The Registrant hereby amends this registration statement on such date or dates as may be necessary to delay its effective date until the registrant shall file a further amendment which specifically states that this registration statement shall thereafter become effective in accordance with section 8(a) of the Securities Act of 1933 or until the registration statement shall become effective on such date as the Securities and Exchange Commission, acting pursuant to such section 8(a), may determine.

PROSPECTUS

THE INFORMATION IN THIS PROSPECTUS MAY BE CHANGED. THESE SECURITIES MAY NOT BE SOLD UNTIL THE REGISTRATION STATEMENT FILED WITH THE SECURITIES AND EXCHANGE COMMISSION IS EFFECTIVE. THIS PROSPECTUS IS NOT AN OFFER TO SELL THESE SECURITIES AND IT IS NOT SOLICITING AN OFFER TO BUY THESE SECURITIES IN ANY STATE WHERE THE OFFER OR SALE IS NOT PERMITTED. THERE IS NO MINIMUM PURCHASE REQUIREMENT FOR THE OFFERING TO PROCEED

WALL STREET ACQUISITIONS CORP

WALL STREET ACQUISITIONS CORP

3,000,000 SHARES OF COMMON STOCK OFFERED BY WALL STREET ACQUISITIONS CORP

300,000 SHARES OF COMMON STOCK OFFERED BY SELLING STOCKHOLDERS $7.00 PER SHARE

NO MINIMUM

This prospectus relates to both (i) the initial public offering of the common stock of Wall Street acquisitions Corp, a Delaware corporation (“WSAC,” the “Company,” “we,” “us,” “our””our” and words of similar import), in which we are offering a maximum of 3,000,000 of our common stock, and (ii) the resale by certain Selling Stockholders of WSAC of up to 300,000 shares of common stock held by Selling Stockholders of WSAC. While we will receive proceeds from our own sale of our common stock, we will not receive any of the proceeds from the sale of the shares by the Selling Stockholders. Any purchaser of common stock in the offerings may be the only purchaser, given the lack of a minimum offering amount.

In our initial public offering, we are offering for sale a total of 3,000,000 shares of common stock at a fixed price of $7.00 per share for the duration of the offering. There is no minimum number of shares that must be sold by us for the offering to proceed, and we will retain the proceeds from the sale of any of the offered shares. The offering is being conducted on a self-underwritten, best effortsbest-efforts basis, which means our management will attempt to sell the shares. This prospectus will permit our President, Jimmy Ramirez to sell the shares directly to the public, with no commission or other remuneration payable to him for any shares he may sell. Mr. Ramirez will sell the shares and intends to offer them to friends, family members and business acquaintances. In offering the securities on our behalf, our officers and directors will rely on the safe harbor from broker-dealer registration set out in Rule 3a4-1 under the Securities Exchange Act of 1934, as amended (the “Exchange Act”). The shares will be offered at a fixed price of $7.00 per share for the duration of the offering, which is a period of 18 months from the effective date of this prospectus. Mr. Jimmy Ramirez and Franklin Ogele, Vice President/General Counsel are the two Selling Stockholders. The Selling Stockholders will not sell any of their 300,000 shares until the Company sells all of the 3,000,000 shares registered herein or the Offering is terminated as provided in this Registration Statement whichever occurs earlier. In the resale by Selling Stockholders, the Selling stockholders will be offering their shares of common stock at a fixed price of $7.00 per share, for the duration of the offering, until our shares are listed on a national securities exchange or quoted on the OTCBB and thereafter at prevailing market prices or privately negotiated prices. Each of the Selling Stockholders may be deemed to be an “underwriter” as such term is defined in the Securities Act of 1933, as amended (the “Securities Act”). The net proceeds to be received by the Selling Stockholders is $1,887,000 assuming that the selling shareholders sell all 300,000 shares they are collectively offering.

We may also engage registered broker-dealers and FINRA member firm to distribute the offering. As of the date of this Registration Statement, (i) no selling agreements had been entered into by us with any broker-dealer firms. In the event a broker-dealer is retained by us to participate in the offering, we must file a post-effective amendment to the registration statement to disclose the arrangements with the broker-dealer, and that the broker-dealer will be acting as an underwriter and will be so named in the prospectus. Additionally, FINRA must approve the terms of the underwriting compensation before the broker-dealer may participate in the offering. We are subject to applicable provisions of the Exchange Act and the rules and regulations under it, including, without limitation, Rule 10b-5 and a distribution participant under Regulation M. All of the foregoing may affect the marketability of the common stock.

We have not made any arrangements to place funds received from share subscriptions in an escrow, trust, or similar account. Any funds raised from the offering will be immediately available to us for our immediate use. Accordingly, if we file for bankruptcy protection or a petition for involuntary bankruptcy is filed by creditors against us, your funds will become part of the bankruptcy estate and administered according to the bankruptcy laws. If a creditor sues us and obtains a judgment against us, the creditor could garnish the bank account and take possession of the subscriptions. As such, it is possible that a creditor could attach your subscription. If that happens, you will lose your investment and your funds will be used to pay creditors.

As there is no existing market for our common stock, the Selling Stockholders will sell their shares of common stock at the fixed price of $7.00 per share until our shares are listed on a national securities exchange or quoted on the OTC Bulletin Board (“OTCBB”) at which time they may sell the shares at the prevailing market prices or at privately negotiated prices. If the Selling Stockholders were to sell all 300,000 Secondary Offering shares at the fixed price of $7.00 per share, the Selling Stockholders would realize gross proceeds of $2,100,000. Because it is impossible to estimate the total amount of any sales commissions or other costs associated with such sales, it is impossible to estimate the net proceeds to be received by the Selling Stockholders in such a case. However, we estimate the Selling Stockholders will net about $1,887,000 if the entire 300,000 shares were sold. Thereafter, the Selling Stockholders may offer their shares at prevailing market prices or at privately negotiated prices. Because such prices are currently unknown, it is impossible to determine the Selling Stockholders’ net proceeds of all of their shares of common stock are sold. Each of the Selling Stockholders may be deemed to be an “underwriter” as such term is defined in the Securities Act of 1933, as amended (the “Securities Act”).

We are an “emerging growth company” as defined in the Jumpstart Our Business Startups Act, or the JOBS Act, and, as such, may elect to comply with certain reduced reporting requirements for this Registration Statement and future filings after this Offering.

There shall be no minimum amount invested before the Company shall have access to the proceeds. The Offering will terminate upon the earlier of (i) such time as all of the shares of Common Stock have been sold pursuant to this Registration Statement or (ii) 548 [18 months] days from the effective date of this Registration Statement, unless extended by the Company’s directors, in their sole discretion, for an additional 90 days (iii)We may however, at any time and for any reason, terminate the Offering without notice to or consent from any purchaser of shares of Common Stock in the Offering.

The proceeds from the sale of the shares of Common Stock will be placed directly into the Company’s account; any investor who purchases shares will have no assurance that any monies, beside their own, will be subscribed pursuant to this Registration Statement. All proceeds from the sale of the shares of Common Stock are non-refundable, except as may be required by applicable laws. The Company will receive the proceeds from the sale of shares offered herein; all expenses incurred in this Offering are being paid for by the Company.

There has been no public trading market for the Common Stock. Upon completion of this Offering, we will attempt to have the shares quoted on the OTCBB operated by the Financial Industry Regulatory Authority (“FINRA”). There is no assurance that the shares of Common Stock will ever be quoted on the OTCBB. To be quoted on the OTCBB, a market maker must apply with the Financial Industry Regulatory Authority (“FINRA”) to make a market in our Common Stock. As of the date of this Registration Statement, we have not engaged in preliminary discussions with a FINRA market maker regarding participation in a future trading market for our securities; however, no filing with FINRA has been made.

THE PURCHASE OF THE SECURITIES OFFERED THROUGH THIS PROSPECTUS INVOLVES A HIGH DEGREE OF RISK. YOU SHOULD CAREFULLY READ AND CONSIDER THE SECTION OF THIS PROSPECTUS ENTITLED “RISK FACTORS” ON PAGE 4 BEFORE BUYING ANY SHARES OF WALL STREET ACQUISITIONS CORP.’S COMMON STOCK.

NEITHER THE SEC NOR ANY STATE SECURITIES COMMISSION HAS APPROVED OR DISAPPROVED OF THESE SECURITIES OR PASSED UPON THE ADEQUACY OR ACCURACY OF THIS PROSPECTUS. ANY REPRESENTATION TO THE CONTRARY IS A CRIMINAL OFFENSE.

THE INFORMATION IN THIS PROSPECTUS IS NOT COMPLETE AND MAY BE CHANGED. WE MAY NOT SELL THESE SECURITIES UNTIL THE REGISTRATION STATEMENT FILED WITH THE SECURITIES AND EXCHANGE COMMISSION IS EFFECTIVE. THIS PROSPECTUS IS NOT AN OFFER TO SELL THESE SECURITIES AND IT IS NOT SOLICITING AN OFFER TO BUY THESE SECURITIES IN ANY STATE WHERE THE OFFER OR SALE IS NOT PERMITTED.

(1) We estimate 10% commission for underwriters and broker-dealers.

(2) We estimate the Offering Expenses consisting of legal and accounting fees to be $100,000.

In the resale by certain Selling Stockholders, the Selling stockholders will be offering their shares of common stock at a fixed price of $7.00 per share, for the duration of the offering, until our shares are listed on a national securities exchange or quoted on the OTCBB and thereafter at prevailing market prices or privately negotiated prices. Each of the Selling Stockholders may be deemed to be an “underwriter” as such term is defined in the Securities Act of 1933, as amended (the “Securities Act”). The net proceeds to be received by the Selling Stockholders is estimated at $1,887,000 assuming that the selling shareholders sell all 300,000 shares they are collectively offering.

Subject to Completion, Dated May 3,August 7, 2022

TABLE OF CONTENTS

WALL STREET ACQUISITIONS CORP.

4440 S. PIEDRAS DR, SUITE 136205

SAN ANTONIO, TX 78228

SUMMARY OF PROSPECTUS

You should read the following summary together with the more detailed business information, financial statements and related notes that appear elsewhere in this prospectus. In this prospectus, unless the context otherwise denotes, references to “the Company”,Company,” “we,” “us,” “our” and are to Wall Street Acquisitions Corp. The Selling Shareholders are referred to herein as “the Selling Shareholders”

GENERAL INFORMATION ABOUT OUR COMPANY

Wall Street Acquisitions Corp was incorporated in the State of Delaware on December 2, 2016. On February 24, 2017, the Company filed a Form 10-12G pursuant to the Exchange Act of 1934 to register 3,000,000 shares of common stock. On September 17, 2019, the Company acquired, in a stock-for-stock exchange transaction, all the issued and outstanding shares of WSA Gold & Minerals, Inc., a Texas corporation (“WSA Gold”). WSA Gold is the owner of various mining properties in Nevada, New Mexico, and Arizona. In the stock-for-stock exchange transaction, 85% of the Company’s shares was retained by Mr. Ramirez, President, and sole shareholder of WSA Gold while Mr. Ogele retained 15% interest in the Company which allocation is memorialized in the Shareholders Agreement. Mr. Ogele also stepped down as President and Director of the Company and Mr. Ramirez was elected President, CEO and Director of the Company. We plan to enter into the gold mining space through the exploitation of the mining properties in Nevada, New Mexico, and Arizona. On April 27, 2020, the Company amended the Certificate of Incorporation raising the authorized common stock to 600,000,000 shares at $.0001 par value. We are in the excavation stage of our planned mining operations. See Exhibit 10.7 - Share Purchase and Merger Agreement.

We intend to use the net proceeds from this offering to develop our business operations (See “Description of Business” and “Use of Proceeds”). The Offering is being conducted on a “best efforts” basis and there is no minimum number of Shares that must be sold. Accordingly, all funds raised in this Offering will become immediately available to us and may be used as they are accepted. Investors will not be entitled to a refund and could lose their entire investment.

There is no assurance that we will generate additional revenue in the first 12 months after completion of our offering or ever generate more revenue.

We are exploration stage company and have a limited operating history. Except as disclosed per Exhibit 10.2 to this Registration Statement, we do not currently have any arrangements for additional financing. If the offering proceeds are less than registration costs, Mr. Ramirez has agreed to loan the Company money to complete the registration process. However, he is not under any legal obligation to fund the registration costs. The loan would be necessary if the proceeds from this offering is not sufficient to maintain our reporting status. Mr. Ramirez has so far advanced us $51,852 on the $100,000 promissory note. The loan is a zero % interest bearing note due on September 30, 2022 Mr. Ogele has also advanced us $15,166 under the same terms. In addition, Global Mortgage Banking, a company owned by Mr. Ramirez, loaned us $2,050.00 under similar terms. Ramirez, Ogele and Global Mortgage Banking will be repaid from revenues of operations if and when we generate sufficient revenues to pay the obligation. See Exhibit 10.2

Our principal executive offices are located at 4440 S. Piedras Drive, San Antonio, TX 78228. Our phone no is 210-468-5356.

From inception until the date of this filing, we have had limited operating activities. Our financial statements from inception on December 2, 2016 through March 31, 20212022 reports $115$241 in cash balance and a net lossan accumulated deficit of $244,203.$293,822. Our independent registered public accounting firm has issued an audit opinion that includes a statement expressing substantial doubt as to our company’s ability to continue as a going concern.

This Offering is being conducted on a “best efforts” basis by our officers, directors, and employees, and may be offered through broker-dealers who are registered with the Financial Industry Regulatory Authority (“FINRA”), or through other independent referral sources. Our executive officers, directors and employees will not receive any commission or any other remuneration for any sales of Shares. In offering Shares on our behalf, our executive officers will rely on the safe harbor from broker-dealer registration set out in Rule 3a4-1 under the Securities Exchange Act of 1934.

As of the date of this prospectus, there is no public trading market for our common stock and no assurance that a trading market for our securities will ever develop.

THE OFFERING

Selected Financial Data

The Following financial information summarizes the Company’s financial condition for period ended March 31, 2021.2022.

RISK FACTORS

Ownership of the common stock involves certain risks. You should carefully consider the risks and uncertainties described in evaluating an investment in the common stock.

Risks Related to Our Business

We have a limited operating history and may not be successful in developing profitable business operations.

We have a limited operating history having been incorporated only in December 2016 and executed a business combination with WSA Gold only in September 2019. Our business operations must be considered in light of the risks, expenses and difficulties frequently encountered in establishing a business in the mining space. As of the date of this prospectus, we have no revenues, except mining properties which are yet to be exploited or excavated. We have an insufficient history at this time on which to base an assumption that our business operations will prove to be successful in the long-term. Our future operating results will depend on many factors, including:

To achieve profitable operations in the future, we must, alone or with others, successfully manage the factors stated above, as well as continue to develop ways to enhance our production efforts. Despite our best efforts, we may not be successful in our efforts to execute on our mining projects or obtain required regulatory approvals.

The value of our property is subject to volatility in the price of gold and any other deposits we may seek or locate.

Our profitability will be significantly affected by changes in the market price of gold and silver, and other minerals. These mineral prices fluctuate widely and are affected by numerous factors, all of which are beyond our control. For example, the price of gold can be influenced by the sale or purchase of gold by central banks and financial institutions; interest rates; currency exchange rates; speculation; inflation or deflation; fluctuation in the value of the United States dollar and other currencies; global and regional supply and demand, including investment, industrial and jewelry demand; and the political and economic conditions of major gold producing countries throughout the world, such as Russia and South Africa. The price of gold and other minerals has fluctuated widely in recent years, and a decline in the price of gold or other minerals could cause a significant decrease in the value of our property, limit our ability to raise money, and render continued exploration and development of our property impracticable. If that happens, then we could lose our rights to our property and be compelled to sell some or all of these rights. Additionally, the future development of our mining properties is heavily dependent upon the level of metals prices remaining sufficiently high to make the development of our property economically viable. An investor may lose its investment if the price of these minerals substantially decreases. The greater the decrease in the price of gold or other minerals, the more likely it is that an investor will lose money.

We do not know if our properties actually contain any gold, silver, copper, or other precious minerals that can be mined at a profit.

Our mining properties have been studied and explored. Although the study report, specifically, the National Reserve Estimate – National Instrument 43-101 Technical Report indicates presence of precious mineral deposits, including, but not limited to gold; we cannot guarantee that the precious metals can be mined at profit. Whether a precious mineral deposit can be mined at a profit depends upon many factors. Some but not all of these factors include: the particular attributes of the deposit, such as size, grade, and proximity to infrastructure; operating costs and capital expenditures required to start mining a deposit; the availability and cost of financing; the price of the gold or other mineral which is highly volatile and cyclical; and government regulations, including regulations relating to prices, taxes, royalties, land use, importing and exporting of minerals and environmental protection.

We are a junior mining company with limited operating mining activities, and we may not be able to increase our mining activities in the future.

Our business is mining for gold, silver, and other precious minerals. Mining operations in the United States are subject to many different federal, state, and local laws and regulations, including stringent environmental, health and safety laws. In the event we increase operations on our mining properties, it is possible that we will be unable to comply with current or future laws and regulations, which can change at any time. It is possible that changes to these laws will be adverse to our mining operations. Moreover, compliance with such laws may cause substantial delays and require capital outlays in excess of those anticipated, adversely affecting any potential mining operations. Our future mining operations may also be subject to liability for pollution or other environmental damage. We are not currently insured against this risk because of high insurance costs.

We are a mining business in the exploration stage, with no experience in the market, and failure to successfully compensate for this inexperience may adversely impact our operations and financial position.

We are considered an “junior mining company”.company.” Junior mining companies typically have proven and probable reserves of less than one million ounces of gold, generally produce less than 100,000 ounces of gold annually, and/or are in the process of trying to raise enough capital to fund the remainder of the steps required to move from a staked claim to production. As a junior mining company in a highly competitive industry, we have little operating history, few substantial tangible assets, no customer base, and no revenue to date. This makes it difficult to evaluate our future performance and prospects. Our prospects must be considered in light of the risks, expenses, delays, and difficulties frequently encountered in establishing a business in an industry characterized by intense competition, including:

We cannot be sure that we will be successful in meeting these challenges and addressing these risks and uncertainties. If we are unable to do so, our business will not be successful and the value of your investment in our company will decline.

Our failure to protect our mineral property rights may significantly impair our competitive advantage.

Our success and ability to compete depend in large part upon protecting our mineral property rights. We rely on a combination of fund raising and deferred financing to protect our property rights. The steps we have taken may not be sufficient to prevent the expiration of these rights.

We may face costly claims against our mineral property rights, the result of which would decrease the amount of cash we would anticipate to operate and complete our business plan.

We anticipate that from time to time we could receive communications from third parties asserting that they have certain property rights. If anticipated claims arise, we will evaluate their merits. Any claims brought by third parties could result in protracted and costly litigation, which could result in substantial cost to us and diversion of our resources, may be necessary to enforce our property rights or to defend us against claims by others. Any litigation could have a material adverse effect on our business, financial condition, and results of operations.

We will incur costs associated with SEC reporting compliance, which may significantly affect our financial condition.

The Company made the decision to become an SEC “reporting company” in order to comply with applicable laws and regulations. We will incur certain costs of compliance with applicable SEC reporting rules and regulations including, but not limited to attorneys’ fees, accounting and auditing fees, other professional fees, financial printing costs and Sarbanes-Oxley compliance costs in an amount estimated at approximately $25,000 per year. On balance, the Company determined that the incurrence of such costs and expenses was preferable to the Company being in a position where it had very limited access to additional capital funding.

Historically, we have not been timely in meeting our required periodic reporting requirements under the Securities Exchange Act of 1934, as amended. As a result, we will be ineligible to use Form S-3 or Form S-4 for a period of time. This may adversely affect our ability to engage in certain types of corporate acquisition and capital-raising transactions.

As a result of our delayed filing of certain of our periodic reports, we will be ineligible to register our securities on Form S-3 or Form S-4 for sale by us or resale by other security holders until we have timely filed all periodic reports under the Securities Exchange Act of 1934 for a period of time. In the meantime, we have the ability to use Form S-1 to raise capital or complete acquisitions. The need to use Form S-1, and the inability to use Form S-3 or Form S-4, could increase our transaction costs and adversely affect our ability to engage in certain types of corporate acquisition and capital-raising transactions until we regain our S-3/S-4 eligibility.

The nature of mineral excavation and production activities involves a high degree of risk and the possibility of uninsured losses that could materially and adversely affect our operations.

Our efforts will be subject to all of the operating hazards and risks normally incident to exploring for and developing mineral properties, including, but not limited to:

Any of these risks can materially and adversely affect, among other things, the development of mineral properties, production quantities and rates, costs and expenditures, and production commencement dates. We currently have no insurance to guard against any of these risks. If we determine that capitalized costs associated with any of our mineral interests are not likely to be recovered, we will incur a write-down of our investment in these interests. All of these factors may result in losses proportionate to amounts spent, which may not be recoverable.

The potential profitability of mineral ventures depends in part upon factors beyond our control and even if we discover and exploit mineral deposits, we may never become commercially viable, and we may be forced to cease operations.

The commercial feasibility of mineral properties is dependent upon many factors beyond our control, including the existence and size of mineral deposits in the properties, the proximity and capacity of processing equipment, market fluctuations of prices, taxes, royalties, land tenure, allowable production, and environmental regulation. These factors cannot be accurately predicted and any one or more of these factors may result in our Company not receiving an adequate return on invested capital. These factors may have material and negative effects on our financial performance and our ability to continue operations.

Mining activities are subject to comprehensive regulation, which may cause substantial delays or require capital outlays in excess of those anticipated, causing an adverse effect on our company.

Mining activities are subject to various laws, regulations and policies governing prospecting, mine development, mineral production, removal, and transport of natural resources, as well as discharge of materials into the environment. Mining activities are also subject to various regulations regarding taxation, import and export, labor standards, occupational health standards, safety standards, waste disposal, toxic substances, land use, water use, environmental protection, and other matters.

Permits from various governmental authorities are required for mining operations to be conducted, and no assurance can be given that such permits will be successfully obtained. Environmental and other legal standards imposed by governmental authorities may be changed, and any such change may prevent us from conducting planned activities, or increase our costs of doing so, which could have material adverse effects on our business. Moreover, compliance with such laws may cause substantial delays or require capital outlays in excess of those anticipated, thus causing an adverse effect on our business operations. Additionally, we may be subject to liability for pollution or other environmental damages, which we may not be able to insure against due to prohibitive premium costs and other financial and practical considerations. Any laws, regulations, or policies of any government body or regulatory agency may be changed, applied, or interpreted in a manner which will alter and negatively affect our ability to carry on our business. We cannot assure you that new rules and regulations will not be enacted, or that existing rules and regulations will not be applied in a manner which could limit or curtail our exploration or development activities on our properties.

We believe that we are in compliance with all material laws and regulations that currently apply to our activities, but there can be no assurance that we can continue to remain in compliance. Further, there can be no assurance that we will be able to obtain or maintain all permits necessary for our future operations, or that we will be able to obtain them on reasonable terms. To the extent such necessary approvals are required and are not obtained, we may be delayed or prohibited from proceeding with planned exploration or development of our mineral properties.

Our property title may be challenged. We are not insured against any challenges, impairments or defects to our mineral claims or property title.

Our property is comprised of patented and unpatented lode claims created and maintained in accordance with the federal General Mining Law of 1872. Unpatented lode claims are unique U.S. property interests and are generally considered to be subject to greater title risk than other real property interests because the validity of unpatented lode claims is often uncertain. This uncertainty arises, in part, out of the complex federal and state laws and regulations under the General Mining Law. Until the claims are surveyed, the precise location of the boundaries of the claims may be in doubt and our claims subject to challenge. If we discover mineralization that is close to the claims’ boundaries, it is possible that some or all of the mineralization may occur outside the boundaries. In such a case we would not have the right to extract those minerals. This uncertainty leaves us exposed to potential title suits. Defending any challenges to our property title will be costly and may divert funds that could otherwise be used for exploration activities and other purposes. In addition, unpatented lode claims are always subject to possible challenges by third parties or contests by the federal government, which, if successful, may prevent us from exploiting our discovery of commercially extractable gold. Challenges to our title may increase our costs of operation or limit our ability to explore on certain portions of our property. We are not insured against challenges, impairments, or defects to our property title, nor do we intend to carry title insurance in the future.

We may not be able to maintain the infrastructure necessary to conduct mining activities.

Our mining activities depend upon adequate infrastructure. Reliable roads, bridges, power sources and water supply are important factors which affect capital and operating costs. Unusual or infrequent weather phenomena, sabotage, government or other interference in the maintenance or provision of such infrastructure could adversely affect our mining activities and financial condition.

Our mining activities may be adversely affected by the local climate.

The local climate sometimes affects our mining activities on our properties. Earthquakes, heavy rains, snowstorms, and floods could result in serious damage to or the destruction of facilities, equipment or means of access to our property, or could occasionally prevent us temporarily from conducting mining activities on our property. Because of their rural location and the lack of developed infrastructure in the area, our mineral properties in Utah are occasionally impassible during the winter season. During this time, it may be difficult for us to access our property, maintain production rates, make repairs, or otherwise conduct mining activities on them.

Risks Relating to the Mining Industry

Mining for precious metals is an inherently speculative business. The properties on which we have the right to mine for precious minerals are not known to have any proven or probable reserves. If we are unable to extract gold, silver, or any other resources which can be mined at a profit, our business could fail.

Natural resource mining, and precious metal mining, in particular, is a business that by its nature is speculative. There is a strong possibility that we will not discover gold, silver, or any other resources which can be mined or extracted at a profit. Even if we do discover and mine precious metal deposits, the deposits may not be of the quality or size necessary for us or a potential purchaser of the property to make a profit from mining it. Few properties that are explored are ultimately developed into producing mines. Unusual or unexpected geological formations, geological formation pressures, fires, power outages, labor disruptions, flooding, explosions, cave-ins, landslides, and the inability to obtain suitable or adequate machinery, equipment or labor are just some of the many risks involved in mineral exploration programs and the subsequent development of gold deposits. If we are unable to extract gold, silver, or any other resources which can be mined at a profit, our business could fail.

Our business is subject to extensive environmental regulations which may make exploring or mining prohibitively expensive, and which may change at any time.

All of our operations are subject to extensive environmental regulations which can make exploration expensive or prohibit it altogether. The regulations include, but are not limited to, The Mine Safety and Health Act, The National Environmental Policy Act, The Clean Air Act, The Resource Conservation and Recovery Act, The Clean Water Act, The Toxic Substances Control Act and The Comprehensive Environmental Response, Compensation and Liability Act. We may be subject to potential liabilities associated with the pollution of the environment and the disposal of waste products that may occur as the result of exploring and other related activities on our properties. We may have to pay to remedy environmental pollution, which may reduce the amount of money that we have available to use for exploration. This may adversely affect our financial position, which may cause loss of investor investment. If we are unable to fully remedy an environmental problem, we might be required to suspend operations or to enter into interim compliance measures pending the completion of the required remedy. If a decision is made to mine our properties our potential exposure for remediation may be significant, and this may have a material adverse effect upon our business and financial position. All of our exploration and, if warranted, development activities may be subject to regulation under one or more local, state, and federal environmental impact analyses and public review processes. It is possible that future changes in applicable laws, regulations and permits or changes in their enforcement or regulatory interpretation could have significant impact on some portion of our business, which may require our business to be economically re-evaluated from time to time. These risks include, but are not limited to, the risk that regulatory authorities may increase bonding requirements beyond our financial capability. Inasmuch as posting of bonding in accordance with regulatory determinations is a condition to the right to operate under all material operating permits, increases in bonding requirements could prevent operations even if we are in full compliance with all substantive environmental laws. We will be required to post substantial bonds under various laws relating to mining and the environment and may in the future be required to post further bonds to pursue additional activities. We may be unable or unwilling to post such additional bonds which could prevent us from realizing any commercial mining success or commencing mining activities. We estimate that compliance with existing government environmental regulations will costs us approximately $200,000 which amount we have incorporated in our Use of Proceeds table.

Market forces or unforeseen developments may prevent us from obtaining the supplies, equipment, and skilled manpower necessary to explore for mineral resources.

Precious metals exploration, and resource exploration in general, is a very competitive business. Competitive demands for contractors and unforeseen shortages of supplies and/or equipment could result in the disruption of our planned exploration and production activities. Current demand for exploration drilling services, equipment and supplies is robust and could result in suitable equipment and skilled manpower being unavailable at scheduled times for our exploration and production programs. Fuel prices are extremely volatile as well. We will attempt to locate suitable equipment, materials, manpower and fuel if sufficient funds are available. If we cannot find the equipment, supplies and skilled manpower needed for our various exploration and production programs, we may have to suspend some or all of them until equipment, supplies, funds and/or skilled manpower become available. Any such disruption in our activities may adversely affect our exploration activities and financial condition.

Risks Relating to Our Organization and Common Stock

We are in an early stage of development. If we are not able to develop out business as anticipated, we may not be able to generate revenues or achieve profitability and you may lose your investment.

We were incorporated in December 2016. We have no production, no customers, and we have not earned any revenues to date. Our business prospects are difficult to predict because of our limited operating history, early stage of development, and unproven business strategy. Our primary business activities will be focused on exploitation of our mining properties. Although we believe that our business plan has significant profit potential, we may not attain profitable operations and our management may not succeed in realizing our business objectives. If we are not able to develop out business as anticipated, we may not be able to generate revenues or achieve profitability and you may lose your investment.

There is currently no market for our common stock, and we cannot ensure that one will ever develop or be sustained.

There is currently no public market for our common stock. There can be no assurance that there will be an active market for our shares of common stock either now or in the future. If an active market is established, the market liquidity will be dependent on the perception of our operating business, among other things. We will take certain steps including utilizing investor awareness campaigns, press releases, road shows and conferences to increase awareness of our business and any steps that we might take to bring us to the awareness of investors may require we compensate consultants with cash and/or stock. There can be no assurance that there will be any awareness generated or the results of any efforts will result in any impact on our trading volume. Consequently, investors may not be able to liquidate their investment or liquidate it at a price that reflects the value of the business and trading may be at an inflated price relative to the performance of our company due to, among other things, availability of sellers of our shares. If a market should develop, the price may be highly volatile. Because there may be a low price for our shares of common stock, many brokerage firms or clearing firms may not be willing to effect transactions in the securities or accept our shares for deposit in an account. Even if an investor finds a broker willing to effect a transaction in the shares of our common stock, the combination of brokerage commissions, transfer fees, taxes, if any, and any other selling costs may exceed the selling price. Further, many lending institutions will not permit the use of low-priced shares of common stock as collateral for any loans.

We are subject to the reporting requirements of federal securities laws, and compliance with such requirements can be expensive and may divert resources from other projects, thus impairing our ability to grow.

We are subject to the information and reporting requirements of the Securities and Exchange Act of 1934, as amended (the “Exchange Act”), and other federal securities laws, including compliance with the Sarbanes-Oxley Act of 2002 (the “Sarbanes-Oxley Act”) and the Dodd-Frank Act Wall Street Reform and Consumer Protection Act of 2010 (the “Dodd-Frank Act”). The costs of preparing and filing annual and quarterly reports, proxy statements and other information with the Securities and Exchange Commission and furnishing audited reports to stockholders will cause our expenses to be higher than they would have been if we were privately held.

It may be time consuming, difficult, and costly for us to develop, implement and maintain the internal controls and reporting procedures required by the Sarbanes-Oxley Act and the Dodd-Frank Act. We may need to hire additional financial reporting, internal controls, and other finance personnel in order to develop and implement appropriate internal controls and reporting procedures.

If we fail to establish and maintain an effective system of internal control, we may not be able to report our financial results accurately or to prevent fraud. Any inability to report and file our financial results accurately and timely could harm our reputation and adversely impact the trading price of our common stock.

Effective internal control is necessary for us to provide reliable financial reports and prevent fraud. If we cannot provide reliable financial reports or prevent fraud, we may not be able to manage our business as effectively as we would if an effective control environment existed, and our business and reputation with investors may be harmed. As a result, our small size and any current internal control deficiencies may adversely affect our financial condition, results of operation and access to capital. Because of its inherent limitations, internal control over financial reporting may not prevent or detect misstatements. Projections of any evaluation of effectiveness to future periods are subject to the risk that controls may become inadequate because of changes in conditions, or that the degree of compliance with any policies and procedures may deteriorate.

Public company compliance may make it more difficult to attract and retain officers and directors.

The Sarbanes-Oxley Act and rules implemented by the Securities and Exchange Commission have required changes in corporate governance practices of public companies. As a public company, we expect these rules and regulations to increase our compliance costs in 20202021 and beyond and to make certain activities more time consuming and costly. As a public company, we also expect that these rules and regulations may make it more difficult and expensive for us to obtain director and officer liability insurance and we may be required to accept reduced policy limits and coverage or incur substantially higher costs to obtain the same or similar coverage. As a result, it may be more difficult for us to attract and retain qualified persons to serve on our board of directors or as executive officers, and to maintain insurance at reasonable rates, or at all.

Our stock price may be volatile.

If a market for our common stock is ever established, the market price of our common stock is likely to be highly volatile and could fluctuate widely in price in response to various factors, many of which are beyond our control, including the following:

In addition, the securities markets have from time to timetime-to-time experienced significant price and volume fluctuations that are unrelated to the operating performance of particular companies. These market fluctuations may also materially and adversely affect the market price of our common stock.

Our common stock may be deemed a “penny stock,” which would make it more difficult for our investors to sell their shares.

Our common stock may be subject to the “penny stock” rules adopted under Section 15(g) of the Exchange Act. The penny stock rules generally apply to companies whose common stock is not listed on the NASDAQ Stock Market or other national securities exchange and trades at less than $4.00 per share, other than companies that have had average revenue of at least $6,000,000 for the last three years or that have tangible net worth of at least $5,000,000 ($2,000,000 if the company has been operating for three or more years). These rules require, among other things, that brokers who trade penny stock to persons other than “established customers” complete certain documentation, make suitability inquiries of investors and provide investors with certain information concerning trading in the security, including a risk disclosure document and quote information under certain circumstances. Many brokers have decided not to trade penny stocks because of the requirements of the penny stock rules and, as a result, the number of broker-dealers willing to act as market makers in such securities is limited. If we remain subject to the penny stock rules for any significant period, it could have an adverse effect on the market, if any, for our securities. If our securities are subject to the penny stock rules, investors will find it more difficult to dispose of our securities.

FINRA sales practice requirements may also limit a stockholder’s ability to buy and sell our stock.

In addition to the “penny stock” rules promulgated by the Commission, FINRA has adopted rules that require that in recommending an investment to a customer, a broker-dealer must have reasonable grounds for believing that the investment is suitable for that customer. Prior to recommending speculative low-priced securities to their non-institutional customers, broker-dealers must make reasonable efforts to obtain information about the customer’s financial status, tax status, investment objectives and other information. Under interpretations of these rules, FINRA believes that there is a high probability that speculative low-priced securities will not be suitable for at least some customers. The FINRA requirements make it more difficult for broker-dealers to recommend that their customers buy our Common Stock, which may limit your ability to buy and sell our stock.

Our auditor indicated that certain factors raise substantial doubt about our ability to continue as a going concern.

We are a startup and our ability to survive as a going concern is not assured. As of March 31, 20212022 we have only $115 $224 cash; our net lossaccumulated deficit from December 2, 2016 inception to March 31, 20212022 is $244,203. $293,822. Our ability to continue as a going concern is dependent upon our ability to generate future profitable operations and/or to obtain the necessary financing to meet our obligations for our normal business operations when they come due. Management’s plan to address our ability to continue as a going concern includes: (1) obtaining debt or equity funding from private placement or institutional sources; (2) obtaining loans from financial institutions, where possible, or (3) participating in joint venture transactions with third parties. Although management believes that it will be able to obtain the necessary funding to allow us to remain a going concern through the methods discussed above, there can be no assurances that such methods will prove successful. The accompanying financial statements do not include any adjustments that might result from the outcome of this uncertainty.

Our officers and directors control a significant percentage of our current outstanding common stock, and their interests may conflict with those of our stockholders.

As of the date of this prospectus, our executive officers and directors collectively and beneficially own all the issued and outstanding common stock. If we sell all the 3,000,000 shares in the Primary Offering and the Selling Stockholders sell all the 300,000 shares of the Secondary Offering registered herein, there will be 136,033,333 shares issued and outstanding, consisting of the 133,033,333 shares held by Ramirez and Ogele and 3,300,000 shares in public hands. This concentration of voting control, including the Company’s ability to issue more shares, gives our executives and directors substantial influence over any matters which require a stockholder vote, including without limitation the election of directors and approval of merger and/or acquisition transactions, even if their interests may conflict with those of other stockholders. It could have the effect of delaying or preventing a change in control or otherwise discouraging a potential acquirer from attempting to obtain control of us. This could have a material adverse effect on the market price of our common stock or prevent our stockholders from realizing a premium over the then prevailing market prices for their shares of common stock. See also Security Ownership of Certain Beneficial Owners and Management”.Management.”

Our Offering is being conducted on a “best efforts” basis and does not require a minimum amount to be raised. As a result, we may not be able to raise enough funds to fully implement our business plan and our investors may lose their entire investment.

The Offering is on a “best efforts” basis and does not require a minimum amount to be raised. If we are not able to raise sufficient funds, we may not be able to fund our operations as planned, and our growth opportunities may be materially adversely affected. This could increase the likelihood that an investor may lose their entire investment.

We have broad discretion in how we use the net proceeds of this Offering, and we may not use these proceeds effectively or in ways with which you agree.

Our management will have broad discretion as to the application of the net proceeds of this Offering and could use them for purposes other than those contemplated at the time of this Offering. Our stockholders may not agree with the manner in which our management chooses to allocate and spend the net proceeds. Moreover, our management may use the net proceeds for corporate purposes that may not increase the market price of our Common Stock.

Although we may ultimately engage underwriters for the Offering, for the moment, we plan to sell the shares of this Offering without an underwriter and may be unable to sell any shares.

This Offering is “self-underwritten” meaning we intend to sell it ourselves through our officers, directors, and employees under Rule 3a4-1 of the Securities Exchange Act of 1934. However, we will not receive any sales commission for our sales efforts. In addition, the offering will be conducted on a “best efforts” basis meaning we would do our best to sell it.Since this is a “best efforts” endeavor, there is no guarantee that we will be able to sell any of the shares. Unless we are successful in selling all of the shares in this Offering, we may have to seek alternative financing to implement our business plan. Nevertheless, we reserve the right to offer the stocks through broker-dealers who are registered with the Financial Industry Regulatory Authority (“FINRA”). As of the date of this Registration Statement, no selling agreements had been entered into by us with any broker-dealer firms.

We will incur ongoing costs and expenses for Commission reporting and compliance. Without sufficient funds, we may not be able to remain in compliance, making it difficult for investors to sell their shares, if at all.

We estimate our total offering costs to be $100,000 in legal fees and accounting costs. If we experience a shortage of funds prior to funding, Mr. Jimmy Ramirez has agreed to loan us money to pay for offering costs, filing fees, and professional fees and correspondence with our shareholders. The loan amount may not exceed $100,000. Mr. Ramirez has already advanced $51,852 to us. Mr. Ogele has also advanced us $15,166. In addition, Global Mortgage Banking, a company owned by Mr. Ramirez, loaned us $2,050.00 under similar terms. Loan agreements are filed as Exhibit 10.2 to this Registration Statement. In order for us to remain in compliance with the filing requirements, including annual, quarterly, and current reports, or other information with the Commission as provided by the Exchange Act, we will require funds to cover the cost of these filings, which could comprise a substantial portion of our available cash resources. If we are unable to generate sufficient revenues or raise sufficient capital to remain in compliance, we may have to curtail our business plan and it may be difficult for you to resell any shares you may purchase, if at all.

There presently no market for our common stock.

We are not registered on any market or public stock exchange. There is presently no demand for our common stock and no public market exists for the shares being offered in this prospectus. We plan to contact a market maker immediately following the completion of the offering and apply to have the shares quoted on the OTCBB. The OTCBB is a regulated quotation service that displays real-time quotes, last sale prices and volume information in over-the-counter securities. The OTCBB is not an issuer listing service, market, or exchange. Although the OTCBB does not have any listing requirements, to be eligible for quotation on the OTCBB, issuers must remain current in their filings with the SEC or applicable regulatory authority. If we are not able to pay the expenses associated with our reporting obligations, we will not be able to apply for quotation on the OTCBB. Market makers are not permitted to begin quotation of a security whose issuer does not meet this filing requirement. Securities already quoted on the OTCBB that become delinquent in their required filings will be removed following a 30 to 60 day30-to-60-day grace period if they do not make their required filing during that time. We cannot guarantee that our application will be accepted or approved, and our stock listed and quoted for sale. As of the date of this filing, there have been no discussions or understandings between us and anyone acting on our behalf, with any market maker regarding participation in a future trading market for our securities. If no market is ever developed for our common stock, it will be difficult for you to sell any shares you purchase in this offering. In such a case, you may find that you are unable to achieve any benefit from your investment or liquidate your shares without considerable delay, if at all. In addition, if we fail to have our common stock quoted on a public trading market, your common stock will not have a quantifiable value and it may be difficult, if not impossible, to ever resell your shares, resulting in an inability to realize any value from your investment.

Because the offering price has been arbitrarily set by the Company, you may not realize a return on your investment upon resale of your shares.

The offering price and other terms and conditions relative to the Company’s shares have been arbitrarily determined by us and do not bear any relationship to assets, earnings, book value or any other objective financial criteria. Additionally, as the Company was formed only in December 2016 and has only a limited operating history with no earnings, the price of the offered shares is not based on its past earnings, and no investment banker, appraiser, or other independent third party, has been consulted concerning the offering price for the shares or the fairness of the offering price used for the shares, as such our stockholders may not be able to receive a return on their investment when they sell their shares of common stock.

The Company’s investors may suffer future dilution due to issuances of shares for various considerations in the future.

Our Articles of Incorporation authorizes the issuance of 600,000,000 shares of common stock, par value $0.0001 per share. If we sell the 3,000,000 shares being offered in this offering, and the 300,000 shares being offered by the Selling Stockholders, we will have 136,033,333 shares issued and outstanding consisting of 133,033,333 shares held by Ramirez and Ogele and 3,300,000 shares in public hands. Additionally, the Company has entered into a Shareholders Agreement pursuant to which Ramirez and Ogele would always own the Company on 85%:15% pro rata basis. The issuance of common stock for future services or acquisitions or other corporate actions may have the effect of diluting the value of the shares held by our investors and might have an adverse effect on any trading market for our common stock. See “Dilution”. “Dilution.” See also Security Ownership of Certain Beneficial Owners and Management.

Offers or availability for sale of a substantial number of shares of our common stock may cause the price of our common stock to decline.

Our stockholders could sell substantial amounts of common stock in the public market, including shares sold upon the filing of a registration statement that registers such shares and/or upon the expiration of any statutory holding period under Rule 144 of the Securities Act of 1933 (the “Securities Act”), if available, or upon the expiration of trading limitation periods. Such volume could create a circumstance commonly referred to as a market “overhang” and in anticipation of which the market price of our common stock could fall. Additionally, we have a large number of warrants that are presently exercisable. The exercise of a large amount of these securities followed by the subsequent sale of the underlying stock in the market would likely have a negative effect on our common stock’s market price. The existence of an overhang, whether or not sales have occurred or are occurring, also could make it more difficult for us to secure additional financing through the sale of equity or equity-related securities in the future at a time and price that we deem reasonable or appropriate.

Our directors and officers have rights to indemnification.

Our Amended Certificate of incorporation and Bylaws provide, as permitted by governing Delaware law, that we will indemnify our directors, officers, and employees whether or not then in service as such, against all reasonable expenses actually and necessarily incurred by him or her in connection with the defense of any litigation to which the individual may have been made a party because he or she is or was a director, officer, or employee of the company. The inclusion of these provisions in the Bylaws may have the effect of reducing the likelihood of derivative litigation against directors and officers and may discourage or deter stockholders or management from bringing a lawsuit against directors and officers for breach of their duty of care, even though such an action, if successful, might otherwise have benefited us and our stockholders.

Insofar as indemnification for liabilities arising under the Securities Act may be permitted to our directors, officers or persons controlling us under the foregoing provisions, we have been informed that, in the opinion of the SEC, such indemnification is against public policy as expressed in the Securities Act and is therefore unenforceable.

Additionally, although our bylaws designate the Court of Chancery of the State of Delaware as exclusive forum for adjudication, including certain litigation and derivative action, such provisions do not preclude the exclusive jurisdiction of the federal courts over all suits brought to enforce any duty or liability created by the Exchange Act of 1934 or the rules and regulations thereunder, thereunder,nor the concurrent jurisdiction of federal and state courts over all such matters under Section 22 of the Securities Act of 1933. Moreover, the forum selection provisions in our Bylaws does not apply to actions arising under the Securities Act or the Exchange Act. See Bylaws of Wall Street Acquisitions Corp.

We do not anticipate paying any cash dividends on our common stock.

We do not anticipate paying cash dividends on our common stock for the foreseeable future. The payment of dividends, if any, would be contingent upon our revenues and earnings, if any, capital requirements, and general financial condition. The payment of any dividends will be within the discretion of our Board of Directors. We presently intend to retain all earnings, if any, to implement our business strategy; accordingly, we do not anticipate the declaration of any dividends in the foreseeable future.

CAUTIONARY NOTE REGARDING FORWARD-LOOKING STATEMENTS

This prospectus, including information included or incorporated by reference in this prospectus or any supplement to this prospectus, may contain forward-looking statements within the meaning of the Private Securities Litigation Reform Act of 1995. These forward-looking statements include, but are not limited to, statements about our plans, objectives, expectations, and intentions that are not historical facts, and other statements identified by words such as “may,” “will,” “expects,” believes,” “plans,” “estimates,” “potential,” or “continue,” or the negative thereof or other and similar expressions are forward-looking statements. In addition, in some cases, you can identify forward-looking statements by words of phrases such as “trend,” “potential,” “opportunity,” “believe,” “comfortable,” “expect,” “anticipate,” “current,” “intention,” “estimate,” “position,” “assume,” “outlook,” “continue,” “remain,” “maintain,” “sustain,” “seek,” “achieve,” and similar expressions. These forward lookingforward-looking statements are based on current beliefs and expectations of management and are inherently subject to significant business, economic and competitive uncertainties, and contingencies, many of which are beyond our control. In addition, these forward-looking statements are subject to assumptions with respect to future business strategies and decisions that are subject to change. In addition to the factors set forth in this prospectus the following factors, among others, could cause actual results to differ materially from the anticipated results: commodities prices; our ability to raise or access capital; general economic or industry conditions, nationally and/or in the communities in which our company conducts business; changes in the interest rate environment; legislation or regulatory requirements; conditions of the securities markets; changes in accounting principles, policies or guidelines; financial or political instability; acts of war or terrorism; and other economic, competitive, governmental, regulatory and technical factors affecting our operations, products and prices. All forward-looking statements speak only as of the date of this prospectus or, in the case of any documents incorporated by reference in this prospectus, the date of such document, in each case based on information available to us as of such date, and we assume no obligation to update any forward-looking statements, except as required by law.

USE OF PROCEEDS

Our public offering of 3,000,000 is being made on a self-underwritten basis: no minimum number of shares must be sold in order for the offering to proceed. The net proceeds from the 3,000,000 shares offered herein at a price fixed at $7.00 per share, which will go the Company, will vary depending upon the total number of shares sold. Regardless of the number of shares sold, we expect to incur offering expenses estimated at $100,000 for legal, accounting, printing, and other costs in connection with this offering. We will not receive any proceeds from the sale of 300,000 shares by the Selling Stockholders. We will not maintain an escrow account for the receipt of proceeds from the sale of our shares. Proceeds of the 3,000,000 shares will go directly to the Company’s operating account.

The following table sets forth the uses of proceeds from the primary offering would be used assuming the sale of 25%, 50%, 75% and 100%, respectively, of the securities offered for sale by the Company. There is no assurance that we will raise the full $21,000,000 as anticipated.

The above figures represent only estimated costs. All proceeds will be deposited into our corporate bank account. Any funds that we raise from our offering of 3,000,000 shares will be deposited in a Company bank account immediately available for our use and will not be returned to investors. We do not have any arrangements to place the funds received from the 3,000,000 shares in an escrow, trust, or similar account. Accordingly, if we file for bankruptcy protection or a petition for involuntary bankruptcy is filed by creditors against us, your funds will become part of the bankruptcy estate and administered according to the bankruptcy laws. If a creditor sues us and obtains a judgment against us, the creditor could garnish the bank account and take possession of the subscriptions. As such, it is possible that a creditor could attach your subscription. If that happens, you will lose your investment and your funds will be used to pay creditors.

DETERMINATION OF OFFERING PRICE

We have arbitrarily determined the offering price of the 3,000,000 shares being offered by the Company. The price was arbitrarily determined by us and does not bear any relationship to any objective criterion of value. In determining the number of shares to be offered and the offering price, we took into consideration the amount of money we would need to implement our business plan. Accordingly, the offering price should not be considered an indication of the actual value of the securities. We will not receive any of the proceeds from the sale of the 300,000 common shares being offered for sale by the Selling Stockholders. The Selling Stockholders will sell their shares at a fixed price of $7.00 per share for the duration of the offering until such time as our common stock may be listed on a national securities exchange or quoted on the OTCBB.

SELLING STOCKHOLDERS

The common shares being offered for resale by the two Selling Stockholders consists of 300,000 shares of our common stock, $0.0001 par value. The following table sets forth the shares beneficially owned, as of the date of this prospectus, by the Selling Stockholders, as well as the number of shares each Selling Stockholder is offering by this prospectus and the number of shares which each would own beneficially if all such offered shares are sold. Until such time as any market for our common stock exists on a national securities exchange, the OTCBB, the Selling Stockholders will be offering the Secondary Offering shares of common stock at the fixed price of $7.00 per share. At such time as our shares are listed on a national securities exchange or quoted on the OTCBB, the Selling Stockholders may offer and sell their shares of common stock at prevailing market prices or at privately negotiated prices. The Company will not receive any of the proceeds from the sale of shares by the Selling Stockholders. No underwriting arrangements have been entered into by any of the Selling Stockholders.

Beneficial ownership is determined in accordance with SEC rules. Under these rules, a person is deemed to be a beneficial owner of a security if that person has or shares voting power, which includes the power to vote or direct the voting of the security, or investment power, which includes the power to vote or direct the voting of the security. The person is also deemed to be a beneficial owner of any security of which that person has a right to acquire beneficial ownership within 60 days. Under SEC rules, more than one person may be deemed to be a beneficial owner of the same securities, and a person may be deemed to be a beneficial owner of securities as to which he or she may not have any pecuniary beneficial interest. Except as noted below, each person has sole voting and investment power.

The percentages below are calculated based on 133,333,333 shares of our common stock issued and outstanding as of the date of this prospectus. We do not have any outstanding options, warrants or other securities exercisable for or convertible into shares of our common stock.

DILUTION OF THE PRICE YOU PAY FOR YOUR SHARES

Dilution shows the difference between the price at the time of the offering and the net tangible book value per share immediately after completion of this offering.

Net tangible book value is the amount that results from subtracting total liabilities and intangible assets from total assets. Dilution arises mainly as a result of our arbitrary determination of the offering price of the shares being offered. Dilution of the value of the shares you purchase is also a result of the lower book value of the shares held by our existing stockholders.

As of March 31, 2021,2022, the net tangible book value of our shares was ($241,970)266,374) or approximately $(0.0018)$(0.0019) per share, based upon 133,333,333 shares outstanding.

The table below represents the dilution per share to the new investors. However, it does not give any effect to the results of any operations after March 31, 2021.2022. The following table shows the per share dilution assuming that 50%, 75% and 100% of the shares respectively of the primary Offering by the Company is sold.

DILUTION TABLE

If we sell only 25% of the offering, the book value of your $7.00 per share purchase will be worth only $0.0326$0.0344 meaning that you would absorb ($6.9683)6.9656) in net dilution; if we sell 50% of the offering, the book value of your $7.00 per share purchase would be worth $0.0675$0.0673 meaning that you would absorb ($6.9375)6.9327) in net dilution; if we sell 75% of the offering, the book value of your per share purchase would be worth $0.1020$0.1018 meaning that you would absorb ($6.8980)6.8982) in net dilution and if we sell the entire 100% of the offering, the book value of your $7.00 per share purchase would be worth $0.1367$0.1365 meaning that you would absorb ($6.8633)6.8635) in net dilution.

MANAGEMENT’S DISCUSSION AND ANALYSIS OF FINANCIAL CONDITIONAND RESULTS OF OPERATION

You should read the following discussion and analysis of our financial condition and results of operations together with our consolidated financial statements and the related notes and other financial information included elsewhere in this prospectus. Some of the information contained in this discussion and analysis or set forth elsewhere in this prospectus, including information with respect to our plans and strategy for our business and related financing, includes forward-looking statements that involve risks and uncertainties. You should review the “Risk Factors” section of this prospectus for a discussion of important factors that could cause actual results to differ materially from the results described in or implied by the forward-looking statements contained in the following discussion and analysis.

Wall Street Acquisitions Corp was incorporated in the State of Delaware on December 2, 2016. On February 24, 2017, the Company filed a Form 10-12G pursuant to the Exchange Act of 1934 to register 20,000,000 shares of common stock. On September 17, 2019, the Company acquired, in a stock-for-stock exchange transaction, all the issued and outstanding shares of WSA Gold & Minerals, Inc., a Texas corporation (“WSA Gold”). WSA Gold is the owner of various mining properties in Nevada, New Mexico, and Arizona. In the stock-for-stock exchange transaction, 85% of the Company’s shares was retained by Mr. Ramirez, President, and sole shareholder of WSA Gold while Mr. Ogele retained 15% interest in the Company which allocation is memorialized in the Shareholders Agreement. Mr. Ogele also stepped down as President and Director of the Company and Mr. Ramirez was elected President, CEO and Director of the Company. We plan to enter into the gold mining space through the exploitation of the mining properties in Nevada, New Mexico, and Arizona. On April 27 2020, the Company amended the Certificate of Incorporation raising the authorized common stock to 600,000,000 shares at $.0001 par value. We are in the excavation stage of our planned mining operations. See Share Purchase and Merger Agreement.

We qualify as an “emerging growth company” under the JOBS Act. As a result, we are permitted to, and intend to, rely on exemptions from certain disclosure requirements. For so long as we are an emerging growth company, we will not be required to:

●have an auditor report on our internal controls over financial reporting pursuant to Section 404(b) of the Sarbanes-Oxley Act;

In addition, Section 107 of the JOBS Act also provides that an emerging growth company can take advantage of the extended transition period provided in Section 7(a)(2)(B) of the Securities Act for complying with new or revised accounting standards. In other words, an emerging growth company can delay the adoption of certain accounting standards until those standards would otherwise apply to private companies. We have elected to take advantage of the benefits of this extended transition period. Our financial statements may therefore not be comparable to those of companies that comply with such new or revised accounting standards.

We will remain an “emerging growth company” for up to five years, or until the earliest of (i) the last day of the first fiscal year in which our total annual gross revenues is $1 billion, (ii) the date that we become a “large accelerated filer” as defined in Rule 12b-2 under the Securities Exchange Act of 1934, which would occur if the market value of our ordinary shares that is held by non-affiliates is $700 million as of the last business day of our most recently completed second fiscal quarter or (iii) the date on which we have issued more than $1 billion in non-convertible debt during the preceding three year period.

Our cash balance is $115$224 as of March 31, 2021.2022. We believe our cash balance is not sufficient to fund our operations for any period of time. We have been utilizing and may utilize funds from Mr. Jimmy Ramirez, who has agreed to loan us money to pay for offering costs, filing fees, and professional fees. The loan amount may not exceed $100,000. Mr. Ramirez has already advanced $51,852 to us. Mr. Ogele has also advanced us $15,166. In addition, Global Mortgage Banking, a company owned by Mr. Ramirez, loaned us $2,050.00 under similar terms. Loan agreements are filed as Exhibit 10.2 to this Registration Statement. In order to fully implement our plan of operations during the next twelve months, we require a minimum of $21,000,000 of funding from this offering. Being a start-up company, we have very limited operating history we do not currently have any arrangements for additional financing. Our principal executive offices are located at 4440 S. Piedras Drive, Suite 136,205, San Antonio, TX 78228. Our phone number is 210-468-5356.

Our independent registered public accountant has issued a going concern opinion. This means that there is substantial doubt that we can continue as an on-going business for the next twelve months unless we obtain additional capital to pay our bills. This is because we have not generated sufficient revenues and no significant revenues are anticipated until we complete our initial business development. There is no assurance we will ever reach that stage.

To meet our need for cash we are attempting to raise money from this offering. If we are unable to successfully find customers, we may quickly use up the proceeds from this offering and will need to find alternative sources. At the present time, we have not made any arrangements to raise additional cash, other than through this offering.

If we need additional cash and cannot raise it, we will either have to suspend operations until we do raise the cash or cease operations entirely. Even if we raise $21,000,000 from this offering, we may need more funds for ongoing business operations after the first year and would have to obtain additional funding in the form debt or equity financing.

Plan of Operations

We plan to engage in mining activities and have not yet generated or realized any revenues from our business. We own fee simple title/deed to ten (10) mines located in Nevada, New Mexico, and Arizona. During the 12 months following the date of this prospectus, we will be focused on publicly selling our shares of common stock being offered hereunder in order to raise $21,000,000 to commence mining operations. We have no assurance that future financing will materialize. If that financing is not available, we may be unable to continue. Management believes that if the public offering of 3,000,000 shares under this prospectus is successful, we still may not be able to generate sales revenue within the following 12 months thereof. Therefore, if such public financing is not available, we could fail to satisfy our future cash requirements.

If we are unsuccessful in raising the additional proceeds through the public offering under this prospectus, we will then have to seek additional funds through a private placement offering or debt financing, which would be highly difficult for a new exploration stage company to secure. Therefore, the Company is highly dependent upon the success of the anticipated public offering under this prospectus and failure thereof would result in the Company having to seek capital from other sources such as debt financing, which may not even be available to the Company. However, if such financing were available, because we are aan exploration stage company with no operations to date, we would likely have to pay additional costs associated with high riskhigh-risk loans and be subject to an above market interest rate. At such time as these funds are required, management would evaluate the terms of such debt financing and determine whether the business could sustain operations and growth and manage the debt load. If we cannot raise additional proceeds via a private placement of our common stock or secure debt financing we would be required to cease business operations. As a result, investors in our common stock would lose all of their investment.

If we fail to complete the offering, we may have to cease our operations. As of March 31, 2021,2022, we had a working capital deficiency of $241,970.$266,374.

The Company’s project is broken down into 4 phases: Planning, implementation, production, and closure. The Company is currently in the planning phase where conceptual studies have been conducted and pre-feasibility studies are underway. Currently the Company has topographic maps, preliminary maps displaying claim boundaries, purchased claims, conducted site visits, and started geologic studies by conducting surface samples and mapping of major structures along with surface deposits of 23 minerals. Research and press releases by offset mines and historical geological findings have been reviewed and incorporated into the decision making. The next step will be a feasibility study where more field data will be collected, analyzed, and used to move to the next phase of the project. Design a safe, environmentally sound, and economically viable plan for the extraction of minerals. The Implementation phase will take all previously assembled data and finalize all previous plans before construction begins. Equipment will be purchased, and processing plant will be built and tested. During the Production phase ore will be processed commercially. Staff will be ramped up and improvements will be made to the process as data is collected. During the closure phase all environmental concerns will be addressed before abandonment.

Initial plans include drilling a minimum of 8 bore holes to collect core samples to a depth of 400’. The projected timeline will be 12 months from initial funding to allow for permitting, construction of drill pads and the drilling of core. Analysis of samples will take an additional 3 months and will be conducted by multiple groups. Just Refiners Inc will analyze core samples and develop an efficient and economic system for mineral extraction. Just Refiners (USA) Inc was incorporated in 1993. Just Refiners is situated in Sparks, Nevada and is currently expanding into processing spent carbon in house. The main core of Just Refiners is to provide a service to the mining industry by receiving, preparing, sampling, and processing their by-product materials. CJHx4 Consulting will have geologist oversee coring program and log core. CJHx4 Consulting was established in 2014 and has assisted clients in both mining and hydrocarbon exploration. Two independent assay labs will be used to compare core samples. Drilling will be conducted by Boart Longyear with over 130 years in the drilling industry. The coring project is budgeted at $2.5M and will include all 10 claims in the Tonopah, NV mining district.

After completion of the coring project, an additional 2 years will be spent updating geologic database, improving geologic models, and collecting geotechnical data from core samples for use in mine design. Environmental Studies and permitting will take 24 months with an expected costs of $200,000. Additional resources will be used for equipment planning and optimization. A centralized facility would be optimal due to close proximity of claims. Geologic work will be carried out by CJHx4 Consulting, other work will be carried out by various engineering firms on an as needed basis. Estimated budget is $1,800,000.

Once all feasibility studies have been completed, the Company will move to the implementation phase and work on final mine design and begin construction. The timeline and budget of this will depend on results from the feasibility studies conducted in the planning phase and exploratory drilling. Due to the size, cost of processing equipment and layout the cost are expected to be high. Lastly the mines will move into the production phase and start operations.

Results of Operations

Fiscal year ended December 31, 2020,2021, compared to fiscal year ended December 31, 2019.2020.

We did not earn revenues for the years ended December 31, 2020,2021, and December 31, 2019.2020.

For year-ended December 31, 2020,2021, our operating expenses was $58,980.00$19,899 compared to $138,518.00$58,980 as of year ended December 2019.2020. For December 31, 20202021, our professional fees for the National Instruments 43-101 Technical Report was $53,957.00$17,400 compared to $130,462.00$53,958 for year ended December 2019.2020. For year ended December 31, 2020,2021, we had a net loss of $58,980.00$19,899 or $0.00044$0.00015 loss per shares compared to $138,518.00$58,980 loss for year ended December 2019 or $0.00104$0.0044 per share.

For period ended March 31, 2021,2022, our operating expenses stood at $6,620,$60,207, compared to $7,612$6,620 as of June 2020March 31, 2021 and our net loss was ($7,612)60,207) or $0.00006$0.00045 loss per share, compared to $14,232$-0- on June 30, 2020March 31, 2021 net loss or $0.00011$0.00 loss per share.

Limited Business History; Need for Additional Capital

There is limited historical financial information about the Company upon which to base an evaluation of our performance. We are aan exploration stage corporation and have not generated any revenues from our business. We cannot guarantee that we will be successful in our business plans. Our business is subject to risks inherent in the establishment of a mining business enterprise, including limited capital resources, possible delays in the commencement of mining operations and possible cost overruns due to price and cost increases in services. We have no intention of entering into a merger or acquisition within the next 12 months and we have a specific business plan and timetable to complete our 12-month plan of operation based on the success of the primary offering.

We anticipate that additional funding, if required, will be in the form of equity financing from the sale of our common stock. However, we cannot provide investors with any assurance that we will be able to raise sufficient funding from the sale of shares to fund additional expenditures. We do not currently have any arrangements in place for any future equity financing. Our limited operating history makes it unlikely that we will be able to obtain significant debt financing in the near future. If such financing is not available on satisfactory terms, we may be unable to continue or expand our business. Equity financing could result in additional dilution to existing shareholders.

If we raise the $21,000,000 gross proceeds, in the primary offering, we believe that we can pay for our offering expenses and satisfy our cash requirements to complete our 12-month plan of operation without having to raise additional funds for the next twelve months.

Our cash balance is not sufficient to fund our operations for any period of time. We have been utilizing and may utilize funds from Mr. Ramirez who has agreed to loan us money to pay for offering costs, filing fees, and professional fees. The loan amount may not exceed $100,000. As of March 31, 20212022 Mr. Ramirez has already advanced $51,852 to us, while Mr. Ogele has advanced us $15,166. In addition, Global Mortgage Banking, a company owned by Mr. Ramirez, loaned us $2,050.00 under similar terms. Loan agreements are filed as Exhibit 10.2 to this Registration Statement. In order to implement our plan of operations for the next twelve-month period, we require a minimum of $21,000,000 of funding from this offering.

Liquidity and Capital Resources

AtOn December 31, 2019,2021, we had a cash balance of $1,000.00,$241, total current assets $19,430.00,$241, total current liabilities of approximately $171,933.00$231,028; working capital deficiency of $152,503.00$212,357 and accumulated deficit of approximately $154,736.00. At$233,615. On December 31, 2020, we had a cash balance of $115.00, total current assets $18,545.00,$115, total current liabilities of approximately $230,028.00,$230,028, working capital deficiency of $211,483.00$211,483 and accumulated deficit of approximately $213,716.00.$213,716. For period ended March 31, 20212022 we had a cash balance of $115,$224, total current assets $18,545,$224, total current liabilities of approximately $260,515,$285,028, working capital deficiency of $241,970$266,374 and accumulated deficit of approximately $244,203.$293,822. We do not have sufficient cash on hand to commence our 12-month plan of operation or to fund our ongoing operational expenses. We will need to raise funds to commence our plan of operation and fund our ongoing operational expenses. Additional funding will likely come from equity financing from the sale of our common stock or debt securities. If we are successful in completing an equity or debt financing, existing shareholders will experience dilution of their interest in our Company. We do not have any financing arranged and we cannot provide investors with any assurance that we will be able to raise sufficient funding from the sale of our common stock or debt securities to fund our planned activities and ongoing operational expenses. In the absence of such financing, our business will likely fail. There are no assurances that we will be able to achieve further sales of our common stock or any other form of additional financing. If we are unable to achieve the financing necessary to continue our plan of operations, then we will not be able to continue our operations and our business will fail.

Summary of Significant Accounting Policies

Refer to Note 2 to the financial statements for a summary of the Company’s significant accounting policies.

Our Properties

Our principal offices are located at our principal office is located at 4440 S. Piedras Drive, Suite 136,205, San Antonio, Texas 78228. We do not currently lease or own any other real property. We intend to commence excavation of our mining properties with the funds raised in this Offering. See “Use of Proceeds”

We currently own titles/deeds to ten (10) mining properties: namely, Yellow Aster, Fat Mule Flats, Cobin, Jasper, Barracks Nine, Eclipse, Fortuna, Purple Heart, Blackmoor, and the New River Mine.

Mine 1 – Yellow Aster

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found the Yellow Aster Mine Property located in Tonopah, Nevada in Nye County.

The Probable Gross Gold Resources are 2,214,249.62 oz based on projected 200 feet excavation.

Yellow Aster Mine is a lode mine. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

The general course of this claim is North and South, and it is situated in the NE Quarter of Section 28, Township 3N, Range 42E, Mount Diablo Meridian, Nye County, Nevada. This claim is 600 feet in width and 1,500 feet in length. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in a Northerly direction to the North end line and approximately 300 feet in a Southerly direction to the South end line. This claim is marked by four (4) monuments, one at each corner of the claim. Additionally, there are two (2) end-line markers on each side of the center of the claim. All markers are 4” x 4” wooden posts that are buried 1.5’ in the ground and protrude 4.5’ above the ground embossed with the name of the claim and its location in relation to the claim.

The location monument on which this notice is posted is situated within Section 28, Township 3N, Range 42E, Mount Diablo Meridian, Nye County Nevada and this claim encompasses portions of the following quarter section (s), Township (s), and Range (s); NE 1/4 of NE 1/4, and SE 1/4 of NE 1/4 Section 28, T3N, R42E, Mount Diablo Meridian, Nye County Nevada. The locality of this claim with reference to some natural object or permanent monument and additional information (if any) concerning its locality are as follows: NE corner of this claim is 300 Feet West and 55 Feet South of the NE corner of Section 28, T3N, R42E, thence heads due South for 1,500 feet to the SE corner of this claim, thence due West for 600 feet to the SW corner of this claim, thence due North for 1,500 feet to the NW corner of this claim, thence due East 600 feet to the place of beginning, the NE corner.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMC1186294 in the NE Quarter of Section 28, Township 3N, Range 42E, Mount Diablo Meridian, Nye County, Nevada from Gateway Gold & Minerals, Inc.

Yellow Aster Mine

The property is almost entirely within the boundaries of the municipality of Tonopah Nevada. The property is readily accessible via Highway 95 from Las Vegas to the South or Hwy’s 95/6 from the North/West from Northern Nevada/Reno or Bishop California, and from Highway 6 from the east which intersects highway 95 in the heart of Tonopah. This mine can be accessed by dirt roads using an ATV (all-terrain vehicle) or four-wheel drive vehicle and a GPS, main dirt roads leading through the mining district are maintained, but two track roads to the individual mines are often difficult to traverse. Caution is mandatory within the entire valley as it is dotted with abandoned mines – some of them are easy to see from a distance, and other are impossible to see until you are right on top of them. 20% of them are roped or fenced off – the rest do not have safety barriers and one should be extremely careful in entering them. Being situated in the high desert there are limited water sources in the area throughout 10 months out of the year.

Tonopah is located slightly inboard of the western margin of the Basin and Range province, and on the eastern margin of the “Walker Lane”,Lane,” a zone of Miocene structural deformation trending northwest to southeast parallel to the trend of the Sierra Madre Mountains in Eastern California. The Walker Lane can best be characterized as a broad zone of abundant strike-slip right-stepping faulting. The trend of the pre-Tertiary geologic units over much of the Walker Lane exhibits an arcuate pattern as a result of the influence of two major structuralstructural regimes. A series of these arcs have been identified by past workers with the Tonopah area having been identified as being within the Silver Peak-Palmetto- Montezuma Oroflex (Albers & Stewart 1972). The oroflex is described as southward convex with bedding, fold axes and faults trending to the northwest in the Silver Peak Range, trending east-west in the Palmetto Mountains and swinging around to the Northeast in the Montezuma Peak region. The Tonopah area lies on the eastern limb of the oroflex. The Walker Lane is also noted as being particularly well endowed with mineral deposits and the coincidence of these two structural regimes has created favorable plumbing, which is responsible for the high frequency of deposits in the region.

To the west of Tonopah, the White Mountains represent the westernmost range of the central Basin and Range province. They are situated to the east of the unextended Sierra Nevada Range and represent a crustal block that is bounded along its western flank by the high-angle White Mountains fault zone, with up to 8 km of total dip-slip displacement. Miocene volcanic rocks preserved along the eastern side of the range unconformably overlie Mesozoic granitic basement and dip up to 25° to the east, tilting occurred in the middle Miocene. The early geology of the general Tonopah region is relatively simple with the earliest Cambrian and Precambrian rocks comprised primarily of distal maritime facies - limestones, and dolomites with some hornfelsed shales. These are in fault contact withwith Ordivician limestones, argillites, and shales. From this point in time forward things become increasingly complex due to extensive volcanism in possibly alternating terrestrial and lacustrine settings. None of the Cambrian or Precambrian rocks outcrop in the immediate Tonopah area but fragments of these lithologies are present in volcanic breccias locally, so it is believed they form the basement of the volcanic complex.

The local geology is extremely well documented with geological investigations going back as early as 1905 when Spurr first published his voluminous observations of the camp. Spurr continued his work in the camp well into the 1920’s, followed by Bastin and Laney (1918), and later Nolan in 1930 published a study of the mines in the western part of the camp, and later expanded on this work, publishing a study that encompassed the entire camp in 1935. Later work was done in the area by Bonham (1970) and Bonham & Garside (1974 & 1979) during the time that work was carried out by Summa, Tenneco, and Houston Oil and Minerals. The earlier workers in the area had the distinct advantage of having the bulk of the mine workings available at one time or another for inspection, while the later workers had the ability to draw from all the earlier well-documented work.

Given the nature of this primarily felsic volcanic center, and the considerable alteration that has taken place prior, during and possibly somewhat after the mineralizing events, the geology of the camp is quite complex, and deciphering the history of the geology and mineralization of the area is only possible due to the thorough the attention paid to detail and the recording of these findings by earlier workers.

The “Early” andesite of the Mizpah formation is almost exclusively the host rock for mineralization, however Bonanza style lode mineralization of the epoch does extend into the later andesite and in certain mines above the Mizpah into the Extension Breccia, the West End Rhyolitic intrusive and into the Fraction Tuff. From relative positioning and age dating it has been established that the earliest mineralizing event occurred between 20.5m.y. to 17m.y. before present.

The later mineralization event occurred around the end of the emplacement of the Fraction Tuff. At Three Hills the gold bearing discontinuous, irregular, narrow, brecciated chalcedony quartz veinlets, and stockworks occur in a zone of pervasive silicification of the Siebert Formation immediately above the contact with the Fraction Tuff. At Hasbrouck, some gold-silver mineralization is seen within the Fraction Tuff, near its contact with the overlying Siebert formation, which hosts the bulk of the gold- silver mineralized veinlet and stockwork deposits. These occur as erratic bodies of hydrothermal breccia accompanied by strong pervasive silicification with associated adularia and pyrite. Adularia associated with mineralization at the Divide deposit was dated at between 16.3 m.y. and 16.4 m.y. before present.

No significant exploration has been noted at these mines in a few decades so a historical account of publicly found data was assimilated. The Tonopah Mining District began circa 1900 with the discovery of gold and silver-rich ore by prospector Jim Butler when he went looking for a lost burro he owned. The burro had wandered off during the night and sought shelter near a rock outcropping. When Butler discovered the animal the next morning, he picked up a rock to throw at the beast, but instead noticed the rock was unusually heavy. He had stumbled upon the second-richest silver strike in Nevada history. While Butler may have been responsible for the first ore strike, it took men of wealth and power to consolidate the mines and reinvest their profits into the infrastructure of the town of Tonopah.

George Wingfield, a 24-year old24-year-old poker player when he arrived in Tonopah, played poker, and dealt faro in the town saloons. Once he had a small bankroll, he talked Jack Carey, owner of the Tonopah Club, into taking him in as a partner and to file for a gaming license. In 1903, miners rioted against Chinese workers in Tonopah, which spurred a boycott in China of U.S. goods. By 1904, after investing his winnings in the Boston-Tonopah Mining Company, Wingfield was worth $2 million. When old friend George S. Nixon, a banker, arrived in town, Wingfield invested in his Nye County Bank. They grub staked miners with friend Nick Abelman, bought existing mines, and by the time the partners moved to Goldfield, Nevada and made their Goldfield Consolidated Mining Company a public corporation in 1906, , Nixon and Wingfield were worth over $30 million. Small mining ventures continue to this day to provide income for local miners.

The discovery and development of the Tonopah area can be separated into four periods. From 1900 to 1903 the various participants acquired their ground and commenced development work by sinking shafts to access the ore. Between 1903 and 1907 development continued and better and more efficient equipment was deployed to increase production. The recession of 1907 to 1910 caused production to drop off as only the higher-grade ore could be profitably mined with silver prices dropping to as low as $0.25/oz. During this period many of the weaker companies went out of business and consolidation of claims occurred. The high point of the Tonopah camp occurred between 1910 and 1930 with production peaking around 1918 at 622,364 tons/year, with a recorded value of $9,311,560,, and declining steadily through the 1920’s.

Production came to a halt with the exception of leasehold mining in the 30’s due to the depression and low precious metals prices. There was virtually no activity during the war in the 40’s but there was somewhat of a resurgence of activity in the 50’s. In total the Tonopah area produced in the order of 174 million ounces of silver, and 1.86 million ounces of gold from approximately 8.8 million tons of ore. Sporadic exploration has continued in the general area with new prospects being discovered including the Hall Molybdenum Mine, the Midway, Three Hills, and Hasbrouck gold prospects.

By January of 1901 there were between 40 and 50 lessees working leases granted by Butler et al, which consisted of 100 feet of vein and 50 feet to either side. It is problematic to determine exactly what production came from which claim or lease as typically several were amalgamated by a single company, and quite often the underground workings connected from one claim to the next. Often a shaft on one claim was used pretty much exclusively while a nearby shaft on the same groups of claims sat idle. It is likely impossible to ascertain or differentiate what production came from a single source or ascribe in many cases the full significance of some of these veins especially as quite often the production from one mine was brought to surface at another shaft, and not reported in a segregated manner.

Recent exploration phase for these properties has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from $20,000 and $200,000. This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on April 5, 2019. Samples were taken on 100 ft grid spacing vs 100M used in conventional Greenfields Exploration technics over the entire surface where safe to do so for each of the claims. At the start of each day and periods where the gun was off for more than 30 minutes the XRF was recalibrated using self-calibration then checked against a check sample with 1.25 Cr and .5 Mo. Additional calibrations were performed periodically throughout the day as altitude varied more than 1,000’ and/or temperatures changed more than 20 degrees Fahrenheit using a check sample with 1.25 Cr and .5 Mo. The XRF was primarily used by a technical staff with prior XRF field experience. Sample collection was conducted with direct supervision by Mr. Corey Holton who has over 12 years working with both fixed and handheld XRF machines within the lab and field environments. MrMr. Holton worked on the RUFF database from 2009-2010 in its infancy analyzing thousands of mineral compositions by XRF and XRD in a lab setting building a Spectro database. Samples were prepared in the following manner for rock faces of outcrops fresh surfaces were exposed using a rock hammer and the XRF was placed perpendicular to the face and a minimum of 30 seconds of data collection were taken to increase the accuracy of the readings. For areas where only quaternary alluvium was present holes were dug at a minimum depth of 6 inches below the surface to eliminate windblown deposits and uv altered samples. Sample materials were gathered pulverized and sampled for a minimum of 30 seconds. If any single sample was significantly different than surrounding data multiple samples were taken and averaged for the given sample location. If a sample was an extreme outlier or determined to be a false reading it was removed from the analysis. The XRF and tools were cleaned using alcohol pads between each sample location to minimize contamination between samples. Spectrographs were created for each sample and are included in Appendix C of the NI 43-101 Technical Report. XRF sampling is often used in exploration and is rapid compared to assay with a maximum error of 20%, although calibration and longer analysis times have proven to be 98% accurate as compared to assay analysis. All gross numbers presented in the NI 43-101 Technical Report were further reduced by 25% from original sample values. The XRF has been used in labs and the field for more than two decades and has shown that if used properly can have highly accurate results. Cross contamination has been shown to occur in both traditional assay and XRF therefore proper cleaning and preparation of each sample is critical. Mineral Resource and Ore Reserve Estimation – The AusIMM Guide to Good Practice (2^nd Ed) speaks to the reliability and validity of portable X-ray fluorescence spectrometry data. During the past 10 years the sample databases for XRF have improved resulting in a greater acceptance of XRF data for reserve studies.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Yellow Aster Mine showed that the elements promising for economic benefiting are:

Nearby geological attractions include Lunar Crater, the Sump and Monte Cristo’s Castle and there are five wilderness areas within hours of the community. The nearby Tonopah Test Range is the town’s main source of employment. The military has used the range and surrounding areas over the last half dozen decades as a nuclear test site, a bombing range, and as a base of operations for the development of the F-117 Nighthawk. Its location about halfway between Reno and Las Vegas as a stopover and rest spot on a lonely highway, the town has done fairly well. The Tonopah Station has slots, and the Banc Club also offers some gaming. Numerous restaurants, shops, gas stations and motels means it is a perfect place for staging while you work this mine.

Infrastructure is excellent in Tonopah district. Power is available at various points throughout the prospect, with a high-tension line running east-west along the northern margin of the Belmont tailings. Most supplies are available in Tonopah, while the nearest railhead is in Mina Nevada, approximately 85 kilometers (53 miles) to the northwest along highway 95. Manpower is available in the region, and personnel exist locally with training specific to the mining industry due to the proximity of the property to Kinross’s Round Mountain, and Scorpio Gold’s Mineral Peak operations. The owned claims all have cell phone service. Las Vegas is located approximately 280 kilometers (174 miles) to the southeast of the property, while Reno (which is an important mining supply center) is 270 kilometers (168 miles) to the northwest. The claim block area should be large enough to accommodate a production facility, and there are several potential processing plant sites in the area.

There is no developed infrastructure on this property.

Mine 2 – Fat Mule Flats

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found in the Fat Mules Flats Mine Property located in Tonopah, Nevada in Esmeralda County.

Fat Mule Flats Mine is a lode mine. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

The general course of this claim is North and South, and it is situated in the Southwest Quarter of Section 10, Township 2N, Range 42E, Mount Diablo Meridian, Esmeralda County, Nevada. This claim is 600 feet in length and 1,500 feet in width. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in a Northerly direction to the North end line and approximately 300 feet in a Southerly direction to the South end line. This claim is marked by four (4) monuments, one at each comer of the claim. Additionally, there are two (2) end-line markers on 3ach side of the center of the claim. All markers are 4” x 4” wooden posts that are buried 1.5’ in the ground and protrude 4.5’ above the ground embossed with the name of the claim and its location in relation to the claim.

The location monument on which this notice is posted is situated within Section 10, Township 2N, Range 42E, Mount Diablo Meridian, Esmeralda County Nevada and this claim encompasses portions of the following quarter section (s), Township (s), and Range (s); NW 1/4 of SW 1/4 and SW 1/4 of SW 1/4 Section 10, T2N, R42E, Mount Diablo Meridian, Esmeralda County Nevada. The locality of this claim with reference to some natural object or permanent monument and additional information (if any) concerning its locality are as follows: SW corner of this claim is 0 feet north and 730 feet east of the SW corner of Section 10, T2N, R42E. Beginning at the SW corner of this claim thence north a distance of 1,500 feet to the NW corner of this claim, thence east 600 feet to the NE corner of this claim, thence south 1,500 feet to the SE corner of this claim, thence west 600 feet back to the place of beginning, the SW Corner.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMC1188453 in the SW Quarter of Section 10, Township 2N, Range 42E, Mount Diablo Meridian, Esmeralda County, Nevada from Gateway Gold & Minerals, Inc.

Fat Mule Flats Mine

The Fat Mules Flats Mine is located in the Lone Mountain (West Divide, Weepah) mining district. The property is readily accessible via Highway 95 from Las Vegas to the South or Hwy’s 95/6 from the North/West from Northern Nevada/Reno or Bishop California, and from Highway 6 from the east which intersects highway 95 in the heart of Tonopah. This mine can be accessed by dirt roads using an ATV (all-terrain vehicle) or four-wheel drive vehicle and a GPS, main dirt roads leading through the mining district are maintained, but two track roads to the individual mines are often difficult to traverse. Caution is mandatory within the entire valley as it is dotted with abandoned mines – some of them are easy to see from a distance, and other are impossible to see until you are right on top of them. 20% of them are roped or fenced off – the rest do not have safety barriers and one should be extremely careful in entering them. Being situated in the high desert there are limited water sources in the area throughout 10 months out of the year.

Tonopah is located slightly inboard of the western margin of the Basin and Range province, and on the eastern margin of the “Walker Lane”,Lane,” a zone of Miocene structural deformation trending northwest to southeast parallel to the trend of the Sierra Madre Mountains in Eastern California (Figure 7.1). The Walker Lane can best be characterized as a broad zone of abundant strike-slip right-stepping faulting. The trend of the pre-Tertiary geologic units over much of the Walker Lane exhibits an arcuate pattern as a result of the influence of two major structural regimes. A series of these arcs have been identified by past workers with the Tonopah area having been identified as being within the Silver Peak-Palmetto-Montezuma Oroflex (Albers & Stewart 1972). The oroflex is described as southward convex with bedding, fold axes and faults trending to the northwest in the Silver Peak Range, trending east-west in the Palmetto Mountains and swinging around to the Northeast in the Montezuma Peak region. The Tonopah area lies on the eastern limb of the oroflex. The Walker Lane is also noted as being particularly well endowed with mineral deposits and the coincidence of these two structural regimes has created favorable plumbing, which is responsible for the high frequency of deposits in the region.

To the west of Tonopah, the White Mountains represent the westernmost range of the central Basin and Range province. They are situated to the east of the unextended Sierra Nevada Range and represent a crustal block that is bounded along its western flank by the high-angle White Mountains fault zone, with up to 8 km of total dip-slip displacement. Miocene volcanic rocks preserved along the eastern side of the range unconformably overlie Mesozoic granitic basement and dip up to 25° to the east, tilting occurred in the middle Miocene. The early geology of the general Tonopah region is relatively simple with the earliest Cambrian and Precambrian rocks comprised primarily of distal maritime facies - limestones, and dolomites with some hornfelsed shales. These are in fault contact with Ordivician limestones, argillites, and shales. From this point in time forward things become increasingly complex due to extensive volcanism in possibly alternating terrestrial and lacustrine settings. None of the Cambrian or Precambrian rocks outcrop in the immediate Tonopah area but fragments of these lithologies are present in volcanic breccias locally, so it is believed they form the basement of the volcanic complex.

The local geology is extremely well documented with geological investigations going back as early as 1905 when Spurr first published his voluminous observations of the camp. Spurr continued his work in the camp well into the 1920’s, followed by Bastin and Laney (1918), and later Nolan in 1930 published a study of the mines in the western part of the camp, and later expanded on this work, publishing a study that encompassed the entire camp in 1935. Later work was done in the area by Bonham (1970) and Bonham & Garside (1974 & 1979) during the time that work was carried out by Summa, Tenneco, and Houston Oil and Minerals.

The earlier workers in the area had the distinct advantage of having the bulk of the mine workings available at one time or another for inspection, while the later workers had the ability to draw from all the earlier well-documented work. Given the nature of this primarily felsic volcanic center, and the considerable alteration that has taken place prior, during and possibly somewhat after the mineralizing events, the geology of the camp is quite complex, and deciphering the history of the geology and mineralization of the area is only possible due to the thorough the attention paid to detail and the recording of these findings by earlier workers

The “Early” andesite of the Mizpah formation is almost exclusively the host rock for mineralization, however Bonanza style lode mineralization of the epoch does extend into the later andesite and in certain mines above the Mizpah into the Extension Breccia, the West End Rhyolitic intrusive and into the Fraction Tuff. From relative positioning and age dating it has been established that the earliest mineralizing event occurred between 20.5m.y. to 17m.y. before present.

The later mineralization event occurred around the end of the emplacement of the Fraction Tuff.

At Three Hills the gold bearing discontinuous, irregular, narrow, brecciated chalcedony quartz veinlets, and stockworks occur in a zone of pervasive silicification of the Siebert Formation immediately above the contact with the Fraction Tuff. At Hasbrouck, some gold-silver mineralization is seen within the Fraction Tuff, near its contact with the overlying Siebert formation, which hosts the bulk of the gold-silver mineralized veinlet and stockwork deposits. These occur as erratic bodies of hydrothermal breccia accompanied by strong pervasive silicification with associated adularia and pyrite. Adularia associated with mineralization at the Divide deposit was dated at between 16.3m.y. and 16.4 m.y. before present.

This mine was cut in 1908 as far as our research could determine. But it was worked for 23 years prior to 1940. The mine appear to have been a medium-sized operation – maybe by 2 to 3 miners at the most based on the size of the workings. When part of the General Thomas Mine was split up into smaller properties for sale (owned by the Tonopah-Belcher Mining Co. at that time as well as the General Thomas Of Tonopah Co. before the split), this mine was likely called the Tonopah-Belcher Mine. Classified by a 1904 USGS report as a “past producer of Gold, Lead, Silver (Primary) and Copper (Secondary) -this area is a legendary part of Tonopah that has history dating as far back as 1863 when the district was founded.

Recent exploration phase for these properties has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from $20,000 and $200,000. This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on 4/5/2019. The Niton XRF (X-Ray Fluorescence) instrument was used in mining mode to analyze 23 minerals with GOLDD Technology enabled. GOLDD Technology: When low detection limits and high sample throughput are critical, the Niton XL3t GOLDD+ XRF analyzer delivers measurement times up to 10-times faster than conventional Si-PIN detectors and up to 3-times more precise than conventional smaller silicon drift detectors (SDD) – without helium purge or vacuum. Niton analyzers also feature the highest performance X-ray tube and speed detector available on the market. Spectrographs were created for each sample and are included in Appendix C.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Yellow Aster MineFat Mules showed that the elements promising for economic benefiting are Gold, Titanium, Manganese, Iron, Arsenic, Rubidium, Strontium, Zirconium, Niobium and Bismuth.

Infrastructure is excellent in Tonopah district. Power is available at various points throughout the prospect, with a high-tension line running east-west along the northern margin of the Belmont tailings. Most supplies are available in Tonopah, while the nearest railhead is in Mina Nevada, approximately 85 kilometers (53 miles) to the northwest along highway 95. Manpower is available in the region, and personnel exist locally with training specific to the mining industry due to the proximity of the property to Kinross’ Round Mountain, and Scorpio Gold’s Mineral Peak operations. The owned claims all have cell phone service. Las Vegas is located approximately 280 kilometers (174 miles) to the southeast of the property, while Reno (which is an important mining supply center) is 270 kilometers (168 miles) to the northwest. The claim block area should be large enough to accommodate a production facility, and there are several potential processing plant sites in the area.

●Property Infrastructure

The Fat Mule Flats mine shows 88 feet deep with 700 feet of tunnels, drifts, and crosscuts on 2 separate levels. The wood collar looks like it is still in pretty good shape, but the head frame is long gone.

Mine 3 – Cobin

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found in the Cobin Mine Property located in Tonopah, Nevada in Esmeralda County.

Cobin Mine is a lode mine. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

The general course of this claim is North and South, and it is situated in the Southwest Quarter of Section 30, Township 2N, Range 41E, Mount Diablo Meridian, Esmeralda County, Nevada. This claim is 1,500 feet in width and 600 feet in height. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in a Northerly direction to the North end line and approximately 300 feet in a Southerly direction to the South end line. This claim is marked by four (4) monuments, one at each corner of the claim. Additionally, there are two (2) end-line markers on each side of the center of the claim. All markers are 4” x 4” wooden posts that are buried 1.5’ in the ground and protrude 4.5’ above the ground embossed with the name of the claim and its location in relation to the claim.

The location monument on which this notice is posted is situated within Section 30, Township 2N, Range 41E, Mount Diablo Meridian, Esmeralda County Nevada and this claim encompasses portions of the following quarter section (s), Township (s), and Range (s); L3/NW 1/4 of SW 1/4 and L4/SW 1/4 of SW 1/4 Section 30, T2N, R41E, Mount Diablo Meridian, Esmeralda County Nevada. The locality of this claim with reference to some natural object or permanent monument and additional information (if any) concerning its locality are as follows: SW corner of this claim is 595 Feet north and 340 Feet east of the SW corner of Section 30, T2N, R41E. Beginning at the SW corner of this claim thence due north 1,500 feet to the NW corner of this claim, thence due east a distance of 600 feet to the NE corner of this claim thence due south 1,500 feet to the SE comer of this claim, thence due west 600 feet back to the place of beginning, the SW Corner.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMC1187753 in the SW Quarter of Section 30, Township 2N, Range 41E, Mount Diablo Meridian, Esmeralda County, Nevada from Gateway Gold & Minerals, Inc.

Cobin Mine

Tonopah is located slightly inboard of the western margin of the Basin and Range province, and on the eastern margin of the “Walker Lane”,Lane,” a zone of Miocene structural deformation trending northwest to southeast parallel to the trend of the Sierra Madre Mountains in Eastern California. The Walker Lane can best be characterized as a broad zone of abundant strike-slip right-stepping faulting.

The trend of the pre-Tertiary geologic units over much of the Walker Lane exhibits an arcuate pattern as a result of the influence of two major structural regimes. A series of these arcs have been identified by past workers with the Tonopah area having been identified as being within the Silver Peak-Palmetto- Montezuma Oroflex (Albers & Stewart 1972). The oroflex is described as southward convex with bedding, fold axes and faults trending to the northwest in the Silver Peak Range, trending east-west in the Palmetto Mountains and swinging around to the Northeast in the Montezuma Peak region. The Tonopah area lies on the eastern limb of the oroflex. The Walker Lane is also noted as being particularly well endowed with mineral deposits and the coincidence of these two structural regimes has created favorable plumbing, which is responsible for the high frequency of deposits in the region.

To the west of Tonopah, the White Mountains represent the westernmost range of the central Basin and Range province. They are situated to the east of the unextended Sierra Nevada Range and represent a crustal block that is bounded along its western flank by the high-angle White Mountains fault zone, with up to 8 km of total dip-slip displacement. Miocene volcanic rocks preserved along the eastern side of the range unconformably overlie Mesozoic granitic basement and dip up to 25° to the east, tilting occurred in the middle Miocene. The early geology of the general Tonopah region is relatively simple with the earliest Cambrian and Precambrian rocks comprised primarily of distal maritime facies - limestones, and dolomites with some hornfelsed shales. These are in fault contact with Ordivician limestones, argillites, and shales. From this point in time forward things become increasingly complex due to extensive volcanism in possibly alternating terrestrial and lacustrine settings.

None of the Cambrian or Precambrian rocks outcrop in the immediate Tonopah area but fragments of these lithologies are present in volcanic breccias locally, so it is believed they form the basement of the volcanic complex.

The local geology is extremely well documented with geological investigations going back as early as 1905 when Spurr first published his voluminous observations of the camp. Spurr continued his work in the camp well into the 1920’s, followed by Bastin and Laney (1918), and later Nolan in 1930 published a study of the mines in the western part of the camp, and later expanded on this work, publishing a study that encompassed the entire camp in 1935. Later work was done in the area by Bonham (1970) and Bonham & Garside (1974 & 1979) during the time that work was carried out by Summa, Tenneco, and Houston Oil and Minerals.

The earlier workers in the area had the distinct advantage of having the bulk of the mine workings available at one time or another for inspection, while the later workers had the ability to draw from all the earlier well-documented work. Given the nature of this primarily felsic volcanic center, and the considerable alteration that has taken place prior, during and possibly somewhat after the mineralizing events, the geology of the camp is quite complex, and deciphering the history of the geology and mineralization of the area is only possible due to the thorough the attention paid to detail and the recording of these findings by earlier workers

The “Early” andesite of the Mizpah formation is almost exclusively the host rock for mineralization, however Bonanza style lode mineralization of the epoch does extend into the later andesite and in certain mines above the Mizpah into the Extension Breccia, the West End Rhyolitic intrusive and into the Fraction Tuff. From relative positioning and age dating it has been established that the earliest mineralizing event occurred between 20.5m.y. to 17m.y. before present.

The later mineralization event occurred around the end of the emplacement of the Fraction Tuff.

At Three Hills the gold bearing discontinuous, irregular, narrow, brecciated chalcedony quartz veinlets, and stockworks occur in a zone of pervasive silicification of the Siebert Formation immediately above the contact with the Fraction Tuff. At Hasbrouck, some gold-silver mineralization is seen within the Fraction Tuff, near its contact with the overlying Siebert formation, which hosts the bulk of the gold-silver mineralized veinlet and stockwork deposits. These occur as erratic bodies of hydrothermal breccia accompanied by strong pervasive silicification with associated adularia and pyrite. Adularia associated with mineralization at the Divide deposit was dated at between 16.3m.y. and 16.4 m.y. before present.

No significant exploration has been noted at these mines in a few decades so a historical account of publicly found data was assimilated. The Tonopah Mining District began circa 1900 with the discovery of gold and silver-rich ore by prospector Jim Butler when he went looking for a lost burro he owned. The burro had wandered off during the night and sought shelter near a rock outcropping. When Butler discovered the animal the next morning, he picked up a rock to throw at the beast, but instead noticed the rock was unusually heavy. He had stumbled upon the second-richest silver strike in Nevada history. While Butler may have been responsible for the first ore strike, it took men of wealth and power to consolidate the mines and reinvest their profits into the infrastructure of the town of Tonopah.

George Wingfield, a 24-year old24-year-old poker player when he arrived in Tonopah, played poker, and dealt faro in the town saloons. Once he had a small bankroll, he talked Jack Carey, owner of the Tonopah Club, into taking him in as a partner and to file for a gaming license. In 1903, miners rioted against Chinese workers in Tonopah, which spurred a boycott in China of U.S. goods. By 1904, after investing his winnings in the Boston-Tonopah Mining Company, Wingfield was worth $2 million. When old friend George S. Nixon, a banker, arrived in town, Wingfield invested in his Nye County Bank. They grub staked miners with friend Nick Abelman, bought existing mines, and by the time the partners moved to Goldfield, Nevada and made their Goldfield Consolidated Mining Company a public corporation in 1906, Nixon and Wingfield were worth over $30 million. Small mining ventures continue to this day to provide income for local miners.

The discovery and development of the Tonopah area can be separated into four periods. From 1900 to 1903 the various participants acquired their ground and commenced development work by sinking shafts to access the ore. Between 1903 and 1907 development continued and better and more efficient equipment was deployed to increase production. The recession of 1907 to 1910 caused production to drop off as only the higher-grade ore could be profitably mined with silver prices dropping to as low as $0.25/oz. During this period many of the weaker companies went out of business and consolidation of claims occurred. The high point of the Tonopah camp occurred between 1910 and 1930 with production peaking around 1918 at 622,364 tons/year, with a recorded value of $9,311,560,, and declining steadily through the 1920’s.

Production came to a halt with the exception of leasehold mining in the 30’s due to the depression and low precious metals prices. There was virtually no activity during the war in the 40’s but there was somewhat of a resurgence of activity in the 50’s. In total the Tonopah area produced in the order of 174 million ounces of silver, and 1.86 million ounces of gold from approximately 8.8 million tons of ore. Sporadic exploration has continued in the general area with new prospects being discovered including the Hall Molybdenum Mine, the Midway, Three Hills, and Hasbrouck gold prospects.

By January of 1901 there were between 40 and 50 lessees working leases granted by Butler et al, which consisted of 100 feet of vein and 50 feet to either side. It is problematic to determine exactly what production came from which claim or lease as typically several were amalgamated by a single company, and quite often the underground workings connected from one claim to the next. Often a shaft on one claim was used pretty much exclusively while a nearby shaft on the same groups of claims sat idle. It is likely impossible to ascertain or differentiate what production came from a single source or ascribe in many cases the full significance of some of these veins especially as quite often the production from one mine was brought to surface at another shaft, and not reported in a segregated manner.

Recent exploration phase for these properties has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from $20,000 and $200,000.This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on 4/5/2019. The Niton XRF (X-Ray Fluorescence) instrument was used in mining mode to analyze 23 minerals with GOLDD Technology enabled. GOLDD Technology: When low detection limits and high sample throughput are critical, the Niton XL3t GOLDD+ XRF analyzer delivers measurement times up to 10-times faster than conventional Si-PIN detectors and up to 3-times more precise than conventional smaller silicon drift detectors (SDD) – without helium purge or vacuum. Niton analyzers also feature the highest performance X-ray tube and speed detector available on the market. Spectrographs were created for each sample and are included in Appendix C.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Cobin Mine showed that the elements promising for economic benefiting are Gold, Titanium, Manganese, Iron, Arsenic, Rubidium, Strontium, Zirconium, Niobium, Hafnium and Bismuth.

Nearby geological attractions include Lunar Crater, the Sump and Monte Cristo’s Castle and there are five wilderness areas within hours of the community. The nearby Tonopah Test Range is the town’s main source of employment. The military has used the range and surrounding areas over the last half dozen decades as a nuclear test site, a bombing range, and as a base of operations for the development of the F-117 Nighthawk. Its location about halfway between Reno and Las Vegas as a stopover and rest spot on a lonely highway, the town has done fairly well. The Tonopah Station has slots, and the Banc Club also offers some gaming. Numerous restaurants, shops, gas stations and motels means it is a perfect place for staging while you work this mine.

Infrastructure is excellent in Tonopah district. Power is available at various points throughout the prospect, with a high-tension line running east-west along the northern margin of the Belmont tailings. Most supplies are available in Tonopah, while the nearest railhead is in Mina Nevada, approximately 85 kilometers (53 miles) to the northwest along highway 95. Manpower is available in the region, and personnel exist locally with training specific to the mining industry due to the proximity of the property to Kinross’s Round Mountain, and Scorpio Gold’s Mineral Peak operations. The owned claims all have cell phone service. Las Vegas is located approximately 280 kilometers (174 miles) to the southeast of the property, while Reno (which is an important mining supply center) is 270 kilometers (168 miles) to the northwest. The claim block area should be large enough to accommodate a production facility, and there are several potential processing plant sites in the area.

There is no developed infrastructure on this property.

Mine 4 – Jasper

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found in the Jasper Mine Property located in Tonopah, Nevada in Esmeralda County.

The Probable Gross Gold Resources are 1,141,774.55 oz based on projected 200 feet excavation.

Jasper Mine is a lode mine as well as an open-pitopen pit mine. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

As defined by Anglo-American, open-pit mining, also known as opencast mining, is a surface mining technique that extracts minerals from an open pit in the ground. Open-pit mining is the most common method used throughout the world for mineral mining and does not require extractive methods or tunnels. This surface mining technique is used when mineral or ore deposits are found relatively close to the surface of the earth. Open-pitsOpen pits are sometimes called ‘quarries’ when they produce building materials and dimension stone.

The general course of this claim is North and South, and it is situated in the Southeast Quarter of Section 1, Township 1N, Range 40E, Mount Diablo Meridian, Esmeralda County, Nevada. This claim is 600 feet in width and 1,500 feet in length. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in a Northerly direction to the North end line and approximately 300 feet in a Southerly direction to the South end line. This claim is marked by four (4) monuments, one at each corner of the claim. Additionally, there are two (2) end-line markers on each side of the center of the claim. All markers are 4” x 4” wooden posts that are buried 1.5’ in the ground and protrude 4.5’ above the ground embossed with the name of the claim and its location in relation to the claim. The location monument on which this notice is posted is situated within Section 1, Township 1N, Range 40E, Mount Diablo Meridian, Esmeralda County Nevada and this claim encompasses portions of the following quarter section (s), Township (s), and Range (s); NE 1/4 of SE 1/4, NW 1/4 of SE 1/4, SE 1/4 of SE 1/4, and SW 1/4 of SE 1/4 of Section 1, T1N, R40E, Mount Diablo Meridian, Esmeralda County Nevada. The locality of this claim with reference to some natural object or permanent monument and additional information (if any) concerning its locality are as follows: SE corner of this claim is 990 Feet West and 825 Feet North of the SE corner of Section 1, T1N, R40E. Beginning at the SE corner of this claim thence 1,500 feet due north to the NE corner of this claim, thence 600 feet due west to the NW corner of this claim, thence 1,320 feet due south to the SW corner of this claim, thence due east 600 feet back to the place of beginning, the SE corner.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMC1191786 in SE Quarter of Section 1, Township 1N, Range 40E, Mount Diablo Meridian, Esmeralda County, Nevada from Gateway Gold & Minerals, Inc.

Jasper Mine

The property is readily accessible via Highway 95 from Las Vegas to the South or Hwy’s 95/6 from the North/West from Northern Nevada/Reno or Bishop California, and from Highway 6 from the east which intersects highway 95 in the heart of Tonopah. This mine can be accessed by dirt roads using an ATV (all-terrain vehicle) or four-wheel drive vehicle and a GPS, main dirt roads leading through the mining district are maintained, but two track roads to the individual mines are often difficult to traverse. Caution is mandatory within the entire valley as it is dotted with abandoned mines – some of them are easy to see from a distance, and other are impossible to see until you are right on top of them. 20% of them are roped or fenced off – the rest do not have safety barriers and one should be extremely careful in entering them. Being situated in the high desert there are limited water sources in the area throughout 10 months out of the year.

Tonopah is located slightly inboard of the western margin of the Basin and Range province, and on the eastern margin of the “Walker Lane”,Lane,” a zone of Miocene structural deformation trending northwest to southeast parallel to the trend of the Sierra Madre Mountains in Eastern California. The Walker Lane can best be characterized as a broad zone of abundant strike-slip right-stepping faulting.

The trend of the pre-Tertiary geologic units over much of the Walker Lane exhibits an arcuate pattern as a result of the influence of two major structural regimes. A series of these arcs have been identified by past workers with the Tonopah area having been identified as being within the Silver Peak-Palmetto- Montezuma Oroflex (Albers & Stewart 1972). The oroflex is described as southward convex with bedding, fold axes and faults trending to the northwest in the Silver Peak Range, trending east-west in the Palmetto Mountains and swinging around to the Northeast in the Montezuma Peak region. The Tonopah area lies on the eastern limb of the oroflex. The Walker Lane is also noted as being particularly well endowed with mineral deposits and the coincidence of these two structural regimes has created favorable plumbing, which is responsible for the high frequency of deposits in the region.

To the west of Tonopah, the White Mountains represent the westernmost range of the central Basin and Range province. They are situated to the east of the unextended Sierra Nevada Range and represent a crustal block that is bounded along its western flank by the high-angle White Mountains fault zone, with up to 8 km of total dip-slip displacement. Miocene volcanic rocks preserved along the eastern side of the range unconformably overlie Mesozoic granitic basement and dip up to 25° to the east, tilting occurred in the middle Miocene. The early geology of the general Tonopah region is relatively simple with the earliest Cambrian and Precambrian rocks comprised primarily of distal maritime facies - limestones, and dolomites with some hornfelsed shales. These are in fault contact with Ordivician limestones, argillites, and shales. From this point in time forward things become increasingly complex due to extensive volcanism in possibly alternating terrestrial and lacustrine settings.

None of the Cambrian or Precambrian rocks outcrop in the immediate Tonopah area but fragments of these lithologies are present in volcanic breccias locally, so it is believed they form the basement of the volcanic complex.

The local geology is extremely well documented with geological investigations going back as early as 1905 when Spurr first published his voluminous observations of the camp. Spurr continued his work in the camp well into the 1920’s, followed by Bastin and Laney (1918), and later Nolan in 1930 published a study of the mines in the western part of the camp, and later expanded on this work, publishing a study that encompassed the entire camp in 1935. Later work was done in the area by Bonham (1970) and Bonham & Garside (1974 & 1979) during the time that work was carried out by Summa, Tenneco, and Houston Oil and Minerals.

The earlier workers in the area had the distinct advantage of having the bulk of the mine workings available at one time or another for inspection, while the later workers had the ability to draw from all the earlier well-documented work. Given the nature of this primarily felsic volcanic center, and the considerable alteration that has taken place prior, during and possibly somewhat after the mineralizing events, the geology of the camp is quite complex, and deciphering the history of the geology and mineralization of the area is only possible due to the thorough the attention paid to detail and the recording of these findings by earlier workers.

Mineralization

The “Early” andesite of the Mizpah formation is almost exclusively the host rock for mineralization, however Bonanza style lode mineralization of the epoch does extend into the later andesite and in certain mines above the Mizpah into the Extension Breccia, the West End Rhyolitic intrusive and into the Fraction Tuff. From relative positioning and age dating it has been established that the earliest mineralizing event occurred between 20.5m.y. to 17m.y. before present.

The later mineralization event occurred around the end of the emplacement of the Fraction Tuff.

At Three Hills the gold bearing discontinuous, irregular, narrow, brecciated chalcedony quartz veinlets, and stockworks occur in a zone of pervasive silicification of the Siebert Formation immediately above the contact with the Fraction Tuff. At Hasbrouck, some gold-silver mineralization is seen within the Fraction Tuff, near its contact with the overlying Siebert formation, which hosts the bulk of the gold-silver mineralized veinlet and stockwork deposits. These occur as erratic bodies of hydrothermal breccia accompanied by strong pervasive silicification with associated adularia and pyrite. Adularia associated with mineralization at the Divide deposit was dated at between 16.3m.y. and 16.4 m.y. before present.

No significant exploration has been noted at these mines in a few decades so a historical account of publicly found data was assimilated.

Recent exploration phase for these properties has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from $20,000 and $200,000. This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on 4/5/2019. The Niton XRF (X-Ray Fluorescence) instrument was used in mining mode to analyze 23 minerals with GOLDD Technology enabled. GOLDD Technology: When low detection limits and high sample throughput are critical, the Niton XL3t GOLDD+ XRF analyzer delivers measurement times up to 10-times faster than conventional Si-PIN detectors and up to 3-times more precise than conventional smaller silicon drift detectors (SDD) – without helium purge or vacuum. Niton analyzers also feature the highest performance X-ray tube and speed detector available on the market. Spectrographs were created for each sample and are included in Appendix C.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Jasper Mine showed that the elements promising for economic benefiting are Gold, Titanium, Manganese, Iron, Arsenic, Rubidium, Strontium, Zirconium, Niobium and Bismuth.

Nearby geological attractions include Lunar Crater, the Sump and Monte Cristo’s Castle and there are five wilderness areas within hours of the community.

Infrastructure is excellent in Tonopah district. Power is available at various points throughout the prospect, with a high-tension line running east-west along the northern margin of the Belmont tailings. Most supplies are available in Tonopah, while the nearest railhead is in Mina Nevada, approximately 85 kilometers (53 miles) to the northwest along highway 95. Manpower is available in the region, and personnel exist locally with training specific to the mining industry due to the proximity of the property to Kinross’s Round Mountain, and Scorpio Gold’s Mineral Peak operations. The owned claims all have cell phone service. Las Vegas is located approximately 280 kilometers (174 miles) to the southeast of the property, while Reno (which is an important mining supply center) is 270 kilometers (168 miles) to the northwest. The claim block area should be large enough to accommodate a production facility, and there are several potential processing plant sites in the area.

There are remains of what is believed to be a good-sized cabin outside.

Mine 5 – Barracks Nine

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found in the Barracks Nine Property located in Tonopah, Nevada in Esmeralda County.

The Probable Gross Gold Resources are 1,001,531.19 oz based on projected 200 feet excavation.

The mine is lode and open-pitopen pit mine. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

The general course of this claim is North and South, and it is situated in the NE Quarter of Section 9, Township 1N, Range 41E, Mount Diablo Meridian, Esmeralda County, Nevada. This claim is 600 feet wide and 1,500 feet tall. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in a Northerly direction to the North end line and approximately 300 feet in a Southerly direction to the South end line. This claim is marked by four (4) monuments, one at each corner of the claim. Additionally, there are two (2) end-line markers on each side of the center of the claim. All markers are 4” x 4” wooden posts that are buried 1.5’ in the ground and protrude 4.5’ above the ground embossed with the name of the claim and its location in relation to the claim.

The location monument on which this notice is posted is situated within Section 9, Township 1N, Range 41E, Mount Diablo Meridian, Esmeralda County Nevada and this claim encompasses portions of the following quarter section (s), Township (s), and Range (s); NE 1/4 of NE 1/4 and SE 1/4 of NE ¼ Section 9, T1N, R41E, Mount Diablo Meridian, Esmeralda County Nevada. The locality of this claim with reference to some natural object or permanent monument and additional information (if any) concerning its locality are as follows: NE corner of this claim is the NE corner of Section 9, T1N, R41E. Beginning at the NE corner of this claim thence 600 feet due west to the NW corner of this claim, thence 1,500 feet due south to the SW corner of this claim, thence 600 feet due east to the SE corner of this claim, thence due north 1,500 feet back to the place of beginning, the NE corner.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMC1186292 in the NE Quarter of Section 9, Township 1N, Range 41E, Mount Diablo Meridian, Esmeralda County, Nevada from Gateway Gold & Minerals, Inc.

Barracks Nine Mine

The property is readily accessible via Highway 95 from Las Vegas to the South or Hwy’s 95/6 from the North/West from Northern Nevada/Reno or Bishop California, and from Highway 6 from the east which intersects highway 95 in the heart of Tonopah. This mine can be accessed by dirt roads using an ATV (all-terrain vehicle) or four-wheel drive vehicle and a GPS, main dirt roads leading through the mining district are maintained, but two track roads to the individual mines are often difficult to traverse. Caution is mandatory within the entire valley as it is dotted with abandoned mines – some of them are easy to see from a distance, and other are impossible to see until you are right on top of them. 20% of them are roped or fenced off – the rest do not have safety barriers and one should be extremely careful in entering them. Being situated in the high desert there are limited water sources in the area throughout 10 months out of the year.

Tonopah is located slightly inboard of the western margin of the Basin and Range province, and on the eastern margin of the “Walker Lane”,Lane,” a zone of Miocene structural deformation trending northwest to southeast parallel to the trend of the Sierra Madre Mountains in Eastern California. The Walker Lane can best be characterized as a broad zone of abundant strike-slip right-stepping faulting. The trend of the pre-Tertiary geologic units over much of the Walker Lane exhibits an arcuate pattern as a result of the influence of two major structural regimes. A series of these arcs have been identified by past workers with the Tonopah area having been identified as being within the Silver Peak-Palmetto- Montezuma Oroflex (Albers & Stewart 1972). The oroflex is described as southward convex with bedding, fold axes and faults trending to the northwest in the Silver Peak Range, trending east-west in the Palmetto Mountains and swinging around to the Northeast in the Montezuma Peak region. The Tonopah area lies on the eastern limb of the oroflex. The Walker Lane is also noted as being particularly well endowed with mineral deposits and the coincidence of these two structural regimes has created favorable plumbing, which is responsible for the high frequency of deposits in the region.

To the west of Tonopah, the White Mountains represent the westernmost range of the central Basin and Range province. They are situated to the east of the unextended Sierra Nevada Range and represent a crustal block that is bounded along its western flank by the high-angle White Mountains fault zone, with up to 8 km of total dip-slip displacement. Miocene volcanic rocks preserved along the eastern side of the range unconformably overlie Mesozoic granitic basement and dip up to 25° to the east, tilting occurred in the middle Miocene. The early geology of the general Tonopah region is relatively simple with the earliest Cambrian and Precambrian rocks comprised primarily of distal maritime facies - limestones, and dolomites with some hornfelsed shales. These are in fault contact with Ordivician limestones, argillites, and shales. From this point in time forward things become increasingly complex due to extensive volcanism in possibly alternating terrestrial and lacustrine settings. None of the Cambrian or Precambrian rocks outcrop in the immediate Tonopah area but fragments of these lithologies are present in volcanic breccias locally, so it is believed they form the basement of the volcanic complex.

The local geology is extremely well documented with geological investigations going back as early as 1905 when Spurr first published his voluminous observations of the camp. Spurr continued his work in the camp well into the 1920’s, followed by Bastin and Laney (1918), and later Nolan in 1930 published a study of the mines in the western part of the camp, and later expanded on this work, publishing a study that encompassed the entire camp in 1935. Later work was done in the area by Bonham (1970) and Bonham & Garside (1974 & 1979) during the time that work was carried out by Summa, Tenneco, and Houston Oil and Minerals. The earlier workers in the area had the distinct advantage of having the bulk of the mine workings available at one time or another for inspection, while the later workers had the ability to draw from all the earlier well-documented work.

Given the nature of this primarily felsic volcanic center, and the considerable alteration that has taken place prior, during and possibly somewhat after the mineralizing events, the geology of the camp is quite complex, and deciphering the history of the geology and mineralization of the area is only possible due to the thorough the attention paid to detail and the recording of these findings by earlier workers.

The “Early” andesite of the Mizpah formation is almost exclusively the host rock for mineralization, however Bonanza style lode mineralization of the epoch does extend into the later andesite and in certain mines above the Mizpah into the Extension Breccia, the West End Rhyolitic intrusive and into the Fraction Tuff. From relative positioning and age dating it has been established that the earliest mineralizing event occurred between 20.5m.y. to 17m.y. before present.

The later mineralization event occurred around the end of the emplacement of the Fraction Tuff.

At Three Hills the gold bearing discontinuous, irregular, narrow, brecciated chalcedony quartz veinlets, and stockworks occur in a zone of pervasive silicification of the Siebert Formation immediately above the contact with the Fraction Tuff. At Hasbrouck, some gold-silver mineralization is seen within the Fraction Tuff, near its contact with the overlying Siebert formation, which hosts the bulk of the gold-silver mineralized veinlet and stockwork deposits. These occur as erratic bodies of hydrothermal breccia accompanied by strong pervasive silicification with associated adularia and pyrite. Adularia associated with mineralization at the Divide deposit was dated at between 16.3m.y. and 16.4 m.y. before present.

It is easy to see the vein they were following, a rich vein with lots of gem-quality quartz in a thick, wide vein running from the surface down. A shaft was cut 62 feet deep at about a 20-degree angle, and at the bottom, it branches into a horizontal adit running North to North EastNortheast under the peak of this hill right next to the General Thomas Hill (where one of the largest producing mines in the area is still located). There is some really good color even at the top of the shaft, so easy to get to. There is plenty of material in the access point before you even enter the mine. This is one of the last Tonopah mines available for mining.

No significant exploration has been noted at these mines in a few decades so a historical account of publicly found data was assimilated. The Tonopah Mining District began circa 1900 with the discovery of gold and silver-rich ore by prospector Jim Butler when he went looking for a lost burro he owned. The burro had wandered off during the night and sought shelter near a rock outcropping. When Butler discovered the animal the next morning, he picked up a rock to throw at the beast, but instead noticed the rock was unusually heavy. He had stumbled upon the second-richest silver strike in Nevada history. While Butler may have been responsible for the first ore strike, it took men of wealth and power to consolidate the mines and reinvest their profits into the infrastructure of the town of Tonopah.

George Wingfield, a 24-year old24-year-old poker player when he arrived in Tonopah, played poker, and dealt faro in the town saloons. Once he had a small bankroll, he talked Jack Carey, owner of the Tonopah Club, into taking him in as a partner and to file for a gaming license. In 1903, miners rioted against Chinese workers in Tonopah, which spurred a boycott in China of U.S. goods. By 1904, after investing his winnings in the Boston-Tonopah Mining Company, Wingfield was worth $2 million. When old friend George S. Nixon, a banker, arrived in town, Wingfield invested in his Nye County Bank. They grub staked miners with friend Nick Abelman, bought existing mines, and by the time the partners moved to Goldfield, Nevada and made their Goldfield Consolidated Mining Company a public corporation in 1906, , Nixon and Wingfield were worth over $30 million. Small mining ventures continue to this day to provide income for local miners.

The discovery and development of the Tonopah area can be separated into four periods. From 1900 to 1903 the various participants acquired their ground and commenced development work by sinking shafts to access the ore. Between 1903 and 1907 development continued and better and more efficient equipment was deployed to increase production. The recession of 1907 to 1910 caused production to drop off as only the higher-grade ore could be profitably mined with silver prices dropping to as low as $0.25/oz. During this period many of the weaker companies went out of business and consolidation of claims occurred. The high point of the Tonopah camp occurred between 1910 and 1930 with production peaking around 1918 at 622,364 tons/year, with a recorded value of $9,311,560,, and declining steadily through the 1920’s.

Production came to a halt with the exception of leasehold mining in the 30’s due to the depression and low precious metals prices. There was virtually no activity during the war in the 40’s but there was somewhat of a resurgence of activity in the 50’s. In the Tonopah area produced in the order of 174 million ounces of silver, and 1.86 million ounces of gold from approximately 8.8 million tons of ore. Sporadic exploration has continued in the general area with new prospects being discovered including the Hall Molybdenum Mine, the Midway, Three Hills, and Hasbrouck gold prospects.

By January of 1901 there were between 40 and 50 lessees working leases granted by Butler et al, which consisted of 100 feet of vein and 50 feet to either side. It is problematic to determine exactly what production came from which claim or lease as typically several were amalgamated by a single company, and quite often the underground workings connected from one claim to the next. Often a shaft on one claim was used pretty much exclusively while a nearby shaft on the same groups of claims sat idle. It is likely impossible to ascertain or differentiate what production came from a single source or ascribe in many cases the full significance of some of these veins especially as quite often the production from one mine was brought to surface at another shaft, and not reported in a segregated manner.

Recent exploration phase for the property has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from$20,000 $20,000 and $200,000. This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on 4/5/2019. The Niton XRF (X-Ray Fluorescence) instrument was used in mining mode to analyze 23 minerals with GOLDD Technology enabled. GOLDD Technology: When low detection limits and high sample throughput are critical, the Niton XL3t GOLDD+ XRF analyzer delivers measurement times up to 10-times faster than conventional Si-PIN detectors and up to 3-times more precise than conventional smaller silicon drift detectors (SDD) – without helium purge or vacuum. Niton analyzers also feature the highest performance X-ray tube and speed detector available on the market. Spectrographs were created for each sample and are included in Appendix C.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Barracks Nine Mine showed that the elements promising for economic benefiting are: Gold, Titanium, Manganese, Iron, Arsenic, Rubidium, Strontium, Zirconium, Niobium and Bismuth.

Nearby geological attractions include Lunar Crater, the Sump and Monte Cristo’s Castle and there are five wilderness areas within hours of the community. The nearby Tonopah Test Range is the town’s main source of employment. The military has used the range and surrounding areas over the last half dozen decades as a nuclear test site, a bombing range, and as a base of operations for the development of the F-117 Nighthawk. Its location about halfway between Reno and Las Vegas as a stopover and rest spot on a lonely highway, the town has done fairly well. The Tonopah Station has slots, and the Banc Club also offers some gaming. Numerous restaurants, shops, gas stations and motels means it is a perfect place for staging while you work this mine.

Infrastructure is excellent in Tonopah district. Power is available at various points throughout the prospect, with a high-tension line running east-west along the northern margin of the Belmont tailings. Most supplies are available in Tonopah, while the nearest railhead is in Mina Nevada, approximately 85 kilometers (53 miles) to the northwest along highway 95. Manpower is available in the region, and personnel exist locally with training specific to the mining industry due to the proximity of the property to Kinross’s Round Mountain, and Scorpio Gold’s Mineral Peak operations. The owned claims all have cell phone service. Las Vegas is located approximately 280 kilometers (174 miles) to the southeast of the property, while Reno (which is an important mining supply center) is 270 kilometers (168 miles) to the northwest. The claim block area should be large enough to accommodate a production facility, and there are several potential processing plant sites in the area.

There is no developed infrastructure on this property.

Mine 6 – Eclipse

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found in the Eclipse Mine Property located in Tonopah, Nevada in Esmeralda County.

The Probable Gross Gold Resources are 2,657,630.86 oz based on projected 200 feet excavation. This estimate includes the Jasper mine claim. Due to the topography less, samples were taken at these two adjacent claims which leads to greater uncertainty in reserve numbers.

The Eclipse mine is lode and open-pit mines. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

The general course of this claim is North and South, and it is situated in the NW Quarter of Section 11, Township 1N, Range 40E, Mount Diablo Meridian, Esmeralda County, Nevada. This claim is 1,500 feet in length and 600 feet in width. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in a Northerly direction to the North end line and approximately 300 feet in a Southerly direction to the South end line. This claim is marked by four (4) monuments, one at each corner of the claim. Additionally, there are two (2) end-line markers on each side of the center of the claim. All markers are 4” x 4” wooden posts that are buried 1.5’ in the ground and protrude 4.5’ above the ground embossed with the name of the claim and its location in relation to the claim.

The location monument on which this notice is posted is situated within Section 11, Township IN, Range 40E, Mount Diablo Meridian, Esmeralda County Nevada and this claim encompasses portions of the following quarter section (s), Township (s), and Range (s); NW 1/4 of Section 11, T1N, R40E, Mount Diablo Meridian, Esmeralda County Nevada. The locality of this claim with reference to some natural object or permanent monument and additional information (if any) concerning its locality are as follows: NW corner of this claim is located 1,130 Feet South and 1,230 Feet East from the NW corner of Section 11, T1N, R40E. Beginning at the NW corner of this claim thence south a distance of 1,500 feet to the SW corner of this claim, thence east 600 feet to the SE corner of this claim, thence North 1,500 feet to the NE corner of this claim, thence west 600 feet back to the place of beginning.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMC1187899 in the NW Quarter of Section 11, Township 1N, Range 40E, Mount Diablo Meridian, Esmeralda County, Nevada from Gateway Gold & Minerals, Inc.

Eclipse Mine

The property is readily accessible via Highway 95 from Las Vegas to the South or Hwy’s 95/6 from the North/West from Northern Nevada/Reno or Bishop California, and from Highway 6 from the east which intersects highway 95 in the heart of Tonopah. This mine can be accessed by dirt roads using an ATV (all-terrain vehicle) or four-wheel drive vehicle and a GPS, main dirt roads leading through the mining district are maintained, but two track roads to the individual mines are often difficult to traverse. Caution is mandatory within the entire valley as it is dotted with abandoned mines – some of them are easy to see from a distance, and other are impossible to see until you are right on top of them. 20% of them are roped or fenced off – the rest do not have safety barriers and one should be extremely careful in entering them. Being situated in the high desert there are limited water sources in the area throughout 10 months out of the year.

Tonopah is located slightly inboard of the western margin of the Basin and Range province, and on the eastern margin of the “Walker Lane”,Lane,” a zone of Miocene structural deformation trending northwest to southeast parallel to the trend of the Sierra Madre Mountains in Eastern California. The Walker Lane can best be characterized as a broad zone of abundant strike-slip right-stepping faulting. The trend of the pre-Tertiary geologic units over much of the Walker Lane exhibits an arcuate pattern as a result of the influence of two major structural regimes. A series of these arcs have been identified by past workers with the Tonopah area having been identified as being within the Silver Peak-Palmetto- Montezuma Oroflex (Albers & Stewart 1972). The oroflex is described as southward convex with bedding, fold axes and faults trending to the northwest in the Silver Peak Range, trending east-west in the Palmetto Mountains and swinging around to the Northeast in the Montezuma Peak region. The Tonopah area lies on the eastern limb of the oroflex. The Walker Lane is also noted as being particularly well endowed with mineral deposits and the coincidence of these two structural regimes has created favorable plumbing, which is responsible for the high frequency of deposits in the region.

To the west of Tonopah, the White Mountains represent the westernmost range of the central Basin and Range province. They are situated to the east of the unextended Sierra Nevada Range and represent a crustal block that is bounded along its western flank by the high-angle White Mountains fault zone, with up to 8 km of total dip-slip displacement. Miocene volcanic rocks preserved along the eastern side of the range unconformably overlie Mesozoic granitic basement and dip up to 25° to the east, tilting occurred in the middle Miocene. The early geology of the general Tonopah region is relatively simple with the earliest Cambrian and Precambrian rocks comprised primarily of distal maritime facies - limestones, and dolomites with some hornfelsed shales. These are in fault contact with Ordivician limestones, argillites, and shales. From this point in time forward things become increasingly complex due to extensive volcanism in possibly alternating terrestrial and lacustrine settings. None of the Cambrian or Precambrian rocks outcrop in the immediate Tonopah area but fragments of these lithologies are present in volcanic breccias locally, so it is believed they form the basement of the volcanic complex.

The local geology is extremely well documented with geological investigations going back as early as 1905 when Spurr first published his voluminous observations of the camp. Spurr continued his work in the camp well into the 1920’s, followed by Bastin and Laney (1918), and later Nolan in 1930 published a study of the mines in the western part of the camp, and later expanded on this work, publishing a study that encompassed the entire camp in 1935. Later work was done in the area by Bonham (1970) and Bonham & Garside (1974 & 1979) during the time that work was carried out by Summa, Tenneco, and Houston Oil and Minerals. The earlier workers in the area had the distinct advantage of having the bulk of the mine workings available at one time or another for inspection, while the later workers had the ability to draw from all the earlier well-documented work.

Given the nature of this primarily felsic volcanic center, and the considerable alteration that has taken place prior, during and possibly somewhat after the mineralizing events, the geology of the camp is quite complex, and deciphering the history of the geology and mineralization of the area is only possible due to the thorough the attention paid to detail and the recording of these findings by earlier workers.

The “Early” andesite of the Mizpah formation is almost exclusively the host rock for mineralization, however Bonanza style lode mineralization of the epoch does extend into the later andesite and in certain mines above the Mizpah into the Extension Breccia, the West End Rhyolitic intrusive and into the Fraction Tuff. From relative positioning and age dating it has been established that the earliest mineralizing event occurred between 20.5m.y. to 17m.y. before present.

The later mineralization event occurred around the end of the emplacement of the Fraction Tuff.

At Three Hills the gold bearing discontinuous, irregular, narrow, brecciated chalcedony quartz veinlets, and stockworks occur in a zone of pervasive silicification of the Siebert Formation immediately above the contact with the Fraction Tuff. At Hasbrouck, some gold-silver mineralization is seen within the Fraction Tuff, near its contact with the overlying Siebert formation, which hosts the bulk of the gold-silver mineralized veinlet and stockwork deposits. These occur as erratic bodies of hydrothermal breccia accompanied by strong pervasive silicification with associated adularia and pyrite. Adularia associated with mineralization at the Divide deposit was dated at between 16.3m.y. and 16.4 m.y. before present.

No significant exploration completed prior to our exploration phase.

Recent exploration phase for these properties has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from $20,000 and $200,000. This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on 4/5/2019. The Niton XRF (X-Ray Fluorescence) instrument was used in mining mode to analyze 23 minerals with GOLDD Technology enabled. GOLDD Technology: When low detection limits and high sample throughput are critical, the Niton XL3t GOLDD+ XRF analyzer delivers measurement times up to 10-times faster than conventional Si-PIN detectors and up to 3-times more precise than conventional smaller silicon drift detectors (SDD) – without helium purge or vacuum. Niton analyzers also feature the highest performance X-ray tube and speed detector available on the market. Spectrographs were created for each sample and are included in Appendix C.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Fortuna & Eclipse Mines are combined and showed that the elements promising for economic benefiting are:are Gold, Titanium, Manganese, Iron, Arsenic, Rubidium, Strontium, Zirconium, Niobium, Hafnium, Tungsten, and Bismuth. These mines are adjacent to one another and were combined during mapping and analysis. The terrain was extreme and difficult to traverse. Limited samples were taken on slopes greater than 30% due to safety concerns. All visible pits, shafts and ridges were sampled, refer to Ni 43-101 Technical Report for further details. Due to limited samples many of the values were extrapolated from inputs into mapping software and thus should be considered when reviewing.

Nearby geological attractions include Lunar Crater, the Sump and Monte Cristo'sCristo’s Castle and there are five wilderness areas within hours of the community. The nearby Tonopah Test Range is the town’s main source of employment. The military has used the range and surrounding areas over the last half dozen decades as a nuclear test site, a bombing range, and as a base of operations for the development of the F-117 Nighthawk. Its location about halfway between Reno and Las Vegas as a stopover and rest spot on a lonely highway, the town has done fairly well. The Tonopah Station has slots, and the Banc Club also offers some gaming. Numerous restaurants, shops, gas stations and motels means it is a perfect place for staging while you work this mine.

Infrastructure is excellent in Tonopah district. Power is available at various points throughout the prospect, with a high-tension line running east-west along the northern margin of the Belmont tailings. Most supplies are available in Tonopah, while the nearest railhead is in Mina Nevada, approximately 85 kilometers (53 miles) to the northwest along highway 95. Manpower is available in the region, and personnel exist locally with training specific to the mining industry due to the proximity of the property to Kinross’s Round Mountain, and Scorpio Gold’s Mineral Peak operations. The owned claims all have cell phone service. Las Vegas is located approximately 280 kilometers (174 miles) to the southeast of the property, while Reno (which is an important mining supply center) is 270 kilometers (168 miles) to the northwest. The claim block area should be large enough to accommodate a production facility, and there are several potential processing plant sites in the area.

There is no developed infrastructure on this property.

Mine 7 – Fortuna

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found in the Fortuna Mine Property located in Tonopah, Nevada in Esmeralda County.

●The Probable Gross Gold Resources are 2,657,630.86 oz based on projected 200 feet excavation. This estimate includes the Eclipse mine claim. Due to the topography less, samples were taken at these two adjacent claims which leads to greater uncertainty in reserve numbers.

The Fortuna mine is lode and open-pit mines. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

The FORTUNA MINE lode mining claim, NMC1190597. The general course of this claim is North and South, and it is situated in the NW Quarter of Section 11, Township 1N, Range 40E, Mount Diablo Meridian, Esmeralda County, Nevada. This claim is 600 feet wide and 1,500 feet high. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in a Northerly direction to the North end line and approximately 300 feet in a Southerly direction to the South end line. This claim is marked by four (4) monuments, one at each corner of the claim. Additionally, there are two (2) end-line markers on each side of the center of the claim. All markers are 4"4” x 4"4” posts that are buried 1.5'1.5’ in the ground and protrude 4.5'4.5’ above the ground embossed with the name of the claim and its location in relation to the claim.

The location monument on which this notice is posted is situated within Section 11, Township 1N, Range 40E, Mount Diablo Meridian, Esmeralda County Nevada and this claim encompasses portions of the following quarter section (s), Township (s), and Range (s); NW 1/4 of NW 1/4 and SW 1/4 of NW 1/4 Section 11, T1N, R40E, Mount Diablo Meridian, Esmeralda County Nevada. The locality of this claim with reference to some natural object or permanent monument and additional information (if any) concerning its locality are as follows: NW corner of this claim is located 1,150 Feet South and 570 Feet East from the NW corner of Section 11, T1N, R40E. Beginning at the NW corner of this claim thence 1,500 feet due south to the SW corner of this claim, thence due east 600 feet to the SE corner of this claim, thence due north 1,500 feet to the NE corner of this claim, thence due west 600 feet back to the place of beginning, the NW corner.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMC1190597 in the NW Quarter of Section 11, Township 1N, Range 40E, Mount Diablo Meridian, Esmeralda County, Nevada from Gateway Gold & Minerals, Inc.

Fortuna Mine

The property is readily accessible via Highway 95 from Las Vegas to the South or Hwy’s 95/6 from the North/West from Northern Nevada/Reno or Bishop California, and from Highway 6 from the east which intersects highway 95 in the heart of Tonopah. This mine can be accessed by dirt roads using an ATV (all-terrain vehicle) or four-wheel drive vehicle and a GPS, main dirt roads leading through the mining district are maintained, but two track roads to the individual mines are often difficult to traverse. Caution is mandatory within the entire valley as it is dotted with abandoned mines – some of them are easy to see from a distance, and other are impossible to see until you are right on top of them. 20% of them are roped or fenced off – the rest do not have safety barriers and one should be extremely careful in entering them. Being situated in the high desert there are limited water sources in the area throughout 10 months out of the year.

Tonopah is located slightly inboard of the western margin of the Basin and Range province, and on the eastern margin of the “Walker Lane”,Lane,” a zone of Miocene structural deformation trending northwest to southeast parallel to the trend of the Sierra Madre Mountains in Eastern California. The Walker Lane can best be characterized as a broad zone of abundant strike-slip right-stepping faulting. The trend of the pre-Tertiary geologic units over much of the Walker Lane exhibits an arcuate pattern as a result of the influence of two major structural regimes. A series of these arcs have been identified by past workers with the Tonopah area having been identified as being within the Silver Peak-Palmetto- Montezuma Oroflex (Albers & Stewart 1972). The oroflex is described as southward convex with bedding, fold axes and faults trending to the northwest in the Silver Peak Range, trending east-west in the Palmetto Mountains and swinging around to the Northeast in the Montezuma Peak region. The Tonopah area lies on the eastern limb of the oroflex. The Walker Lane is also noted as being particularly well endowed with mineral deposits and the coincidence of these two structural regimes has created favorable plumbing, which is responsible for the high frequency of deposits in the region.

To the west of Tonopah, the White Mountains represent the westernmost range of the central Basin and Range province. They are situated to the east of the unextended Sierra Nevada Range and represent a crustal block that is bounded along its western flank by the high-angle White Mountains fault zone, with up to 8 km of total dip-slip displacement. Miocene volcanic rocks preserved along the eastern side of the range unconformably overlie Mesozoic granitic basement and dip up to 25° to the east, tilting occurred in the middle Miocene. The early geology of the general Tonopah region is relatively simple with the earliest Cambrian and Precambrian rocks comprised primarily of distal maritime facies - limestones, and dolomites with some hornfelsed shales. These are in fault contact with Ordivician limestones, argillites, and shales. From this point in time forward things become increasingly complex due to extensive volcanism in possibly alternating terrestrial and lacustrine settings. None of the Cambrian or Precambrian rocks outcrop in the immediate Tonopah area but fragments of these lithologies are present in volcanic breccias locally, so it is believed they form the basement of the volcanic complex.

The local geology is extremely well documented with geological investigations going back as early as 1905 when Spurr first published his voluminous observations of the camp. Spurr continued his work in the camp well into the 1920’s, followed by Bastin and Laney (1918), and later Nolan in 1930 published a study of the mines in the western part of the camp, and later expanded on this work, publishing a study that encompassed the entire camp in 1935. Later work was done in the area by Bonham (1970) and Bonham & Garside (1974 & 1979) during the time that work was carried out by Summa, Tenneco, and Houston Oil and Minerals. The earlier workers in the area had the distinct advantage of having the bulk of the mine workings available at one time or another for inspection, while the later workers had the ability to draw from all the earlier well-documented work.

Given the nature of this primarily felsic volcanic center, and the considerable alteration that has taken place prior, during and possibly somewhat after the mineralizing events, the geology of the camp is quite complex, and deciphering the history of the geology and mineralization of the area is only possible due to the thorough the attention paid to detail and the recording of these findings by earlier workers.

The “Early” andesite of the Mizpah formation is almost exclusively the host rock for mineralization, however Bonanza style lode mineralization of the epoch does extend into the later andesite and in certain mines above the Mizpah into the Extension Breccia, the West End Rhyolitic intrusive and into the Fraction Tuff. From relative positioning and age dating it has been established that the earliest mineralizing event occurred between 20.5m.y. to 17m.y. before present.

The later mineralization event occurred around the end of the emplacement of the Fraction Tuff.

At Three Hills the gold bearing discontinuous, irregular, narrow, brecciated chalcedony quartz veinlets, and stockworks occur in a zone of pervasive silicification of the Siebert Formation immediately above the contact with the Fraction Tuff. At Hasbrouck, some gold-silver mineralization is seen within the Fraction Tuff, near its contact with the overlying Siebert formation, which hosts the bulk of the gold-silver mineralized veinlet and stockwork deposits.

These occur as erratic bodies of hydrothermal breccia accompanied by strong pervasive silicification with associated adularia and pyrite. Adularia associated with mineralization at the Divide deposit was dated at between 16.3m.y. and 16.4 m.y. before present.

No significant exploration has been noted at these mines in a few decades so a historical account of publicly found data was assimilated.

Recent exploration phase for these properties has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from $20,000 and $200,000. This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on 4/5/2019. The Niton XRF (X-Ray Fluorescence) instrument was used in mining mode to analyze 23 minerals with GOLDD Technology enabled. GOLDD Technology: When low detection limits and high sample throughput are critical, the Niton XL3t GOLDD+ XRF analyzer delivers measurement times up to 10-times faster than conventional Si-PIN detectors and up to 3-times more precise than conventional smaller silicon drift detectors (SDD) – without helium purge or vacuum. Niton analyzers also feature the highest performance X-ray tube and speed detector available on the market. Spectrographs were created for each sample and are included in Appendix C.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Fortuna & Eclipse Mines are combined and showed that the elements promising for economic benefiting are:are Gold, Titanium, Manganese, Iron, Arsenic, Rubidium, Strontium, Zirconium, Niobium, Hafnium, Tungsten, and Bismuth. These mines are adjacent to one another and were combined during mapping and analysis. The terrain was extreme and difficult to traverse. Limited samples were taken on slopes greater than 30% due to safety concerns. All visible pits, shafts and ridges were sampled, refer to Ni 43-101 Technical Report for further details. Due to limited samples many of the values were extrapolated from inputs into mapping software and thus should be considered when reviewing.

Nearby geological attractions include Lunar Crater, the Sump and Monte Cristo’s Castle and there are five wilderness areas within hours of the community. The nearby Tonopah Test Range is the town’s main source of employment. The military has used the range and surrounding areas over the last half dozen decades as a nuclear test site, a bombing range, and as a base of operations for the development of the F-117 Nighthawk. Its location about halfway between Reno and Las Vegas as a stopover and rest spot on a lonely highway, the town has done fairly well. The Tonopah Station has slots, and the Banc Club also offers some gaming. Numerous restaurants, shops, gas stations and motels means it is a perfect place for staging while you work this mine.

Infrastructure is excellent in Tonopah district. Power is available at various points throughout the prospect, with a high-tension line running east-west along the northern margin of the Belmont tailings. Most supplies are available in Tonopah, while the nearest railhead is in Mina Nevada, approximately 85 kilometers (53 miles) to the northwest along highway 95. Manpower is available in the region, and personnel exist locally with training specific to the mining industry due to the proximity of the property to Kinross’s Round Mountain, and Scorpio Gold’s Mineral Peak operations. The owned claims all have cell phone service. Las Vegas is located approximately 280 kilometers (174 miles) to the southeast of the property, while Reno (which is an important mining supply center) is 270 kilometers (168 miles) to the northwest. The claim block area should be large enough to accommodate a production facility, and there are several potential processing plant sites in the area.

Three (3) Mines here – one shaft and 2 adits. The shaft is cut on an ancient riverbed. Two Adits/Tunnels are very solid and cut from hard rock right across the wash.

Mine 8 – Purple Heart

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found the Purple Heart Mine Property located in Buckhorn, New Mexico, in Grant County.

The Probable Gross Gold Resources are 1,184,332.39 oz based on projected 200 feet excavation.

The mine is a lode mine. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

The general course of this claim is East and West, and it is situated in the SE quarter of Section 3, T18S, R17W, New Mexico Meridian, Grant County, New Mexico. This claim is 1,500 feet in length and 600 feet in width. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in an Easterly direction to the East end line and approximately 300 feet in a Westerly direction to the West end line. The claim excludes any and all patented mining claims and Federal Highways located within said boundaries. This claim is marked by four (4) monuments, one at each corner of the claim. Additionally, there are two (2) end-line markers on each side of the center of the claim. All markers are 4” x 4” posts that are buried 1.5’ in the ground and protrude 4.5’ above the ground embossed with the name of the claim and its location in relation to the claim. The location monument on which this notice is posted is situated within Section 3, Township 18S, Range 17W, New Mexico Meridian, Grant County, New Mexico. This claim encompasses portions of the following quarter section (s), Township (s), and Range (s); NE 1/4 of SE 1/4 and NW 1/4 of SE 1/4 of S3, T18S, R17W, New Mexico Meridian, Grant County, New Mexico. More specifically, the locality of this claim with reference to some natural object or permanent monument and 0 feet West of the SSE corner pf Section 3, T18S, R17W.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMMC200984 in the SE quarter of Section 3, T18S, R17W, New Mexico Meridian, Grant County, New Mexico from Gateway Gold & Minerals, Inc.

Purple Heart Mine

The Black Hawk mining district is mostly in sections. 20, 21, 22, 28, and 29, T. 18 S., R. 16 W., in Grant County, N. Mex., and is 21 miles by road west of Silver City, the terminus of a branch line of the Atchison, Topeka and Santa Fe Railway. Access roads are plentiful being situated in Gila National Forest with thousands of miles of off-road vehicle trails. A four-wheel drive, high ground clearance vehicle with good tires is highly recommended due to large rock obstacles and deep sandy washes that must be traversed to access the mines.

The 12’ tall and 15’ wide entrance of Purple Heart mine is partially blocked by a tree and some brush but is still easy to access on foot. The mine shaft is visible for 70-feet before water prohibits the full exploration of the shaft(s). Local ranchers have used this water for decades to fill cattle troughs, so it is likely replenished every year during the wet season. The adit will not be entirely explored without dewatering the mine. Evidence of old tracking and tailings onsite indicated that the workings on this main adit will likely be extensive.

The oldest rocks in the Black Hawk mining district belong to the Proterozoic Bullard Peak Group, which includes quartzite, amphibolite, migmatite and various types of schist and gneiss (Hewitt, 1959; Gillerman, 1964). Intruding these rocks is Proterozoic quartz diorite gneiss, which is the predominant rock in the area and part of the Burro Mountain batholith that crops out extensively to the south and southwest of the area (Gillerman, 1964). The gneiss, which contains 35 ppm Co and 23 ppm Ni (Gerwe and Norman, 1985), is in turn intruded by Tertiary Twin Peaks monzonite porphyry and other rock types.

The Twin Peaks monzonite stock also occurs as dikes and irregular masses in the northern portion of the district (Gillerman, 1964). This monzonite contains approximately 20 ppm Co and 11 ppm Ni (Gerwe and Norman, 1985), is Late Cretaceous age (72.5 +- 4.7 Ma; Hedlund, 1985a), and is associated with the mineralized veins. A whole-rock sample of altered material adjacent to a vein has an age date of 65.3 +- 1.2 Ma (K-Ar; Gerwe, 1986). Metamorphic and igneous rocks are overlain by Cretaceous quartzite and Tertiary rhyolite in the northern area of the district (Gillerman, 1964).

Two prominent fault systems trending slightly east of north are the main geologic structures in the district (Gillerman, 1964). Each fault system consists of a rather persistent fault from which other faults split off, trending to the northeast or northwest.

The oldest rocks in the Black Hawk mining district belong to the Proterozoic Bullard Peak Group, which includes quartzite, amphibolite, migmatite and various types of schist and gneiss (Hewitt, 1959; Gillerman, 1964). Intruding these rocks is Proterozoic quartz diorite gneiss, which is the predominant rock in the area and part of the Burro Mountain batholith that crops out extensively to the south and southwest of the area (Gillerman, 1964). The gneiss, which contains 35 ppm Co and 23 ppm Ni (Gerwe and Norman, 1985), is in turn intruded by Tertiary Twin Peaks monzonite porphyry and other rock types.

The Twin Peaks monzonite stock also occurs as dikes and irregular masses in the northern portion of the district (Gillerman, 1964). This monzonite contains approximately 20 ppm Co and 11 ppm Ni (Gerwe and Norman, 1985), is Late Cretaceous age (72.5 +- 4.7 Ma; Hedlund, 1985a), and is associated with the mineralized veins. A whole-rock sample of altered material adjacent to a vein has an age date of 65.3 +- 1.2 Ma (K-Ar; Gerwe, 1986). Metamorphic and igneous rocks are overlain by Cretaceous quartzite and Tertiary rhyolite in the northern area of the district (Gillerman, 1964).

Two prominent fault systems trending slightly east of north are the main geologic structures in the district (Gillerman, 1964). Each fault system consists of a rather persistent fault from which other faults split off, trending to the northeast or northwest.

The unusual nickel-cobalt-silver deposits of the Black Hawk mining district make the area one of special interest. Although similar deposits are described worldwide (Cobalt and Great Bear Lake in Canada and Joachimstah in the former Czechoslovakia (Gillerman and Whitebread, 1956), few known deposits have nickel- cobalt-silver ore with uraniumin carbonate gangue (Gillerman, 1964). In the Black Hawk district, the mineral deposits are simple fissure-filling veins mostly in the quartz diorite gneiss near bodies of monzonite porphyry.

Four mineral assemblages occur: 1) silver-argentite-uraninite-niccolite-te-rannneisberg. 2) silver- rammeisbergite—gersdorffite—nickel skutterudite. 3) chalcopyrite-tennantite-galena-sphalerite. And 4) acanthite-jalpaite-pearceite-covellite (Von Bargen, 1979, 1993). Pitchblend is found with minor pyrite, chalcopyrite, galena, and sphalerite.

Other minerals occurring in these deposits are millerite, erythrite, annabergite, barite, manganocalcite, and various nickel and cobalt sulfarsenides and arsenides (Gillerman, 1964; Von Bargen, 1979, 1993). Deposits are most plentiful in a 1-mi-wide by as much as 3-mi-long area on the southwest side of Twin Peak stock (Gillerman, 1964). The veins can be traced for more than 1,000 ft and have reached as much as 600 ft vertically. They vary in width from 1 to 3 ft but may open to as much as 10 ft wide where they cut quartz diorite gneiss.

The veins are inconspicuous in outcrop and are recognized by brown-stained, carbonate filling (Gillerman, 1964). The carbonates, largely calcite, dolomite, siderite and ankerite, are the most common vein minerals. Quartz is rare, occurring as a dull yellow-green chert or chalcedony. A dump sampled assayed 0.005 % U308, 0.08% Cu, 0.05% Pb, 0.06% Zn, and 0.0052% Ni (McLemore, 1983, #3745). Mineralization occurred about 65.3 +/-1.2 Ma ago and at temperatures of 29O deg - 41O deg C (Gewe, 1986). Low salinities of fluid inclusions (<2 eq. wt.% NaCl) suggest that the water in the system was meteoric (Gewe, 1986; Gewe and Norman, 1985).

Larmide veins consist of native gold and native silver, with silver occurring in the central part of the vein and nickel-and cobalt-bearing minerals, mostly nickel skutterudite, are on the vein margins (Gillerman, 1968). Uraninite is found mostly in the outermost zones associated with nickel-and cobalt- bearing minerals, not with silver. The carbonate vein-minerals form in a sequence where the carbonate species calcite, dolomite, ankerite and siderite replace one another due to increased carbon dioxide in the mineralizing solutions at a constant temperature (Naumov et al., 1971).

The Purple Heart Mine is one of the original mines in the district, and records show that it has changed hands and been worked on several occasions since the turn of the century. The main workings consist of a massive adit cut on a gentle 20-degree downward slope. The entrance is huge - about 12’ feet tall and 15’ wide. You could drive a truck in there.

At 70-feet in the mine is full of water - local ranchers have used this water for decades to feed cattle troughs, so it is likely replenished every year during the wet season. The Black Hawk or Bullard Peak mining districts in the northern Burro Mountains, is approximate 21 miles west of Silver City, NM. The district includes all of the mines and prospect pits within five miles to the east and south of Bullard Peak. Mining began in the district in 1881 with the discovery of the unique gold-silver-nickel-cobalt deposit at the Alhambra mine (Gilleman and Whitebread, 1956).

Subsequent prospecting soon discovered additional deposits. Mining continued until 1893, when a decline in silver price and depletion of rich silver ore caused the mines to close. During 1917, the Black Hawk mine was dewatered, but recorded production numbers varied by report. In 1920, pitchblende (uraninite) was recognized in the mine dumps of the area, and in 1949 the area became of interest as a possible source of uranium, gold, silver, nickel, and cobalt.

Recent exploration phase for these properties has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from $20,000 and $200,000. This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on 4/5/2019. The Niton XRF (X-Ray Fluorescence) instrument was used in mining mode to analyze 23 minerals with GOLDD Technology enabled. GOLDD Technology: When low detection limits and high sample throughput are critical, the Niton XL3t GOLDD+ XRF analyzer delivers measurement times up to 10-times faster than conventional Si-PIN detectors and up to 3-times more precise than conventional smaller silicon drift detectors (SDD) – without helium purge or vacuum. Niton analyzers also feature the highest performance X-ray tube and speed detector available on the market. Spectrographs were created for each sample and are included in Appendix C.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Purple Heart showed that the elements promising for economic benefiting are:are Gold, Titanium, Manganese, Iron, Arsenic, Rubidium, Strontium, Zirconium, Niobium, and Bismuth

There are no close-by power lines, gas lines, or settlements occur near the Purple Heart property.

The Black Hawk or Bullard Peak mining districts in the northern Burro Mountains is approximate 34 kilometers (21 miles) West of Silver City, NM. The district includes all of the mines and prospect pits within five miles to the east and south of Bullard Peak. Infrastructure is great due to proximity to Silver City which is a railhead and former mining town itself. The population of Silver City is adequate to provide a skilled work force. Electricity is available, but it is likely that additional electrical capacity would need to be added to accommodate modern mining activities.

There is no developed infrastructure on this property.

Mine 9 – Blackmoor

Pursuant to the Purchase and Merger Agreement of September 17, 2019, the Company acquired an undivided one hundred percent (100%) interest and deed in and to certain mineral interests found in the Blackmoor Mine Property located in Buckhorn, New Mexico, in Grant County.

The Probable Gross Gold Resources are 1,324,363.81 oz based on projected 200 feet excavation. It should be noted that due to the topography and vegetation, many sample locations were difficult to access and mapping software was used to model much of this claim.

The mine is a lode mine. As defined by the U.S. Department of the Interior Bureau of Land Management, deposits subject to lode claims include classic veins or lodes having well-defined boundaries. They also include other rock in- place bearing valuable minerals and may be broad zones of mineralized rock. Examples include quartz or other veins bearing gold or other metallic minerals and large volume, but low-grade disseminated gold deposits. Descriptions are by metes and bounds surveys beginning at the discovery point on the claim and including a reference to natural objects or permanent monuments. Federal statute limits their size to a maximum of 1500 feet in length, and a maximum width of 600 feet (300 feet on either side of the vein).

The general course of this claim is East and West, and it is situated in the SW quarter of Section 3, T18S, R17W, New Mexico Meridian, Grant County, New Mexico. This claim is 1,500 feet in length and 600 feet in width. This claim runs from the location monument on which this location notice is posted approximately 1,200 feet in an Easterly direction to the East end line and approximately 300 feet in a Westerly direction to the West end line. The claim excludes any and all patented mining claims and Federal Highways located within said boundaries. This claim is marked by four (4) monuments, one at each corner of the claim. Additionally, there are two (2) end-line markers on each side of the center of the claim. All markers are 4” x 4” posts that are buried 1.5’ in the ground and protrude 4.5’ above the ground embossed with the name of the claim and its location in relation to the claim. The location monument on which this notice is posted is situated within Section 3, Township 18S, Range 17W, New Mexico Meridian, Grant County, New Mexico. This claim encompasses portions of the following quarter section (s), Township (s), and Range (s); NW 1/4 of SW 1/4 and NE 1/4 of SW 1/4 of S3, T18S, R17W, New Mexico Meridian, Grant County, New Mexico. More specifically, the locality of this claim with reference to some natural object or permanent monument and additional information (if any) concerning its locality are as follows: SW corner of this claim is 1,775 feet North and 0 feet East of the SW corner of Section 3, T18S, R17W.

WSA Gold & Minerals, Inc. acquired a 100% undivided, transferable interest in Serial No. NMMC200983 in the SW quarter of Section 3, T18S, R17W, New Mexico Meridian, Grant County, New Mexico.

Blackmoor Mine

The Black Hawk mining district is mostly in sections. 20, 21, 22, 28, and 29, T. 18 S., R. 16 W., in Grant County, N. Mex., and is 21 miles by road west of Silver City, the terminus of a branch line of the Atchison, Topeka and Santa Fe Railway. Access roads are plentiful being situated in Gila National Forest with thousands of miles of off-road vehicle trails. A four-wheel drive, high ground clearance vehicle with good tires is highly recommended due to large rock obstacles and deep sandy washes that must be traversed to access the mines.

Blackmoor Mine lies almost at the end of the road before you get to the Gila River, and extensive excavations include a large 2-acre leveled staging area for equipment within a few hundred feet of the mine. The roads are in fairly good shape to access the mine, but there are a few spots that are fairly steep and narrow, so good clearance and good tire tread is recommended.

The Black Hawk or Bullard Peak mining districts in the northern Burro Mountains, is approximate 21 miles west of Silver City, NM. The district includes all of the mines and prospect pits within five miles to the east and south of Bullard Peak. Mining began in the district in 1881 with the discovery of the unique gold-silver-nickel-cobalt deposit at the Alhambra mine (Gilleman and Whitebread, 1956). Subsequent prospecting soon discovered additional deposits. Mining continued until 1893, when a decline in silver price and depletion of rich silver ore caused the mines to close. During 1917, the Black Hawk mine was dewatered, but recorded production numbers varied by report.

In 1920, pitchblende (uraninite) was recognized in the mine dumps of the area, and in 1949 the area became of interest as a possible source of uranium, gold, silver, nickel, and cobalt. Types of deposits found in the Black Hawk mining district include Laramide veins, tungsten placer deposits, and pegmatites. Total metal production from 1881-1960 is estimated as 3,000 lbs Cu, 1,000 oz Au, 1,286,000 oz Ag, and 4,000 lbs Pb. In addition, 10,542 short tons of (2.7-71 % WO,) tungsten ore (Richter and Lawrence, 1983; Dale and McJGnney, 1959) and 615 short tons of fluorspar ore have been produced (Williams, 1966; McAnulty, 1978).

The oldest rocks in the Black Hawk mining district belong to the Proterozoic Bullard Peak Group, which includes quartzite, amphibolite, migmatite and various types of schist and gneiss (Hewitt, 1959; Gillerman, 1964). Intruding these rocks is Proterozoic quartz diorite gneiss, which is the predominant rock in the area and part of the Burro Mountain batholith that crops out extensively to the south and southwest of the area (Gillerman, 1964). The gneiss, which contains 35 ppm Co and 23 ppm Ni (Gerwe and Norman, 1985), is in turn intruded by Tertiary Twin Peaks monzonite porphyry and other rock types.

The Twin Peaks monzonite stock also occurs as dikes and irregular masses in the northern portion of the district (Gillerman, 1964). This monzonite contains approximately 20 ppm Co and 11 ppm Ni (Gerwe and Norman, 1985), is Late Cretaceous age (72.5 +- 4.7 Ma; Hedlund, 1985a), and is associated with the mineralized veins. A whole-rock sample of altered material adjacent to a vein has an age date of 65.3 +- 1.2 Ma (K-Ar; Gerwe, 1986). Metamorphic and igneous rocks are overlain by Cretaceous quartzite and Tertiary rhyolite in the northern area of the district (Gillerman, 1964).

Two prominent fault systems trending slightly east of north are the main geologic structures in the district (Gillerman, 1964). Each fault system consists of a rather persistent fault from which other faults split off, trending to the northeast or northwest.

The main mine consists of a large shaft cut to a depth of 25 feet with two horizontal adits/workings consisting of more than 2,800 feet in length heading northeast and southwest at the 25- foot level. Both adit entrances are largely blocked by natural erosion but would take more than a few hours of work to reopen and explore. There are extensive tailings onsite as well as a large wash that runs past the base of the tailings, which we would also recommending working. The old head frame and a reported cabin are long gone, but the mine is cut only a few feet from the road, so you will be able to work this one fairly easily.

The unusual nickel-cobalt-silver deposits of the Black Hawk mining district make the area one of special interest. Although similar deposits are described worldwide (Cobalt and Great Bear Lake in Canada and Joachimstah in the former Czechoslovakia (Gillerman and Whitebread, 1956), few known deposits have nickel- cobalt-silver ore with uraniumin carbonate gangue (Gillerman, 1964). In the Black Hawk district, the mineral deposits are simple fissure-filling veins mostly in the quartz diorite gneiss near bodies of monzonite porphyry.

Four mineral assemblages occur: 1) silver-argentite-uraninite-niccolite-te-rannneisberg. 2) silver- rammeisbergite—gersdorffite—nickel skutterudite. 3) chalcopyrite-tennantite-galena-sphalerite. And 4) acanthite-jalpaite-pearceite-covellite (Von Bargen, 1979, 1993). Pitchblend is found with minor pyrite, chalcopyrite, galena, and sphalerite.

Other minerals occurring in these deposits are millerite, erythrite, annabergite, barite, manganocalcite, and various nickel and cobalt sulfarsenides and arsenides (Gillerman, 1964; Von Bargen, 1979, 1993). Deposits are most plentiful in a 1-mi-wide by as much as 3-mi-long area on the southwest side of Twin Peak stock (Gillerman, 1964). The veins can be traced for more than 1,000 ft and have reached as much as 600 ft vertically. They vary in width from 1 to 3 ft but may open to as much as 10 ft wide where they cut quartz diorite gneiss. The veins are inconspicuous in outcrop and are recognized by brown-stained, carbonate filling (Gillerman, 1964). The carbonates, largely calcite, dolomite, siderite and ankerite, are the most common vein minerals. Quartz is rare, occurring as a dull yellow-green chert or chalcedony. A dump sampled assayed 0.005 % U308, 0.08% Cu, 0.05% Pb, 0.06% Zn, and 0.0052% Ni (McLemore, 1983, #3745).

Mineralization occurred about 65.3 +/-1.2 Ma ago and at temperatures of 29O deg - 41O deg C (Gewe, 1986). Low salinities of fluid inclusions (<2 eq. wt.% NaCl) suggest that the water in the system was meteoric (Gewe, 1986; Gewe and Norman, 1985).

Larmide veins consist of native gold and native silver, with silver occurring in the central part of the vein and nickel-and cobalt-bearing minerals, mostly nickel skutterudite, are on the vein margins (Gillerman, 1968). Uraninite is found mostly in the outermost zones associated with nickel-and cobalt- bearing minerals, not with silver. The carbonate vein-minerals form in a sequence where the carbonate species calcite, dolomite, ankerite and siderite replace one another due to increased carbon dioxide in the mineralizing solutions at a constant temperature (Naumov et al., 1971).

The Blackmoor Mine is one of the original mines in the Black Hawk District. Reportedly one of the larger producers of gold, silver, nickel, and cobalt, more than 25,000 tons of ore have been attributed to this large operation.

Recent exploration phase for these properties has been completed.

This mine is subject to permitting before boreholes can be drilled for exploration purposes. Based on BLM regulations if the disturbance is less than 5 acres on the claim, a right to explore notice can be obtained within 2 weeks in accordance with the code of federal regulations 43 CFR 3809.301. An assurance bond in the form of a cash will need to be filed with the state for reclamation purposes. After boreholes are plugged and surface is reclaimed with a self-sustaining plant community then the bond can be released, and another 5 acres of disturbance can be utilized in the same manner. Bonds will range from $2,000 and $30,000 depending on the vegetation present. If more than 5 acres are disturbed, then it is a 2-year process with environmental studies that will be required before exploratory drilling can occur. Environmental studies can range from $20,000 and $200,000.This will be required when we move to the implementation phase.

Twenty-Three minerals were analyzed at each sample point by a Niton XL3T 980 GOLDD+ XRF. Values were recorded in ppm (parts per million) for each sample along with GIS coordinates from a Garmin E-trex 30x for georeferencing. Where available, rock samples were analyzed by XRF on a clean surface exposure created by chipping the surface with a rock hammer. Quaternary alluvium was analyzed by XRF when rock samples were not available. Holes were dug 6-8 inches below the surface and then the grains were pulverized using the flat end of rock hammer that was cleaned using disposable cleaning pads between each sample.

Samples were analyzed using a Niton XL3T 980 GOLDD+ XRF, Serial #55948 that was calibrated by Thermo Scientific on 4/5/2019. The Niton XRF (X-Ray Fluorescence) instrument was used in mining mode to analyze 23 minerals with GOLDD Technology enabled. GOLDD Technology: When low detection limits and high sample throughput are critical, the Niton XL3t GOLDD+ XRF analyzer delivers measurement times up to 10-times faster than conventional Si-PIN detectors and up to 3-times more precise than conventional smaller silicon drift detectors (SDD) – without helium purge or vacuum. Niton analyzers also feature the highest performance X-ray tube and speed detector available on the market. Spectrographs were created for each sample and are included in Appendix C.

Data came from two separate programs and were manually merged into a database using Microsoft Excel. The data was then scrutinized to remove any obvious errors, whether it was sample exposure time, or erroneous readings. This data was then manually brought into mapping software and double verified data to ensure there were no errors while migrating data. With approximately 100 ft grid spacing between sample points, it was determined that mapping using least squares algorithm produced the best fit maps for the collected data. Grid flexing was enabled to model data beyond the data points to extend past the mine; although this adds some ambiguity to the edge data it produced much cleaner maps. All data points were created using GIS data collected from the Garmin E-trex 30x coupled with ppm reading recorded from the Niton GOLDD XRF. Surface outcrops were also mapped by hand to help understand subsurface geology. The output maps with their full analysis are shown in the following section.

The analysis of the XRF measurements of Blackmoor showed that the elements promising for economic benefiting are:are Gold, Titanium, Manganese, Iron, Arsenic, Rubidium, Strontium, Zirconium, Niobium, Hafnium and Bismuth. It should be noted that most samples were obtained in and around the main shaft and random locations around the mine claim. Due to the steep terrain and heavy vegetation, it was not possible to take many of the planned samples. Please see maps and sample data in NI 43-101 Technical Report for reference.