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ALT.V ·

Alturas Signs agreement for the Resguardo Copper-Gold Project in the Paleocene-Eocene Metallogenic Belt of Northern Chile

Corporate Updates

PRESS RELEASE TSXV, BVL: ALT

Alturas Signs agreement for the Resguardo Copper-Gold Project in the

Paleocene-Eocene Metallogenic Belt of Northern Chile

Toronto, December 18, 2023 – After a long negotiation and due diligence period, Alturas Minerals Corp.

(Alturas or the “Company”) (TSX-V, BVL: ALT) is pleased to announce that is has moved forward with the

execution of the Option and Lease agreement with Sociedad Contractual Minera Resguardo (“ Minera

Resguardo” or the “ Optionor”), a Chilean mining exp loration company, to lease and acquire 100% of its

Resguardo Copper-Gold Project (the “Concessions” or “Resguardo”), located about 95 km northeast of

Copiapo, in Region III of northern Chile, referred to as “Región de Atacama”.

The transaction remains subject to regulatory and TSX -V approvals, which is in the process of reviewing

all the required documentation. Closing will occur on receipt of these approvals.

Alturas is exploring the possibility of obtaining a permit to extract ore from the existing open pit mine on

the property within six to nine months to generate cash flow to fund Alturas’ future costs”.

As part of its due diligence, the Company has initiated environmental permitting, delineated target areas

and defined its exploitation and production approach.

Miguel Cardozo, President & CEO of Alturas commented , “The Resguardo project represents a key

strategic development for the Company in Chile, one of Latin America’s premier mining jurisdictions.

Alturas will resume its exploration activit ies in Chile’s mineral-rich Andes Mountain chain. The

agreement also includes a 4-year mining lease agreement that allows the Company to explore and

commercially mine 18 contiguous mining concessions covering a total of 3,891 hectares. Alturas intends

to establish a firm presence in the Paleocene-Eocene Metallogenic Belt of northern Chile, immediately

west of the Miocene age Maricunga Metallogenic Belt”.

The Transaction

With the execution of the Agreement, the Optionor grant Alturas a mining option (the “Option”) to

acquire a one hundred percent (100%) undivided interest in the Concessions. On closing, t he Option will

be valid as from May 31, 2023 (the “Effective Date”) and will expire four (4) years after the signing of the

Agreement. The term of the Option shall be mandatory for the Optionor and voluntary for Alturas.

The aggregate purchase price for the Concessions is structured as cash payment s totaling US$2.75

Million (all taxes inclusive), to be paid in five (5) installments, with US$50,000 within f ifteen days of the

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closing date (of which $25,000 has been paid as deposit with the balance held in escrow) , and four (4)

installments payable as follows:

• On or prior to the first anniversary of the Effective Date, the amount of US$100,000;

• On or prior to the second anniversary of the Effective Date, the amount of US$150,000;

• On or prior to the third anniversary of the Effective Date, the amount of US$300,000; and,

• On or prior to the fourth anniversary of the Effective Date, the amount of US$2,150,000.

If, as a result of the mining activities performed by Alturas on the Concessions, a porphyry is confirmed,

the purchase price for acquiring title over the Concessions payable by Alturas to the Optionor will be

increased by ten percent (10%) of the selling price obtained by Alturas for the transfer of the

Concessions to a third party, or US$30 Million, whichever is greater.

Once the Company exercises the Option, a 1.5% Net Smelter Return (“NSR”) Royalty will be applicable

(the “NSR Royalty”) as an additional consideration for the transfer of the Concession to be effective as

from commencement of Commercial Product ion on the Concessions. Until up two (2) years after the

commencement of Commercial Production, the Company may buy five tenths’ percent (0.5%) of the

NSR Royalty (the “Purchased NSR”) at a price between US$2 Million and US$6 Million depending on the

size, grade, and type of mineralization as determined in accordance with National Instrument 43-101

(“NI 43-101”). The Optionor also grants a right of fir st refusal for the acquisition of the remaining NSR

Royalty.

Mining Lease:

During the term of the Option, the Optionor shall also lease the Concessions (the “Mining Lease”) to the

Company, as result of which Alturas will be conferred all the rights and obligations of the Optionor

related to the Concessions, including the right to exploit the Concessions.

The Mining Lease shall be for a period of five (5) years and begins on the Effective Date or, whichever

arrives first, when Alturas notifies the Optionor of its decision to exercise the Option.

Once the Mining Lease is in force, Alturas shall have the right to operate the Concessions at its own sole

cost and risk, subject to compliance with applicable laws, shall have the right to initiate commercial

production of the existing high-grade copper mineralization.

As compensation required for the Mining Lease, Alturas will pay the Optionor a NSR Royalty over all the

minerals extracted and marketed from the Concessions (the “Lease NSR Royalty”). If the mineral

extracted has an average ore grade that is lower than 2.5%, the Lease NSR Royalty will be equivalent to

7.0% of the price at which said mineral is marketed; and, if the mineral extracted has an average ore

grade that is equal to or higher than 2.5%, the Lease NSR Royalty will be equivalent to 9.0% of such

price.

Resguardo Geology and Mineralization

Copper structures on the Resguardo consist of sub -vertical and tabular stockwork bodies (in parts

hydrothermal breccia) that host disseminated and vein co pper mineralization exceeding 2.0% Cu, along

with sub -parallel copper- gold veins. The main mineralized copp er body, which has been historically

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mined, has an average width of 50 to 100 m and is about 1.5 km in length . Historical open pit and

underground mine workings are scattered along the 1.5 km length with areas of mineralization that

often exceed 2.0% Cu-equivalent grade.

Besides exploring the high -grade copper structures and the potential copper porphyry system, the

Company intends to undertake an ini tial small-scale mining operation of the high -grade material. The

maximum tonnage allowed by Chilean regulations is 5,000 tonnes per month. This activity will be of

great help in defining the actual extension and quality of the high -grade copper mineralization with the

view of a future mid-size operation and will generate significant cash-flow to the Company to support its

activities in the Concessions and future exploration projects in Chile.

Given the already known copper mineralization at or near surface and the extensive and intense

hydrothermal alteration covering kilometres of area, there is a high probability that known copper oxide

and sulphide mineralization is genetically connected to a yet unconfirmed porphyry system (i.e., Late

Eocene-Early Oligocene) located topographically lower and therefore deeper in the mineralized system.

Evidence for the possibility of a porphyry system is supported by recent induced polarization and

magnetic geophysical surveys which have delineated a deep -seated chargeability high overlapping the

edge of a magnetic low, the latter which was likely produced by magnetite dest ruction as a result of

hydrothermal fluid movement.

The following has been extracted from a NI 43 -101 technical Reports authored by Dr. Scott Jobin -

Bevans, Principal geoscientist with Caracle Creek International Consulting Inc.

The Resguardo Copper-(Gold) Project and the Paleocene-Eocene Metallogenic Belt (“PEMB”)

The Resguardo Project is located about 45 km southwest of La Coipa Au- Ag Mine (Kinross Gold Corp: Compañía

Minera Mantos de Oro) and about 85 km northeast of Candelaria Copper Mine (Lundin Mini ng)”. Access to the

Resguardo Copper Project is excellent, starting from the southeast end of the City of Copiapó, travelling northeast

on highway 31 for about 85 km to the Quebrada Cortadera access road. Heading northwest on the Quebrada

Cortadera access road for about 5.5 km brings you to the central area of the Project and the historical workings at

the historical mine site. The Project is currently at the exploration stage and Optionor ship of surface rights are

usually not contemplated or necessary unti l a decision to mine has been made. The Mining Code of Chile

guarantees the Optionor of mining concessions the right-of-access to the surface area required for their exploration

and exploitation.

The Resguardo Copper Project lies within Paleocene- Eocene Metallogenic Belt of northern Chile, immediately west

of the Miocene age Maricunga Metallogenic Belt (see Figure 1) . The Project is within the morpho structural zone

known as the Cordillera Domeyko (aka Andean Pre- Cordillera), a region underlain by Paleocene, Eocene and Early

Oligocene Epoch magmatic arc rocks comprising a north -south linear belt. Rocks consist of basaltic to rhyolitic lavas

and tuffs, subvolcanic porphyritic intrusions, and granitoid stocks, which extend from southern Peru to central Chile.

The Paleocene- Eocene porphyry and epithermal Metallogenic Belt hosts a diverse range of mineral deposits and

occurrences, including large-scale porphyry Cu-Mo deposits like BHP Billiton’s Spence Mine (e.g., Sillitoe and McKee,

1996) and Codelco’s El Salv ador Mine (e.g., Gustafson and Hunt, 1975) and low sulphidation epithermal deposits

like Yamana Gold’s El Peñon (e.g., Warren et al., 2004, 2008).

On the Property, in the areas around the historical underground and open pit mines, rocks have experienced

pervasive and intense hydrothermal alteration that includes sericitic, silicic -argillic and propylitic alteration. In the

copper mineralized zones, th e host rock generally shows a hydrothermal alteration of the silicic -argillic type that

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grades laterally to an aureole of weak and irregular propylitic alteration (with epidote and chlorite). Hydrothermal

alteration (both silicic -argillic and propylitic) of the host rock in the extreme western parts of the Property is much

less intense and locally non-existent.

A complex mineralized system dominated by copper but with ancillary gold and silver mineralization exists on the

Resguardo Copper Project, with muc h of the known mineralization focused in the area of the historical workings

and underground mine. Most copper mineralization occurs as disseminated and veinlet copper oxide species but

stockworks, hydrothermal breccias and larger vein systems are also known to occur (Frutos, 2014).

The main east -west mineralized trend, referred to as the Cerro Fraga Mineralized System (“CFMS”), extends for

more than 2 km and with widths from 300 to 500 metres (Frutos, 2014). This copper zone is characterized by areas

of intense hydrothermal alteration with upper areas of oxidized and leached lithologies, hydrothermal breccias, and

veins and stockworks. The main mineralization that has been historically targeted consists of copper oxides and

copper sulphides which in some areas carry important concentrations of silver and gold in structurally controlled

veins that have been historically worked by artisanal miners.

Within the CFMS, principal copper structures consist of sub- vertical and tabular stockworks bodies (in parts

hydrothermal breccia) that are interpreted to be structurally controlled (east -west and sub- vertical), with

disseminated and vein copper mineralization, and sub- parallel veins of copper -gold trending N70 -100E (Frutos,

2014). The main mineralized copper body which has been historically mined has an average width of 50 to 100 m

and is about 1.5 km in length, with good outcrops and several historical open pit and underground mine workings

scattered along its length.

The principal deposit type being explored for on the Property is Porphyry Copper Deposit or “PCD”. Mineralized

systems associated with a PCD system commonly include polymetallic skarn, carbonate replacement and

stratabound (i.e., Manto -style copper), sediment -hosted gold silver, and high, intermediate and low sulphidation

epithermal silver-gold-base metal deposit types (Sillitoe and Perello, 2005; Sillitoe, 2010).

Mineralization styles (replacement Manto -style copper with pervasive disseminated copper oxides and sulphides

and veining) and intense hydrothermal alteration (alunite, kaolinite, illite, lesser propylitic) observed in the

historical workings on the Property, coupled with recent evidence from geophysical surveys support the PCD model

and provide targets for a future exploration program.

The Project area has sufficient size to accommodate a mining operation without any negative impact on the

environment. The area corresponds to the high desert climate of the Atacama Region with only trace rainfall most

of the year and with most precipitation as minor snow in winter months (June- September). Given its excellent

accessibility and climate, all types of exploration activities can be performed year-round.

The Resguardo Copper Project does not have any current mineral resources or mineral reserves and despite having

some historical copper production, is best described as an early -stage exploration project. Historical exploration

work (geological mapping, trenching, geophysical surveys, drilling) and small -scale copper mining is known to have

been completed within the Project area, dating back decades and most recently in 2020. Most of the information

and data available from historical exploration work on the Property begins with SCM’s Optionorship in 2012:

Table 1-1. Summary of known historical mineral exploration programs conducted in the Project area.

Period Company Description Comments

1970-1995 "Candelaria Mine" small-scale mining; mine

referred to as Candelaria Mine no information or data available

2004 Hochschild Mining

PLC

diamond drilling; 6 holes (80-

100 m long); area of open pit

no information or data available;

core location unknown (pers.

comm. Jose Frutos, 2021)

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Period Company Description Comments

2005-2006 Araya Hermanos de

Copiapó S.A.

small-scale mining of Cu

oxides; ~5,000 tpm

mineralized material sold to

ENAMI

2007-2011 Mantos Candelaria small-scale mining mining ended after 7 years due to

internal disagreements

2011

Sociedad de

Inversiones Gema

Limitada

acquired 3 main mining

concessions acquired Resguardo 1, 3 and 4

2012 Sociedad Contractual

Minera Resguardo

company formed to hold 3

main mining concessions

Resguardo 1, 3 and 4 and expand

the property to a total of 18

contiguous concessions

2012

Castillo Copper Chile

SpA/Kingsgate

Consolidated Ltd

optioned property; 2 diamond

drill holes (~200 m each) terminated option in 2014

2018 Orestone Mining

Corp.

optioned property; 2 RC drill

holes; geophysical survey terminated option in 2020

2014-2020 Sociedad Contractual

Minera Resguardo

geological mapping study;

geophysical survey along 2 N-S

profiles (P1 and P2)

financed by SCM

Figure 1. Resguardo Cu-Au Project location and Metallogenic belts of Northern Chile, Atacama & Antofagasta regions

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Photos taken from the NI 43-101 Technical R eport on the Resguardo Copper -Gold Property, that Alturas has in

preparation through its independent contractor Caracle Creek International Consulting Inc.

About Sociedad Contractual Minera Resguardo and Non Arm’s Length Party Disclosure

Sociedad Contractual Minera Resguardo (“Minera Resguardo”) was incorporated in 2012 to acquire additional

concessions in the Resguardo project area. It is controlled by Sociedad de Inversiones Gema Limitada (52%), with

partners Inversiones Mineras El Refugio S.A. (30%) and CP Group Chile Limitada (18%), both owned by Peruvian

investors. CP Group Chile Limitada is a Chilean subsidiary of the family -owned CP Group S.A.C. Peruvian company,

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which shareholders are Mr. Miguel Cardozo, CEO and Director of Alturas Minerals Corp. (the Issuer) and his wife

Mrs. Sara Pajares, owning 50% of this company each.

About Alturas Minerals

Alturas is a Canadian corporation, and is the indirect parent of the Peruvian c ompany, Alturas Minerals S.A.

(“Alturas Peru”) and of the Chilean company, Alturas Chile Limitada (“Alturas Chile”). Alturas had been exploring

various mineral projects in Peru between January 2004 and 2020 and between 2012 and 2014 in Chile through its

subsidiaries. After interrupting its exploration activities in Chile and Peru due to financial constraints, Alturas is now

focusing in new business opportunities, including the initiation of mining operations in Chile.

Qualified Person

Scott Jobin -Bevans (PhD, PMP, P.Geo.) , an independent qualified person (“QP”) as defined in National Instrument

43-101, has reviewed, and approved the technical contents of this news release on behalf of the Company. The QP

as part of his involvement as Principal Geo scientist with Caracle Creek International Consulting Inc. has visited the

Resguardo Copper Project and has completed sufficient work to verify the historic information on the Concessions,

particularly regarding historical exploration, neighboring companies, and government geological work.

ALTURAS MINERALS CORP.

“Miguel Cardozo” Chief Executive Officer

Contact: Mario Miranda

Phone: (416) 363-4900

Alturas Minerals Corp. (TSX-V: ALT)

372 Bay Street, Suite 301 Toronto, Ontario M5H 2W9

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Exchange) nor the Bolsa de Valores de Lima accepts responsibility for the adequacy o r accuracy of this release.