of a concession to get from an exploration concession to a mining concession: ‘pedimento’, ‘manifestacion’, and ‘mensura’ (see below for descriptions). An exploration concession (‘pedimento’) can be placed on any area, whereas the survey to establish a permanent exploitation concession (‘mensura’) can only be effected on “free” areas where no other mensuras exist.

 

26
 

 

Pedimento

 

A pedimento is an initial exploration concession with well-defined UTM coordinates delineating the north-south and east-west boundaries. The minimum size of a pedimento is 100 ha and the maximum is 5000 ha, with a maximum length-to-width ratio of 5:1. A pedimento is valid for a maximum period of 2 years. At the end of the 2-year period it can either be reduced in size by at least 50% and renewed for an additional 2 years or, entered into the process to establish a permanent concession by converting it into a manifestacion. New pedimentos are allowed to overlap pre-existing pedimentos, however, the pedimento with the earliest filing date always takes precedence providing the concession holder maintains their concession in accordance with the Mining Code of Chile and the applicable regulations.

 

Manifestacion

 

Before a pedimento expires, or at any stage during its two-year life (including the first day the pedimento is registered), it may be converted to a manifestacion. A manifestacion is valid for 220 days, and then prior to the expiry date, the owner must request an upgrade to a mensura.

 

Mensura

 

Prior to the expiration of a manifestacion, the owner must request a survey (mensura). After acceptance of the Survey Request (‘Solicitud de Mensura’), the owner has approximately 12 months to have the concession surveyed by a government licensed surveyor. The surrounding concession owners may witness the survey, which is subsequently described in a legal format and presented to the National Mining Service of Chile (Sernageomin) for technical review, which includes field inspection and verification. Following the technical approval by Sernageomin, the file returns to a judge of the appropriate jurisdiction, who dictates the constitution of the claim as a mensura (equivalent to a patented claim in Canada). Once constituted, an abstract describing the claim is published in Chile’s official mining bulletin (published weekly), and 30 days later the claim can be inscribed in the appropriate Mining Registry (Conservador de Minas).

 

Once constituted, a mensura is a permanent property right, with no expiration date. As long as the annual fees (‘patentes’) are paid in a timely manner (from March to May of each year), clear title and ownership of the mineral rights is assured in perpetuity. Failure to pay the annual patentes for an extended period can result in the concession being listed for ‘remate’ (auction sale), wherein a third party may acquire a concession for the payment of back taxes owed (plus a penalty payment). In such a case, the claim is included in a list published 30 days prior to the auction and the owner has the possibility of paying the back taxes plus penalty and thus removing the claim from the auction list.

 

Due to the complicated nature of the land tenure system in Chile, Red Metal has engaged a land tenure specialist who sends a monthly report on the status of all claims in the areas we are working in. This report includes a list of any new concessions in our area along and any obligation on our part to notify new concession holders of our existing concessions.

 

Environmental Liabilities

 

There are no known environmental liabilities within the Carrizal Property. The Company has not applied for any environmental permits on the Carrizal Property and has been advised that none of the exploration work completed to date requires an environmental permit. For all exploration work in Chile, any damage done to the land must be repaired.

 

The Llanos de Challe National Park, which was created in July 1994, covers the southern 750 m of the Farellón Alto 1 - 8 concession. According to the Mining Code of Chile, to mine or complete any exploration work within the park boundaries, the Company will be required to get written authorization from the Chilean government.

 

27
 

 

Exploration History

 

Introduction and Regional History

 

Mining has played an important role in Chile’s economy starting in the 16th century with gold, silver and copper being mined from high grade deposits. Copper mining, in particular, has employed a significant portion of the population both directly and indirectly over the last 100 years. Historically, the most significant mineral producing zone in Chile has been the Coastal Cordillera, ranging between 50 and 100 km wide, extending over 2,500 km from Valparaiso in the south, northward to the Peruvian boarder.

 

The Carrizal Alto Mine area is located within this prolific Coastal Cordilleran range, in the Atacama III Region of northern Chile, between Copiapo and Vallenar. Historical records indicate that copper mining commenced at Carrizal Alto in the 1820s and continued on a significant scale mostly by British companies until 1891, when disastrous flooding occurred and mines closed. The historical reports indicate that the larger mines were obtaining good grades over significant widths in the bottom workings at the time of closure. Very little information regarding mining has survived, but there is a small amount of historical data located in the SERNAGEOMIN National Archives in Santiago, Chile. Up until 1891, mining at the Carrizal Alto Mine site produced over 3 million tonnes of Cu ore, grading between 5 and 15% copper (National Archives in Santiago, Chile). There was also a large quantity of direct shipping ore at 12% copper. At one time there was a considerable body of tailings present to support these figures, however this material has been reprocessed and depleted due to the high prices of gold and copper over the last few years.

 

The Carrizal Alto Mine area contains a series of northeast-trending shear structures, including the principal vein systems of ‘Mina Grande’ and ‘Armonia’. Both vein systems have been worked extensively. The Mina Grande shear contains workings that extend for over 2.5 km as a nearly continuous line of pits, collapsed stopes, narrow open cuts and numerous shafts. The Armonia vein system is similar, extending for 1.8 km. Oxidation depths range from 50 to 150 m, and judging from remnant material, many of the veins were probably worked to this depth and then abandoned as sulfide mineralization was reached.

 

In the most productive zone at Mina Grande (which stretches for 1.5 km), the mineralized vein reached 15 m in width and is composed of quartz, sericite, chalcopyrite and pyrite. Amphibole-rich seams occur proximal to the diorite wall rock, which also frequently contains chalcopyrite and pyrite-bearing impregnations and smaller veins. The main producing mine in the Carrizal Alto Mine area was the Veta Principal on the Mina Grande shear, which was mined to a depth of 400 m along a strike of 1.8 km and over a width varying from 2-15 m. The deepest workings reached 600 m. Several slag dumps remain at old sites of local smelters treating the sulfide ores. Carrizal Alto, despite spectacular past production from the Capote, Mina Grande, and Armonia mines, has remained virtually untouched since the brief gold revival of the 1930s.

 

The current Carrizal Property is comprised of two contiguous blocks, namely the Farellón to the south and Perth to the north (Figure 2). Both of these blocks border the historically-productive Carrizal Alto Mine to the east, sharing geological and mineralogical attributes, and for consistency, the historical names have been retained.

 

Farellón Project Area

 

The Farellón block of concessions, which are contiguous with the Carrizal Alto Mine area, was mined on a limited basis in the 1940s. Very little information remains from this time period, except for a few plans of the limited underground mining (SERNAGEOMIN National Archives, Santiago, Chile).

 

In 1963, eight samples were taken from two high grade veins from the accessible workings within the Farellón project area, namely Veta Pique and Veta Naciente. These samples were analysed for copper, gold, silver, and gangue oxides (Table 4). Unfortunately, no units of measure were provided in the 1963 report accompanying the assay grades, although wt% is most likely for copper. In conjunction with historic records from the 1940s, this information was incorporated into a mineral resource estimate (see below).

 

28
 

 

In the 2010 Technical Report by Micon on the Company’s Farellón Property (which corresponds roughly to the current Farellón Project area), the author stated that “no attempt was made to verify the sampling program of 1963, as the workings were not entirely accessible and there is no sample location map upon which to attempt to duplicate the samples” (Lewis, 2010).

 

Table 4 - Grades of Cu, Au, and Ag from Veins of the Farellón Project

 

Sample       Length   Grade
Number   Vein   (m)   Cu     Au   Ag   CaO   FeO   MgO   SiO2
1   Veta Pique   2.5   1.8     0.5   5   47.89   6.54   0.27   1.34
2   Veta Pique   2.45   6.9     1   20   31.14   13.77   0.3   2
3   Veta Pique   3   3     1   10   46.43   5.86   0.26   2.5
4   Veta Pique   1   1.2     0.2   5   31.52   3.49   0.3   25.66
5   Veta Naciente   2   2.4     0.5   5   47.99   5.52   0.32   1.5
6   Veta Naciente   1.8   3     1   5   38.25   6.09   0.23   17.84
7   Veta Pique   1.7   1.7     0.5   3   43.77   4.51   0.28   10
8   Veta Naciente   0.8   1.6     0.5   3   28.8   3.71   0.23   29.54
Total*       1.8   2.1     0.6   5   40.66   5.1   0.27   12.62

 

* The arithmetic average for the total in the table excludes Sample 2.
Derived from the 1963 report in the Sernageomin files, National Archives, Chile.

 

Oliver Resources, an Irish-based company, through its Chilean subsidiary Oliver Resources Chile Ltda., briefly explored the Farellón Property in 1990 with a stream sediment sampling program and sampling of the Farellón Alto and Bajo mine dumps.

 

The Farellón Property was incorporated into a larger land package called the Azucar Project in the 1990s, owned by Minera Stamford S.A. (Minera Stamford), a Chilean exploration company. In a joint venture with Metalsearch, an Australian company, exploration on these concessions included geological mapping, rock chip sampling, soil geochemistry, reverse circulation (RC) drilling and metallurgical sampling. Geological mapping of the Azucar project showed a NE-trending sheared contact 50 to 200 m wide, containing significant consistent mineralization along a 2 km strike length. Minera Stamford collected 152 rock chip and dump samples from prospective areas along the mineralized shear zone, of which 36 samples fell within the boundary of the Farellón Project. Samples were analyzed for gold, copper and cobalt. The highest gold sample within the Farellón Property was 13.50 g/t Au, the highest copper result was 6.15% Cu, and the highest cobalt result was 0.68% Co.

 

A reverse circulation drilling program of 33 holes totaling 6,486 m was completed between 1996 and 1997 targeting the shear zone on the Azucar property by the JV between Minera Stamford and Metalsearch. Twenty-two (22) of these holes were located within the Farellón Project area, representing a total of 3918 m. Drill holes were placed at irregular intervals along the mineralized shear zone, and the holes were sampled at regular 1 m intervals along their entire length. Results of this drill campaign confirmed the consistent presence of mineralization in the shear zone, to a vertical depth of ~200 m. The highest gold concentration was 21.03 g/t Au, the highest copper result was 9.21% Cu, and the highest cobalt result was 0.58% Co (all of these results are over 1 m intervals).

 

29
 

 

Table 5 - Summary of the Minera Stamford-Metalsearch JV Reverse Circulation Drill Hole Statistics for the Farellón Project area

 

    UTM Coordinates            
Hole Number   Easting   Northern   Elevation (m)   Azimuth (°)   Dip (°)   Depth (m)
FAR-96-06   308962.3   6888011   573   110   -62   100
FAR-96-07   308954.2   6888059   560   110   -62   163
FAR-96-09   309131.2   6888706   552   95   -65   242
FAR-96-010   309167.3   6888980   557   112   -75   211
FAR-96-011   309155.5   6888870   565   102   -62   169
FAR-96-013   309092.8   6888659   540   110   -65   257
FAR-96-014   309131.5   6888703   552   90   -90   203
FAR-96-015   309155   6888867   565   90   -90   200
FAR-96-016   309128.3   6888882   565   111   -65   200
FAR-96-017   309165.4   6888979   557   90   -90   200
FAR-96-018   309181   6889026   562   115   -65   51
FAR-96-019   309180   6889026   562   90   -90   200
FAR-96-020   309138.7   6888640   553   140   -65   150
FAR-96-021   309137.9   6888641   553   90   -90   200
FAR-96-022   309086.1   6888591   564   131   -65   150
FAR-96-023   309085.3   6888601   564   90   -90   200
FAR-96-024   309057.6   6888503   544   110   -65   150
FAR-96-025   309056.6   6888503   544   90   -90   172
FAR-96-026   309029.9   6888387   544   140   -65   150
FAR-96-027   309029.3   6888387   544   90   -90   199
FAR-96-028   309337.5   6889279   500   112   -65   150
FAR-96-029   309336.5   6889280   500   90   -90   201
Total                       3,918

 

Table provided by Red Metal Resources Ltd.

 

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Table 6 - Summary of significant intercepts from the 1996-1997 RC Drilling Program by Minera Stamford and Metalsearch within the Farellón Project area

 

    Significant Interval (m)   Assay Results
Drill Hole    From   To   Length   Gold
(g/t)
  Copper
(%)
  Cobalt
(%)
FAR-96-06   49   54   5   0.15   0.73   0.01
FAR-96-07   25   34   9   0.38   1.05   0.02
FAR-96-09   57   84   27   0.51   0.91   0.03
FAR-96-010   31   36   5   1   0.68   0.04
FAR-96-011   20   26   6   0.67   0.46   0.02
FAR-96-013   86   93   7   0.87   1.68   0.04
FAR-96-014   77   83   6   0.66   0.85   0.06
FAR-96-015   59   79   20   0.99   0.98   0.06
  99   109   10   0.18   1.02   0.03
FAR-96-016   24   26   2   0.95   1.57   0.02
  64   70   6   0.73   0.81   0.07
FAR-96-020   14   16   2   0.46   1.85   0.05
  39   43   4   0.75   0.9   0.03
FAR-96-021   22   25   3   4.17   5.29   0.11
FAR-96-022   29   39   10   1.53   1.31   0.04
 FAR-96-022   100   108   8   3.72   2.49   0.06
FAR-96-023   50   53   3   0.48   1.1   0.06
  59   64   5   0.28   0.78   0.03
  132   147   15   0.6   1.42   0.03
FAR-96-024   33   36   3   0.94   2.89   0.06
FAR-96-025   65   85   20   0.97   1.22   0.02
FAR-96-028   55   58   3   0.12   0.52   0.06
FAR-96-029   30   34   4   0.18   1.15   0.07

 

The historic Farellón workings are in metamorphic units within the sheared metamorphic/tonalite contact zone which is about 200 m wide. The workings are large but restricted to the oxide zone and range from 1-20 m wide. A sample of the wall rock and quartz veined metamorphic rocks taken by Minera Stamford returned 3.0% copper, 1.4 g/t gold, 0.08% cobalt, and 1.1% arsenic.

 

The lower Farellón workings are several hundred metres to the south and associated with massive siderite. A sample collected by Minera Stamford of the lode material returned 5.6% copper, 2.4 g/t gold, 0.02% cobalt. A 20-ton trial parcel of material from the Farellón workings in the 1950s is reported to have returned over 1% cobalt.

 

The Company acquired the rights to the Farellón Property on April 25, 2008, upon its Chilean subsidiary exercising the option to buy the property from Minera Farellón. The Company drilled five RC drill holes in 2009, totaling 725 m using a Tramrock Dx40 RC rig. This larger rig necessitated widening existing roads rehabilitating access to old drill pads. The drill program was designed to twin some of the Minera Stamford 1996-1997 drill holes for data verification, as no geological information was recovered from the Minera Stamford drill program and assays were not accompanied by laboratory certificates. One drill hole tested 100 m below the known mineralization, and another hole tested continuity of mineralization between previously drilled sections.

 

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Collar locations and azimuths for the 2009 drilling were surveyed using a total station surveying tool. Each drill hole had 1.5 m of blue PVC piping added to it as a surface pre-collar which was cemented into place to permanently denote the drill hole location. Downhole surveys were completed on all drill holes from the 2009 program and on six drill holes from the 1996-1997 Minera Stamford program (holes 9, 14, 20, 21, 22, and 23). Surveying of all historic drill holes surrounding the current drilling was attempted, but some of the holes were caved and the survey tool was unable to be lowered into the hole.

 

Table 7 - Summary of Red Metal’s 2009 RC Drill Program on the Farellón Project

 

    UTM Coordinates                
Hole Number   Easting   Northern   Elevation (m)   Azimuth (°)   Dip
(°)
  Depth
(m)
  Comments
FAR-09-A   309,086   6,888,591   550   131   -65   125   twinning FAR-96-22
FAR-09-B   309,125   6,888,709   560   95   -65   100   twinning FAR-96-09
FAR-09-C   309,127   6,888,922   555   105   -65   145   testing continuity between sections
FAR-09-D   308,955   6,888,696   539   95   -65   287   testing depth extent of mineralization
FAR-09-E   309,133   6,888,645   551   Vertical   -90   68   twinning FAR-96-21
Total                       725    

 

Table 8 contains the significant intervals calculated from the 2009 RC drill program by the Company. The intervals are reported as core lengths, as the true width of the mineralized zones have not been determined.

 

Table 8 - Summary of significant intercepts from Red Metal’s 2009 RC Drill Program on the Farellón Project

 

DI9:P21rill   Assay Interval (m)   Assay Grade
Hole
Number
      From   To   Core Length   Gold (g/t)   Copper (%)   Cobalt (%)
FAR-09-A       32   37   5   0.59   1.3   0.02
      97   106   9   0.44   1.63   0.04
  including   103   106   3   0.48   2.49   0.07
FAR-09-B       56   96   40   0.27   0.55   0.02
  including   60   63   7   0.46   1.42   0.04
      75   87   12   0.71   1.28   0.03
FAR-09-C       77   82   5   4.16   2.57   0.05
FAR-09-D       95   134   39   0.11   0.58   0.01
  including   95   103   8   0.33   2.02   0.02
FAR-09-E       25   30   5   0.54   1.35   0.02
      65   68   3   0.58   1.46   0.06

 

Results from the 2009 drilling confirmed the general location and tenor of the mineralization determined during the 1996-1997 Minera Stamford drilling program, however, the 2009 program was not able to reproduce the historical gold assays within holes FAR-09-A and FAR-09-E, designed to duplicate historical holes FAR-96-22 and FAR-96-21, respectively. In the case of FAR-09-E, the disparity between the historical 1996-1997 and 2009 assays was also found with respect to copper. All drill holes during the 2009 drilling program intersected oxide facies mineralization with only minor amounts of sulfide (e.g. hole FAR-09-D).

 

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In 2011, the Company completed a second drilling program, consisting of nine reverse circulation holes and two combined RC/diamond drill (core) holes. Chips and core recovered consisted of 2050 m of RC drilled, and 183 m of diamond (core), for a total of 2233 m. The program was designed to expand the known mineralized zone down-dip to 200 m vertical depth, extend the known mineralized strike length of the overall deposit to 700 m, and infill large gaps with holes drilled at 75 m spacing. Two of the drill holes finished with diamond drill core, providing information to better define the structural controls on mineralization.

 

Collar locations and azimuths for the 2011 drilling were surveyed using a handheld GPS. The Company used a magnetic REFLEX EZ-TRAC instrument to complete downhole surveys using a digital remote gyroscope. Downhole surveys were completed on all 11 drill holes from the 2011 program every 50-100 m downhole so most drill holes had at least three readings taken along with the one at the surface. Due to the high magnetic susceptibility of the subsurface, the azimuth reading and the magnetic readout gave inaccurate readouts. Therefore, only the downhole dip could be recorded with any level of confidence. The significant assays are reported as core lengths as the true width of the mineralized zone was not established.

 

Table 9 - Survey information from Red Metal’s 2011 Combined RC/Diamond drilling program.

 

Hole Number   UTM Coordinates (PSAD 56)   Azimuth (°)   Dip (°)   Depth (m)   Comments
  Easting   Northern   Elevation (masl)        
FAR-11-001   309,298   6,889,226   499   130   -65   101    
FAR-11-002   309,180   6,889,140   508   130   -65   228    
FAR-11-003   308,992   6,888,677   517   130   -60   200    
FAR-11-004   309,095   6,888,808   513   130   -65   200    
FAR-11-005   309,041   6,888,760   497   130   -60   143   Abandoned at 143 m
FAR-11-006   309,113   6,888,870   556   130   -80   200    
FAR-11-007   309,113   6,888,870   556   130   -60   162    
FAR-11-008   309,104   6,888,984   531   130   -65   200    
FAR-11-009   308,955   6,888,710   536   130   -65   247   Diamond 200-247 m
FAR-11-010   309,007   6,888,852   528   130   -60   300   Diamond 164-300 m
FAR-11-011   309,031   6,888,950   541   130   -65   252    
Total                       2,233    

 

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Table 10 - Significant intercepts from Red Metal’s 2011 drill program on the Farellón Project.

 

Drill hole Number       Assay Interval (m)   Assay Grade
      From   To   Core Length   Gold
 (ppm)
  Copper
 (%)
  Cobalt
(%)
FAR-11-001       36   49   13   0.35   2.51   0.06
  including   36   44   8   0.53   3.95   0.09
FAR-11-002   Zone faulted off, no significant intercepts
FAR-11-003       150   155   5   0.28   0.4   0.03
FAR-11-004       141   145   4   0.01   0.73   0.01
FAR-11-005       124   133   9   0.26   0.84   0.02
    Hole lost in mineralization
FAR-11-006       80   112   32   0.99   1.35   0.02
FAR-11-007       64   70   6   0.7   0.66   0.07
FAR-11-008       98   102   4   0.26   0.85   0.01
FAR-11-009       202   211.55   9.55   0.42   0.95   0.05
FAR-11-010       179.13   183   3.87   0.39   0.5   0.05
FAR-11-011       54   56   2   0.48   0.97   0.03

 

Drilling returned copper results as high as 8.86% Cu, with 0.80 g/t Au over 1 m (FAR-11-001), and 5.35 g/t Au, 4.77% Cu, and 0.024% Co over a 2 m interval (FAR-11-006). There was evidence of pinching and swelling in the mineralized vein structures, as significant intercepts ranging in width from 2 m to 32 m. Ten of the eleven drill holes contained significant intercepts (9). Drill hole FAR-11-002 did not intercept the interpreted mineralized zone, likely due to a misinterpretation of localized fault off-set of the mineralized vein.

 

All significant intercepts from the 2011 drilling program were dominated by supergene oxide mineralization from surface to ~150 m depth. Sulfide mineralization was minimal within this shallow depth range, becoming more abundant as the transition to the hypogene zone approached below ~150 m depth. This transition zone was highly variable depending on faulting, groundwater flow pathways, and variable elevation. Below 150 m, hypogene conditions dominated, resulting in abundant sulfide mineralization, as seen in drill holes FAR-11-003 (177-182 m), FAR-11-009 (202-211.55 m), and FAR-11-010 (179.13-183 m). Supergene mineralization was dominated by malachite, chrysocolla, and copper±gold within goethite and limonite iron oxides. Alteration haloes were associated with supergene mineralization such as carbonate, limonite, hematite, goethite, and manganese oxide. Other alteration minerals were present, such as chlorite, epidote, actinolite, biotite, and sericite, however these minerals were not related to the supergene mineralization.

 

Hypogene mineralization was dominated by chalcopyrite with associated gold. Chalcopyrite occurred as amorphous blebs and lesser disseminations hosted in massive, sometimes vuggy quartz and calcite. A good example was found in drill core from hole FAR-11-009 within the mineralized intersection between 202 m and 211.55 m. The mineralized intersections broadly occur along the regional lithological boundary shear zone between overlying Paleozoic metasediments to the west and underlying Jurassic intrusives to the east.

 

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Most of the 2011 drill holes did not pass through the lithological boundaries, even after drilling through the mineralized structures. Therefore, it was interpreted that this mineralization occurs in close proximity to the lithological boundaries, but that the mineralized structures do not exactly follow the contact but instead occur as splays and faults emanating off the major structural boundary.

 

The 2011 drilling results confirmed that mineralization is still present down-dip of the intersections identified during the previous drilling campaign and are still open at depth. The infill drilling confirmed that the mineralization had significant grades and initiated the process of outlining a consistent 75 m spacing between drill holes. The 2011 drilling results also indicated that the significant grades for the copper and gold mineralization were still open along strike to the northeast and southwest, as demonstrated by hole FAR-11-001, which was drilled towards the northwest. All drill holes during the 2011 drilling program intersected oxide facies mineralization with the only significant intercepts bearing sulfides in holes FAR-11-003 and FAR-11-009. The supergene-hypogene transition occurred anywhere between 50 m and 150 m and appeared to be dependent on local fracturing and faulting.

 

A mapping and sampling program was conducted on the Farellón Property in 2012, covering the contact zone between the metasediments and the diorite. The main focus of this program was to ascertain the nature of the veins occurring within each major rock type, and to determine whether any major differences existed in vein structure, mineralogy, alteration, size, and geochemical composition. Over 1,270 mapping sites were visited, with information such as major rock type and mineralization recorded. Of these sites, 56 samples were selected and submitted for geochemical analysis. The range of total copper achieved by this sampling program was between 1.17 and 5.78 % Cu, with between 50 and 99% of that representing copper sulfide mineralization. These samples also contained from 19-2465 ppm Co, and from 0.02-2.87 g/t Au.

 

Two diamond drill holes were completed in 2013 by Perfoandes on behalf of Red Metal totaling 116 m (45 m in the first hole, 71 m in the second). The first hole (F13-001) was located 28 m north of FAR-11-001 on a 45º bearing. Drill core was selectively sampled (16 m sampled from FAR-13-001 and 15 m sampled from FAR-13-002), and analysed for Au, total Cu and soluble Cu. A significant intersection was encountered in each drill hole, returning 0.7 % Cu and 0.2 g/t Au over 6 m. The second hole recorded 1.75% Cu and 0.25 g/t Au over 9 m. These results confirmed similar findings from FAR-11-001, which was collared 28 m to the south. Both holes recorded the change in mineralogy from dominantly ankerite and other carbonates to more quartz-dominant, containing pyrite and chalcopyrite mineralization.

 

In 2014, the Company entered into a contract with a Chilean artisanal miner allowing the artisanal miner to extract mineralized material on the Farellón property in return for a 10% net sales royalty. In January 2015, the artisanal miner began selling mineralized material to ENAMI, the Chilean national mining company. To date approximately 11,265 tonnes of sulfide-mineralized material with an average grade of 1.67% Cu, 5.8 g/t Ag and 0.21 g/t Au, as well as 1813 tonnes of oxide mineralized material with an average grade of 1.56% Cu has been sold to ENAMI. The ENAMI processing facility currently does not have the capability of recovering cobalt and therefore the artisanal miner did not regularly analyse for cobalt. Three grab samples taken from the same location as the mined mineralized material (Level 7 - 70 m level), were analysed for gold, copper, and cobalt, with results shown below in Table 11.

 

Table 11 - Level 7 sampling

 

70 metre Level Sampling*
Gold (ppm)   Copper (%T)   Cobalt (%)
n/a   2.86   0.12
n/a   1.43   0.07
2.2   6.8   0.11

 

*Grab samples are selective in nature and random in size and may not be representative of mineralization characteristics. n/a = not analyzed.

 

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The Kahuna concession (part of the Farellón Project area) was historically held by Vector Mining, a private company, and optioned to Catalina Resources PLC (Catalina), a private UK registered mineral exploration company. Catalina conducted a geophysical exploration program in order to determine whether the mineralized structures to the northeast, exploited in the Carrizal Alto mine, extended into the Kahuna area, to determine whether any such structures were associated with possible sulfide mineralization, and to define drill targets for a subsequent phase of work. The survey area was traversed in detail and a geological map was prepared showing all the different lithologies and previous mine workings. Two target areas were defined; one within the diorite intrusive hosting the high-grade mineralization at the old Carrizal Alto mine, the other in the surrounding metamorphic sediments. Two ground geophysical surveys (induced polarisation (IP) and magnetometry) were completed May 2007, confirming the continuity of the mineral-bearing structures between Carrizal Alto and the Kahuna area, allowing for the definition of sites for follow-up drilling.

 

The ground magnetic survey was completed on a grid measuring 1.2 km by 3.2 km. A total of 70 km were surveyed on lines spaced 50 m apart. In the IP survey a total of 27 km of data were acquired with a gradient array. Three one km lines were surveyed in a more detailed follow-up survey with a multi-array consisting of both pole-dipole and multi-bipole gradient array. The principal orientation of the shear zones was confirmed to be to the northeast towards Carrizal Alto where similar structures were exploited previously for copper and cobalt. However, there are also several trends to the northwest interpreted to be fault zones that offset the mineralized shear zones slightly. A north-south trend is probably due to dykes. A strong IP anomaly was located in the western portion of the survey area. The IP anomaly correlated with a shallow strongly conductive zone known to be associated with mineralization developed on the margin of the intrusive and exposed in shallow workings. Despite positive results warranting further attention, Catalina eventually dropped the option to the Kahuna Property, and it returned to Vector Mining.

 

 

 

Figure 5 - Drill hole collar locations on the Carrizal Property
(Geology based on Arevelo and Welkner, 2003; figure supplied by Red Metal).

 

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Perth Project Area

 

The northern concessions of the Carrizal Property have historically been called the Perth Project. There are numerous artisanal workings throughout this section of the Carrizal Property. The Puenta Negra Mine area contains the Argentina and Dos Amigos veins, with the most significant workings on the property occurring at the Argentina shaft (Figure 6). Unfortunately, no historic mining records have been located for the Argentina and Dos Amigos veins.

 

In the 1990s the Cachina Grande area of the Carrizal Alto received some attention. The Cachina Grande area is underlain by Paleozoic metasediments to the west of the dioritic-hosted Carrizal Alto. In 1991, seven samples from the Cachina Grande area were taken for the report on the Carrizal Alto mining district by Oliver Resources (Ulriksen, 1991). Samples were taken from the Argentina old workings vein 1.8 m, resulting in a range of Cu between 1.76 and 3.4% Cu, and between 0.05 and 1.22 g/t Au. Samples taken from the Dos Amigos North dump were grab samples and ranged between 0.46 and 0.83% Cu, and between 1.29 and 3.41 g/t Au.

 

Appleton Resources Ltd. optioned the Perth Property in 2007 and completed a surface sampling program covering 12 veins identified on the southern portion of the project area, as part of a NI 43-101-compliant report on their Perth Caliza Property (which includes the southern portion of the current Perth project area) (Butrenchuk, 2008). Significant results from the 56-sample program by Appleton Resources in 2007 include total copper between 0.01 and 11.4% Cu, and between 0.01 and 10.7 g/t Au and up to 0.186% Co.

 

 

 

Figure 6 - Argentina Shaft and Headframe in the northern Perth Project Area

 

In 2011, the Company conducted another sampling program, collecting 129 samples from its Perth Property, and analysing for total copper, soluble copper, gold, and cobalt. Results include total copper ranging between 0.01 to 11.36% Cu, gold ranging between 0.01 to 29.93 g/t Au, and cobalt ranging between 2 to 6933 ppm.

 

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In 2013 and 2014, the Company optioned the Perth Project area to Mineria Activa, a Chilean private mining company. Mineria Activa conducted a surface sampling, stripping and channel sampling program followed by a two-phase drilling program within the Perth Project area. The surface sampling and stripping program consisted of collecting 762 samples, a combination of grab and chip samples, and analysing them for total copper, soluble copper, gold, and cobalt. Results included a range of copper total results between 0.001 and 7.16% Cu, between 0.005 and 16.5g/t Au, and between 0.001 and 0.437% Co. Mineria Activa drilled 30 diamond drill holes on the Perth Project area, of these 30 holes, only three were entirely on the Red Metal mineral concessions, the remainder targeted a vein that is exposed at surface on a claim owned by another company that runs through the middle of Red Metal’s Perth Project area. Of these three drill holes only one, DP-04, intersected any significant mineralization; 1 m grading 2.15 gt Au, 1.32% Cu and 0.017% Co.

 

Historical Resource Estimates and Production

 

There are no formal historical resource estimates on the Farellón project. However, a number of old memo-style reports were put together by the provincial engineer for Atacama particularly in 1963. The sources for the 1963 report were other reports dated from 1942 to 1949. In the report it was noted that the deposit consisted of 3 veins in metamorphic rocks and that blocks of material approximately 50 m in length and depth had been extracted. The historical estimates do not conform to the presently accepted CIM standards and definitions, for resource estimates, as required by NI 43-101 regulations.

 

The 1963 report contained a number of tables which indicated the reserves reported in the previous 1949 report by Ing. Herbert Hornkohl. There are a number of inaccuracies in the tables contained in the 1963 report, most likely related to typing errors, and Micon has attempted to correct these errors by comparing them to the 1949 tables, where applicable. The tables from the reports are reproduced below but not all of the units of measurement were provided for the tabulated grades in the reports. Therefore, Micon has not assigned units of measurement to any grades which are not specified in the reports. After the 1949 study was conducted, the mine was worked and at 1963 there was no visible mineralization (positive ore). There were 500 tons of waste and 1,320 tons of extracted material with the following grades.

 

Table 12 - “Positive Ore”

 

    Tons Grade
    Cu (%)   Au (g/t)   Ag   CaO
 (%)
  SiO2
(%)
  Fe2O3   Al2O3   S
Veta Pique*   5,849   3.1   1.2   3.8   45.3   4.4   7.8   1.6   0.7
Veta Naciente*   6,817   2.7   1.1   4.9   44.1   5.0   11.7   2.7   0.7
Total   12,666   2.9   1.1   4.4   44.7   4.7   9.9   2.2   0.7

 

Derived from the 1949 and 1963 reports in the Sernageomin files, Chile.

 

Table 13 - Waste

 

Tons   Cu   Au   Ag   CaO   FeO   MgO   SiO2
500   2.20   1.0   10.0   45.98   5.29   0.60   2.50

 

Derived from the 1949 and 1963 reports in the Sernageomin files, Chile.

 

Table 14 - “Extractions”

 

    Tons   Cu   Au   Ag   CaO   FeO   MgO   SiO2
Veta Pique*   810   N/A   N/A   N/A   N/A   N/A   N/A   N/A
Veta Naciente*   510   N/A   N/A   N/A   N/A   N/A   N/A   N/A
Total   1,320   2.3   1.0   5.0   45.07   6.54   0.22   3.0

 

*Note: Veta Pique = Shaft vein and Veta Naciente = Outcrop vein.

Derived from the 1949 and 1963 reports in the Sernageomin files, Chile.

 

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The May 2000 Minera Stamford report mentions a resource estimate but this is a conceptual resource estimate based on a minimal amount of information. However, Micon has reviewed this conceptual estimate and concluded that it would not meet the criteria necessary for its inclusion in an NI 43-101 report. Therefore, the Company should not rely on it as justification for a program of compilation work and further exploration. Further work is required to locate and evaluate the true extent and nature of the mineralization on the Farellón Project.

 

As mentioned previously a small amount of historical production has occurred on the Farellón Property primarily during the 1940s. However, there are few existing records of the production and there appear to be some discrepancies in the potential size of the waste dumps (1,000 and 500 tons) and grades reported in the material between the 1949 and 1963 reports contained in the archived files.

 

Geological Setting

 

Regional Geology

 

Chile is divided into three major physiographic units running north-south, namely the Coastal Cordillera, Central Valley (also termed the Central Depression), and the High Cordillera (Andes). The Carrizal Property lies within the Coastal Cordillera, on the western margin of Chile (Figure 7).

 

There are five main geological units within the Coastal Cordillera, including, (1) early Cretaceous back-arc basin marine carbonates (east); (2) late-Jurassic to early-Cretaceous calc-alkaline volcanic arc rocks (central); (3) early-Cretaceous Coastal batholith (west) (Marschik, 2001); (4) the Atacama fault zone (west) (Marschik, 2001); and, (5) Paleozoic basement metasedimentary rocks along the western margin (Hitzman, 2000). Many of these geological units are shown in Figure 7.

 

The Coastal Cordillera formed in the Mesozoic Era as major plutonic complexes were emplaced into broadly contemporaneous arc and intra-arc volcanics and underlying Paleozoic deformed metasediments (Hitzman, 2000). This time period also saw development of the NW-trending brittle Atacama fault system, followed by widespread extension-induced tilting. Sedimentary sequences accumulated immediately east of the Mesozoic arc terrane in a series of interconnected, predominantly marine, back-arc basins. Early- to mid-Jurassic through mid-Cretaceous volcanism and plutonism throughout the Coastal Cordillera and immediately adjoining regions are generally considered to have taken place under variably extensional conditions in response to retreating subduction boundaries (slab roll-back) and steep, Mariana-type subduction (Hitzman, 2000).

 

Local Geology

 

The Carrizal Property covers two distinct contact zones between Paleozoic metasedimentary rocks in the central section, and late Jurassic diorites and monzodiorites to the northwest and southeast.

 

Paleozoic metasedimentary rocks belonging to the Chanaral Metamorphic Complex are composed of shales, phyllites and quartz-feldspar schists/gneisses (Minera Stamford, 2000). The sedimentary rocks have a strong NNE-striking shallow foliation dipping 40° southeast. The intrusives towards the southeast corner of the Carrizal Property, in the Farellón Project area, belong to the Canto del Agua formation and consist of diorites and gabbros hosting many NE-oriented intermediate-mafic dykes. These diorites are known to host extensive veining with copper and gold mineralization (Arevalo and Welkner, 2003). Locally, a small stock-like felsic body, called Pan de Azucar, with lesser satellite dykes, intrudes the diorite. The intrusive relationship between the diorite and metasediments on this south end of the Carrizal Property always appears to be tectonic (Willsteed, 1997).

 

Property Geology

 

The southern contact zone between the metasedimentary rocks and the diorite is a mylonitic shear zone, ranging between 5 m and 15 m in width, striking NNE, and dipping 65° to the northwest. This shear zone is host to mineralized quartz-calcite veins that splay off to the east into the diorites of the adjacent Carrizal Alto Mine area.

 

The Perth project area at the northern end of the Carrizal Property, also hosts a significant NS-trending vein swarm. Although these veins pinch and swell, they are generally 2 m wide and have been measured up to 6 m wide. Individual veins can be traced from a few 100 m to greater than 2 km in length. Most of the veins identified thus far on surface lie within the metasedimentary rocks, however several veins have been traced cross-cutting the northern metasediment-granodiorite contact.

 

39
 

 

Mineralization

 

The Carrizal Property occurs within the Central Andean IOCG Province (Sillitoe, 2003; Figure 7). Vein type, plutonic-hosted IOCG deposits such as Carrizal Alto and by extension the contiguous Carrizal Property, are characterized by a distinct mineralogy that includes not only copper and gold but also cobalt, nickel, arsenic, molybdenum, and uranium (Sillitoe, 2003; Clark, 1974). All of the IOCG deposits in the region are partially defined by their iron content in the form of either magnetite or hematite (Sillitoe, 2003).

 

 

 

Figure 7 - The Central Andean IOCG Province of northern Chile (Sillitoe, 2003).

The Carrizal Alto Mine, directly adjacent to the Carrizal Property, is highlighted (red) for reference.

 

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A variety of alteration assemblages has been noted in the Chilean deposits according to whether or not the deposits are hematite or magnetite dominated:

 

1. Magnetite-rich veins contain appreciable actinolite, biotite and quartz, as well as local apatite, clinopyroxene, garnet, hematite and K-feldspar, and possess narrow alteration haloes containing one or more of actinolite, biotite, albite, K-feldspar, epidote, quartz, chlorite, sericite and scapolite.

2. Hematite-rich veins tend to contain sericite and/or chlorite, with or without K-feldspar or albite, and to possess alteration haloes characterised (Sillitoe, 2003) by these same minerals. Typically the vein deposits of the coastal Cordillera are chalcopyrite, actinolite and magnetite deposits (Ruiz, 1962).

 

Carrizal Alto, just east of the Carrizal Property, has historically been known as a significant cobalt deposit (Ruiz, 1962; Clark, 1974) and has returned cobalt grades of up to 0.5% Co in the form of cobaltiferous arsenopyrite (Sillitoe, 2003; Ruiz, 1962), carrollite, and other cobalt sulfides (Clark, 1974). Copper mineralization on the Carrizal Property consists of malachite and chrysocolla in the oxide zone and chalcopyrite in the sulfide zone. There is some indication that in the oxide zone some of the copper mineralization is tied up in a goethite-bearing clay matrix (Willsteed, 1997; Floyd, 2009).

 

Alteration associated with the greater shear zone is comprised of actinolite, biotite, sericite, epidote, quartz and carbonate mineralization. The sulfidized quartz-calcite veins occurring within the shear zone can display an intense pyrite-sericite-biotite alteration halo. In places, there is massive siderite and ankerite alteration (Minera Stamford, 2000).

 

Deposit Types

 

The main target on the Carrizal Property is vein-style iron oxide-copper gold (IOCG) mineralization associated with a shear contact between intrusive diorite and metasedimentary rocks, containing significant amounts of iron oxide, copper, gold and cobalt, distinctive of IOCG deposits in the region (Sillitoe, 2003). IOCG deposits of northern Chile are known to exist in the belt from just south of the town of Vallenar (almost 29°S) to just south of Chanaral (26°S) (Hitzman, 2000). Although this deposit type covers a wide spectrum, the characteristic IOCG deposits of northern Chile have been clearly defined by Sillitoe (2003) as the following:

 

Iron oxide-copper-gold deposits, defined primarily by their elevated magnetite and/or hematite contents, constitute a broad, ill-defined clan related to a variety of tectono-magmatic settings. The youngest and, therefore, most readily understandable IOCG belt is located in the Coastal Cordillera of northern Chile and southern Peru, where it is part of a volcano-plutonic arc of Jurassic through Early Cretaceous age. The arc is characterised by voluminous tholeiitic to calc-alkaline plutonic complexes of gabbro through granodiorite composition and primitive, mantle-derived parentage. Major arc-parallel fault systems developed in response to extension and transtension induced by subduction rollback at the retreating convergent margin. The arc crust was attenuated and subjected to high heat flow. IOCG deposits share the arc with massive magnetite deposits, the copper-deficient end-members of the IOCG clan, as well as with manto-type copper and small porphyry copper deposits to create a distinctive metallogenic signature.

 

The IOCG deposits display close relations to the plutonic complexes and broadly coeval fault systems. Based on deposit morphology and dictated in part by lithological and structural parameters, they can be separated into several styles: veins, hydrothermal breccias, replacement mantos, calcic skarns and composite deposits that combine all or many of the preceding types. The vein deposits tend to be hosted by intrusive rocks, especially equigranular gabbrodiorite and diorite, whereas the larger, composite deposits (e.g. Candelaria-Punta del Cobre) occur within volcano-sedimentary sequences up to 2 km from pluton contacts and in intimate association with major orogen-parallel fault systems. Structurally localised IOCG deposits normally share faults and fractures with pre-mineral mafic dykes, many of dioritic composition, thereby further emphasising the close connection with mafic magmatism. The deposits formed in association with sodic, calcic and potassic alteration, either alone or in some combination, reveal evidence of an upward and outward zonation from magnetite-actinolite-apatite to specular hematite-chlorite-sericite and possess Cu-Co-Au-Ni-As-Mo-U-(LREE) (light rare earth element) signature reminiscent of some calcic iron skarns around diorite intrusions. Scant observations suggest that massive calcite veins and, at shallower paleodepths, extensive zones of barren pyritic feldspar-destructive alteration may be indicators of concealed IOCG deposits.

 

The Carrizal Property lies well within the Chilean IOCG belt and fits many of the tectonic and mineralogical definitions outlined by Sillitoe (2003). The Carrizal Property is considered to be a vein-style IOCG deposit with significant amounts of iron oxide, copper, gold and cobalt distinctive of IOCG deposits in the region.

 

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The main targets on the Carrizal Property are the two mineralized shear contact zones between the metasediments and diorites (Farellón Project area) and monzodiorites (Perth Project area). The shear zone has been interpreted to host several parallel, mineralized lenses.

 

Exploration

 

Red Metal began its exploration programs on the Property in 2009 with a 5-hole RC drilling program followed by programs in 2011 (11 RC/core holes), and in 2013 (2-hole RC drilling program), focusing on the Farellón Project area. Red Metal completed surface sampling and mapping programs between 2011 and 2014, as described below. The last work completed on the Property by the Company was in 2014.

 

Drilling

 

Red Metal acquired the rights to the Farellón Property on April 25, 2008, upon its Chilean subsidiary exercising the option to buy the Project from Minera Farellón. Red Metal completed five RC drill holes in 2009, totaling 725 m and using a Tramrock Dx40 RC rig. In 2011, Red Metal completed a second drilling program, consisting of nine RC holes and two combined RC/diamond drill (core) holes. The program was designed to expand the known mineralized zone down-dip to 200 m vertical depth, extend the known mineralized strike length of the overall deposit to 700 m, and infill large gaps with holes drilled at 75 m spacing. Two of the drill holes finished with diamond drill core, providing information to better define the structural controls on mineralization.

 

2022 Drilling Program on Farellón Alto

 

During January – February 2022, the Company successfully completed a nine-hole 2,010m drill program on its Farellón Alto 1-8 concession. The drill program targeted down dip extensions of known mineralized zones as well as testing new zones.

 

Highlights

 

First hole on new zone intercepted six meters of vein with strong visible copper sulphides; further 1.5 km of untested strike length;
All holes have intercepted visible copper sulphide mineralization and alteration associated with IOCG deposits; and
Diamond drill core provided valuable alteration and structural information not seen in previous RC drilling.

 

Diamond Drilling

 

First five drillholes were focused at the northern end of the previously drilled Farellón project close to the artisanal mine workings. All five drill holes intercepted zones of sulphide mineralization including chalcopyrite and chalcocite, zones of strong alteration associated with IOCG deposits and breccia zones up to 20m in width. Significant elements noted in initial observations included widespread potassic and argillic alteration and significant amounts of iron oxides transitioning from hematite into magnetite at depth.

 

The final four drillholes of the program targeted the south and north end of the Farellón zone and tested a previously undrilled structure parallel to the Farellón zone. These four drillholes intercepted zones of sulphide mineralization including chalcopyrite and chalcocite and zones of strong alteration associated with IOCG deposits.

 

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Table 15 - Summary of holes (1)

 

Drillhole   Target   Length   Highlights
FAR-22-012   Farellón North   143   9 metre zone with visible copper sulphide mineralization, infill gap in historic drilling
FAR-22-013   Farellón North   170   Extending known mineralization down dip by ~50 m, 23 metre zone of quartz/calcite veining with copper sulphides
FAR-22-014   Farellón North   158   Step out ~100m along strike
FAR-22-015   Farellón North   266   Down dip from FAR-22-014
FAR-22-016   Farellón North   286   Extend known mineralization to 196 metres vertical depth
FAR-22-017   Farellón South   326   Mineralized breccia zone at 236-243 m
FAR-22-018   Farellón South   293   Multiple zones of disseminated chalcopyrite mineralization and intense IOCG associated alteration
FAR-22-019   Farellón North   188   85-91 m brecciated quartz veining with strong chalcopyrite mineralization
FAR-22-020   New Zone   182   142-147.6 m quartz calcite vein with strong chalcopyrite mineralization and actinolite, iron and sericite alteration

 

(1) Widths are drill indicated core length as insufficient drilling has been undertaken to determine true widths with at this time.

 

New Zone Drill Tested

 

The newly tested parallel structure lies approximately 250 metres west of the Farellón vein and was mapped and sampled on surface in 2012. Mapping completed in 2012 traced the vein continuously over approximately 1.5km. All six surface samples taken along the structure in 2012 are listed below and all samples returned significant copper, gold and cobalt. The structure was tested with one drillhole and a six-metre quartz calcite vein was intercepted from 142m to 142.6m with visible chalcopyrite mineralization, intense pyrrhotite, albite and actinolite alteration.

 

Table 16 - Historic 2012 surface sampling on new zone

 

Sample ID   Easting   Northing   CuT%   Au g/t   Co%
123984   309701   6889159   4.97   0.43   0.07
123985   309862   6889291   3.73   0.80   0.02
123986   309644   6889070   3.40   0.41   0.03
123987   309424   6888843   1.60   0.23   0.10
123989   309227   6888420   3.86   0.68   0.04
123990   309040   6888003   2.49   0.63   0.02

  

As of the date of this Annual Report on Form 20-F sampling is ongoing for drillholes and no visual estimates of grade have been made.

 

Sample Preparation, Analysis, and Security

 

There have been no exploration or drilling samples collected by Red Metal, and as such, there are no preparation, analysis, or security details to describe.

 

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Data Verification

 

During the site visit for purposes of preparing the Technical Report, the Qualified Person verified that the Carrizal Property contains widespread underground workings. The Qualified Person examined all historical data made available relating to historic sampling and drilling within the Carrizal Property, and took six mineralized rock grab samples from the artisanal mine working and investigated underground, in order to verify the typical grades of Cu, Au, and Co encountered on the Carrizal Property.

 

A description of the samples is provided in Table 17 and assay results in Table 18. Assays from grab rock samples collected on the Carrizal Property confirmed the presence of copper (oxide and sulfide phases), gold, silver, and cobalt. In the opinion of the QP, this verification data was adequate for the purpose of the Technical Report to provide an independent review of the Company’s Carrizal Property and verify the validity of the historical database.

 

Table 17 - Description of verification samples collected on the Farellón claims of the Carrizal Property

 

Sample No.   Location   Type   Alteration/Silicates   Zone   Mineralization
FN-01   Farellón North   Grab – level 7 stockpile on surface   Chlorite; quartz>calcite   Hypogene   chalcopyrite, pyrite
FN-02   Farellón North   Grab – level 7 stockpile on surface   Chlorite; quartz>calcite   Hypogene   chalcopyrite, pyrite
FN-03   Farellón North   Grab – level 7 stockpile on surface   Chlorite; quartz>calcite   Hypogene   chalcopyrite, pyrite
FN-04   Farellón North   Grab – level 7 stockpile on surface   Chlorite; quartz>calcite   Enriched Supergene   chalcopyrite, pyrite, bornite
FS-01   Farellón South   Grab – adit stockpile – roughly 3 years on surface   Oxidized, hematized, limonite   Supergene   cuprite; azurite, malachite
FS-02   Farellón South   Grab – underground, east wall of south drift       Enriched Supergene   chalcocite, chrysocolla

 

Table 18 - Assay results for verification samples collected on the Farellón claims of the Carrizal Property

 

Sample No.   Au   Ag   Cu (total)   Cu (oxide)   Cu (sulfide)   Co   Co
Method   FA-AAS   4ACID-AAS   4ACID-AAS   LIX-AAS   Calc.   FUS-AAS   Calc.
units   ppm   ppm   %   %   %   ppm   %
(Detection Limit)   (-0.01)   (-0.1)   (-0.001)   (-0.001)   (-0.001)   (-1)   (-0.0001)
FN-01   0.46   12.1   2.735   0.119   2.616   17366   1.7366
FN-02   0.25   10.1   5.573   0.076   5.497   578   0.0578
FN-03   0.16   12.3   6.631   0.12   6.511   171   0.0171
FN-04   1.56   28.5   7.145   0.213   6.932   2086   0.2086
FS-01   3.49   5.3   10.62   10.786   0   467   0.0467
FS-02   0.48   2.3   3.538   3.221   0.317   2285   0.2285

 

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Northern Section of the Farellón Project Area

 

Samples FN-01 through FN-04 were collected from an ore dump near the portal to the North Mine. The ore, reported to be from Level 7 of the mine (hypogene/enriched supergene zones), contained mainly chalcopyrite with lesser bornite.

 

 

 

Figure 8 - North Mine portal access

 

 

 

Figure 9 - Mineralized rocks from underground at the North Mine, Level 7

 

Assays from samples FN-01 through FN-04 range from 0.16 to 1.56 ppm Au, 10.1 to 28.5 ppm Ag, 2.74 to 7.15% Cu(T); the copper was mainly in sulfide form (e.g. chalcopyrite). The highest concentration of gold and silver were from sample FN-04 which also had the highest sulfide copper concentration. Analyses for cobalt, using the peroxide fusion method, returned concentrations ranging from 0.21% to 1.74% Co.

 

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Southern Section of the Farellón Project Area

 

Sample FS-01 was collected from a small stockpile near the old workings of the South Mine which had been exposed to the elements for a number of years. This sample was heavily oxidized and contained copper oxides including cuprite, malachite and azurite (supergene zone). Sample FS-02 was collected from the east wall of the south drift in the South Mine Exploration Portal. This sample contained chalcocite, chrysocolla, malachite, and azurite (enriched supergene zone).

 

 

 

Figure 10 - Old south mine workings on the Farellón Project area looking north

Assays from sample FS-01 reflect its high copper oxide content reporting 10.62% Cu(T) and averaging 10.70% Cu between the two assay methods used for copper. This sample contained the highest gold concentration at 3.49 ppm Au and assayed 0.05% Co. Sample FS-02 contained 3.54% Cu(T), with relatively low sulfide copper (enriched supergene zone), and 0.23% Co.

 

 

 

Figure 11 - Main mineralization structure from underground exploratory workings in the South Mine and the site of rock sample FS-02

 

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Figure 12 - Mining personnel standing in front of the South Mine exploration portal in the Farellón Project area

 

Mineral Processing and Metallurgical Testing

 

No mineral processing or metallurgical testing programs have been undertaken on the Carrizal Property.

 

Mineral Resource Estimates

 

No mineral resource estimates have been done for the Carrizal Property. As discussed in the “CARRIZAL PROPERTY – FARELLÓN AND PERTH PROJECTS – Exploration History” section of this Annual Report on Form 20-F, some documentation exists for historical resource estimates on the Farellón Project prior to February 1, 2001. However, the historical estimates do not conform to the presently accepted CIM standards and definitions for resource estimates, as required by NI 43-101 regulations. As such, the Company is not relying on the historical resource estimates as justification for a program of compilation work and further exploration.

 

As exploration progress on the Farellón Project, further economic and technical evaluation of the resource potential for the project will need to be performed in accordance with present industry practices and standards, as set out in NI 43-101.

 

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Mateo Property

 

Property Description and Location

 

The Mateo Property is composed of 5 mineral concessions covering 182 hectares in the III Region of Chile, Region de Atacama. The project is situated 10 kilometres east of the City of Vallenar with the highest point at approximately 1,050 metres above sea level. The property is located close to power, water, and the urban centre of Vallenar, with a readily available mining workforce.

 

Accessibility

 

The property is easily accessible year-round via a well-used road from Vallenar. The road crosses through the middle of the west half of the property and along the southern border of the east half of the property.

 

Geology and Mineralization

 

The Mateo Property is located within the brittle-ductile north-south-trending Atacama Fault System that is known to host many of the major deposits in the Candelaria IOCG belt. Known mineralization is hosted in an andesitic volcaniclastic sequent assigned to the Bandurrias Formation. Widespread iron oxide and skarn style alteration indicate an IOCG mineralizing system further supported by significant amounts of economic grade mineralization found in six historic artisanal mines on the property. Mineralization is found in mantos, veins and breccias.

 

Exploration History

 

Historical work on the Mateo Property includes several drill programs completed by different Chilean private and public companies. Records exist from eight drill holes completed in 1994 on the Irene mine and include two full reports written by ENAMI, the Chilean national mining company, with interpretation of mineralization and recommendations for further exploration and mining work.

 

The Irene mine was investigated by ENAMI in 1994. Work completed during the time included surface RC drilling, including 490 metres in four RC drill holes, and underground diamond drilling, including 220 metres in four drill holes. The Company obtained ENAMI’s reports of mining activities from 1994 to 1997. Approximately 11,875 tonnes of rock were mining in that time averaging 4.3% copper, 61.9 grams per tonne silver, and 1.01 grams per tonne gold. During the period June 2009 to December 2010, the vendor of the Irene mine, Minera Farellón, conducted small scale mining activities on a different area of the Irene claims and mined 1,705 tonnes grading 1.39$ Cu, 1.39 g/t Ag, 0.29 g/t Au in sulphides and 1,477 tonnes grading 1.98% Cu in oxides. The difference in grade between the historic work and recent work is not an indication that further high-grade material will not be found on the Mateo Property and further modeling and exploration work needs to be completed to determine the best drill targets.

 

Drilling

 

No drilling has been completed on the Mateo Property.

 

Sampling, Analysis and Data Verification

 

In 2011, the Company completed a mapping and prospecting program over an area including the Mateo concessions and a wide area surrounding the concessions. The geological mapping identified nine significant zones of mineralization on the property and confirmed widespread skarn style alteration. Reconnaissance samples were collected on multiple mineralized structures from mantos, veins and mineralized breccia bodies. All samples were taken to Geoanalitica Ltda Laboratories in Coquimbo. No reference samples were used for the mapping samples.

 

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Samples of 21.72 g/t Au with 0.69% Cu, 3.10 g/t Au with 0.50% Cu and 3.57 g/t with 0.62% Cu taken from one vein traced for approximately 350 metres on surface. Multiple mineralized veins, mantos and breccia bodies were identified with 36 of 138 samples returning Au results greater than 1.00 g/t and 59 of 138 samples returning Cu results greater than 1.00%.

 

Table 19 - Additional significant reconnaissance sampling results from the Mateo mapping program are listed below:

 

Sample   Easting   Northing   Cu %