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New Geophysical Results Solidify Targets for Upcoming Phase 1 Drilling Program at Fitzroy’s Polimet Gold-Copper-Silver Project, Chile

Exploration Programs

January 27, 2025

New Geophysical Results Solidify Targets for Upcoming Phase 1 Drilling Program

at Fitzroy’s Polimet Gold-Copper-Silver Project, Chile

VANCOUVER, BRITISH COLUMBIA, January 27, 2025 – FITZROY MINERALS INC. (TSXV: FTZ, OTCQB:

FTZFF) (“Fitzroy Minerals” or the "Company") is pleased to announce that new geophysical results, paired

with previously reported soil and rock results, and geologic mapping , have enhanced the understanding

of the epithermal mineral system at the Polimet Gold -Copper-Silver Project, Chile (“ Polimet” or the

“Project”).

An Induced Polarisation (“IP”) geophysical survey showed a very good relationship between conductive

zones and known historical workings, hydrothermal alteration, and elevated Au-Cu-Ag grades. In addition,

a detailed ground magnetic survey confirmed the presence of a structural corridor at least 5 km long by

1.6 km that incorporates known mineralized zones, mapped veins, geochemical anomalies, and historical

workings. This geophysical data has been integrated into the Phase 1 drilling program which will test the

best targets based on a combination of structural setting, gold and copper assay results, hydrothermal

alteration, and IP conductors. A 2,500 metre, minimum seven-hole diamond drill ing program is due to

start in February 2025.

Highlights:

• Newly identified 1,600 m-long conductor, connecting the historical workings of Santo Domingo and

La García that returned grades of 10.6 g/t Au and 6.5 % Cu (Santo Domingo) and 23.3 g/t Au and

3.4 % Cu (La Garcia) from channel samples in the adits.

• Newly identified 680 m -long conductor around the historical San Pedro workings that returned

grades of 43 g/t Au and 7.3 % Cu from channel samples in adits.

• A total geophysical conductor length of 4,700 m identified within the survey zone, with several

anomalies open toward the north.

Merlin Marr-Johnson, CEO and President comments, "There is no doubt that based on what we have seen

to date, the Polimet Project hosts a significant epithermal gold system that has the potential to contain a

high-grade gold-copper-silver deposit. We are very pleased with t he geophysical results which correlate

with previous mapping and sampling work. In particular , the four main vertical conductors have helped

confirm several high priority drill targets that we look forward to testing in the coming weeks. As soon as

the drilling at Caballos finishes we will move the rig and start the Phase 1 drill program at Polimet.”

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Polimet Gold-Copper-Silver Project, Chile

Induced Polarisation “IP” Survey

IP surveys were completed on 9 lines totalling 21.2 line-km. A pole-dipole array was used with a 50 m

dipole spacing expanded through 8 separations (n=1 to 8), which is an arrangement that gives good

penetration up to a depth of about 300 metres. The 9 lines were spaced 300 m apart, and covered an area

of about 540 ha, which is just under 25% of the total concession area. The IP survey was centered on the

best geochemical, geological, and structural zones identified to date. The survey outlined four main

conductors (Figure 1).

The survey data highlighted a relationship between conductive zones and zones of hydrothermal

alteration or geochemical anomalies of copper and/or gold.

Figure 1. IP Resistivity slice at 100 m depth showing four main conductors at Polimet

Typically the conductive zones appear as a strip at least 100 m wide in the footwall of the known

epithermal vein zones and they extend to the limit of the survey at a depth of about 300 metres. The

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survey also identified several horizontal conductors that are interpreted to relate to lithology and are

therefore a lower priority target.

The main vertical conductor trends exhibited sectors with very high conductivity (<250 Ohm -m)

transitioning to medium to low conductivity ranges (250 to 350 Ohm -m). Four main trends of vertical

conductors were identified.

The most extensive vertical conductor is #1 (1 in Figure 1) , in the central part of the structural corridor

and is 1,600 m long, trending NNE-SSW. It connects the Santo Domingo workings to the western part of

the La García workings and extends to a set of mapped veins in the northern part of the structural corridor.

Channel samples within the historic adits returned 10.6 g/t Au and 6.5 % Cu from Santo Domingo and 23.3

g/t Au and 3.4 % Cu from La Garcia (Fitzroy Minerals news release dated February 6, 2024). To the south

the conductor becomes weaker although it continues for an additional 600 m, forming a total anomaly of

2,100 m, and still open to the north.

Vertical Conductor 2 (2 in Figure 1) is a highly prospective anomaly as it coincides with the San Pedro vein

set, where the largest high-grade ore shoot found to date on the property has been exploited. Channel

samples within the historic adits returned 43 g/t Au and 7.3 % Cu (Fitzroy Minerals news release dated

February 6, 2024). This conductor is at least 680 m long and correlates with a mapped vein zone extending

from the San Pedro workings to the N-NW.

Figure 2. Resistivity Section 22350 (see also Figure 1) showing proposed drill hole, structure, vein, and

conductor

The third Vertical Conductor of interest is in the eastern part of the survey area (3 in Figure 1). Part of this

conductor trends NW-SE and correlates well with several veins and silicified zones mapped with

occurrences of Cu and Au. The conductor then appears to swing northwards and continue for another 700

m for a total of 1,400 metres. Finally, in the NW part of the survey coverage, a good vertical conductor

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has been identified which extends 600 m in a N-S direction (4 in Figure 1). This conductor is open to the

north and coincides with several small workings, adits and galleries developed by artisanal miners.

In total, these four vertical conductors comprise more than 4,700 m of strike length . S everal of the

conductors are open to the north. In addition to the conductivity anomalies, the IP survey also identified

chargeability anomalies . Broadly chargeable zones are evident on either side of the main conductive

trends. One interpretation of these anomalies infers a pyrite-rich halo around the mineralized veins.

Figure 3. Polimet Magnetic Survey, Structural Interpretation, and location of the IP survey

Target Generation and Phase 1 Drilling

Fitzroy Minerals has generated several drill targets that will be tested in the Phase 1 diamond drilling

program due to start in February 2025. Areas with strong vertical conductivity anomalies that correlate

well to known or inferred vein trends and/or geochemical anomalies were prioritized in drillhole

scheduling. The proposed drillhole shown in Figure 2 (Resistivity Section 22350) illustrates the compound

nature of the anomalies. The proposed drillhole crosses a known mineralized structure and a strong

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conductivity anomaly. At least seven drillholes are planned to test these targets, and there will be

additional scope to test horizontal conductivity anomalies.

Magnetometry Survey

Ground magnetic surveys were conducted along lines spaced 50 m apart and oriented east-west. A total

of 329 line-km of continuous data was acquired, covering approximately 70% of the total concession area

(Figure 3). The data highlights a structural corridor of 5.0 km x 1.6 km with a general NNW-SSE trend.

Qualified Person

Dr. Scott Jobin-Bevans (P.Geo., Ph.D.), a Qualified Person as defined by National Instrument 43 -101 and

independent geological consultant to the Company, has reviewed and verified the technical information

provided in this news release.

About Fitzroy Minerals

Fitzroy Minerals is focused on exploring and developing mineral assets with substantial upside potential

in the Americas. The Company’s current property portfolio includes the Caballos Copper and Polimet Gold-

Copper-Silver projects located in Valparaiso, Chile, and the Taquetren Gold project located in Rio Negro,

Argentina, as well as the Cariboo project in British Columbia, Canada. Fitzroy Minerals’ shares are listed

on the TSX Venture Exchange under the symbol FTZ and on the OTCQB under the symbol FTZFF.

On behalf of Fitzroy Minerals Inc.

Merlin Marr-Johnson

President and CEO

For further information, please contact:

Merlin Marr-Johnson

[email protected]

+1 604-505-4554

For more information on Fitzroy Minerals, please visit the Company's website: www.fitzroyminerals.com

This press release does not constitute an offer to sell or a solicitation of an offer to buy any of the securities

in the United States. The securities have not been and will not be registered under the United States

Securities Act of 1933, as amended, or any state securities laws and may not be offered or sold within the

United States or to or for the account or benefit of a U.S. person (as defined in Regulation S under the

United States Securities Act) unless registered under the U.S. Securities Act and applicable state securities

laws or an exemption from such registration is available.

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Exchange) accepts responsibility for the adequacy or accuracy of this release.

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