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Fitzroy Minerals Reports Multiple Step-Out Copper Intercepts at Buen Retiro, Chile

Drill Results

August 19, 2025

Fitzroy Minerals Reports Multiple Step-Out Copper Intercepts at Buen Retiro, Chile

Vancouver, British Columbia – August 19, 2025 – Fitzroy Minerals Inc. (TSXV: FTZ, OTCQB: FTZFF)

(“Fitzroy” or the “Company”) is pleased to provide an exploration update from its ongoing 8,000

metre (“m”) Phase 2 drilling program at the Buen Retiro Copper Project, Copiapó, Chile (“ Buen

Retiro” or the “Project”).

Today’s release reports assay results from diamond drill holes 21 1, and 23 to 27 which are all

located in the Southwest Area of the Project. Copper mineralization was intersected in all drill

holes and the extent of mineralization along strike has been increased to 985 m. In addition,

definition of continuity has improved and the average distance between holes along strike has

been reduced to approximately 100 metres. Furthermore, as the trends of the Southwest and

South Areas converge, wider zones of mineralization have been identified. Between holes 21 and

24, several zones of shallow mineralization are present over 360 m of lateral extent. Oxide and

mixed minerals in the Southwest Area are typically seen down to vertical depths of approximately

150 metres along the main trend.

Assays are pending for holes 28 to 33, and will be reported soon. Holes 29 and 31 are testing a

further 300 m of strike length in the Southwest Area. Reverse Circulation (“ RC”) drilling in the

North Area at Buen Retiro is anticipated to start soon. The RC program will target hanging-wall

copper mineralization on a multi-kilometre geophysical anomaly that is interpreted to be shear

zone related and oxidised down to a depth of approximately 90 metres. Previously reported

intersections in this area include 59 m @ 0.39% from surface, in hole 16.

Highlights:

 Hole 27 intersected several mineralized zones from top of bedrock (at 49 m downhole) to a

downhole depth of 314 m, including 119 m @ 0.53% Cu in oxides from 49 metres, and 23 m

@ 0.5% Cu in wall-rock sulphides from 245 m.

 Holes 10, 21, and 24, show several discrete mineralized intersections in a 360 metre-wide

zone.

 Hole 25 returned 32 m @ 0.90% Cu from 2 m, including 11 m @ 2.28 % Cu from 11 m,

confirming oxide and secondary sulphide mineralization at the northwestern extremity of the

Southwest Area.

 Strike extent in the Southwest Area is at least 985 metres, and open along strike.

1 All holes in this report are diamond holes at the Buen Retiro Copper Project, identified by a common

prefix “BRT-DDH” followed by a number. For reader ease these have been reduced to the final two digits

in the text of the report.

Merlin Marr-Johnson, CEO of Fitzroy, commented: “Drilling at Buen Retiro continues to

demonstrate good copper grades and thicknesses below the gravels in the Southwest Area, which

is great news. Our drilling takes the proven strike length of the system to almost 1 km long, and

the wide and shallow mineralization we are finding will increase the dimensions of any potential

future pit.

More holes are pending from the Southwest Area, and our focus is on stepping out to drill shallow

material that we think will leach well. Our ongoing exploration of this major copper system will

expand to include shallow reverse circulation drilling in the North Area and at regional targets,

and diamond drilling to further test the sulphide potential at depth.

These continued good results in shallow oxide and mixed material in the Southwest Area

encourage us to accelerate ongoing resource delineation and technical de-risking work. Fitzroy

aims to advance towards production at Buen Retiro as quickly as possible, while continuing

exploration within the wider Project area. Any development is likely to have capital efficiencies

thanks to a mineral suite that is commonly treated in heap leach operations in Chile, as well as

benefiting from existing infrastructure advantages. The infrastructure at Buen Retiro is excellent

as it is close to the Pan-American highway, high voltage transmission lines, the mining centre of

Copiapó, and it is a brownfield site without any residents.”

Geological Interpretation and Expansion Potential

Today’s release reports assay results from diamond drill holes 23 to 27, as well as new results

from the lower part of drill hole 21 that were pending at the time of the June 6, 2025 news release.

Copper mineralization was intersected in all drill holes and the boundaries of known

mineralization have been expanded. Diamond drilling is ongoing in the Southwest Area, and RC

drilling in the North Area at Buen Retiro and Sierra Fritis is anticipated to start soon.

Extensions to known mineralization in the Southwest Area were identified to the southeast by

drill hole 27 and to the northwest by hole 26. In addition, a zone of shallow mineralization

extending over 360 m across strike was identified where the Southwest Area converged with the

South Area across 21, 24, and hole 10 (drilled in Phase 1). Drill holes 28 to 33 have been completed

and assays are pending.

Copper mineralization was intersected in all holes (23 to 27 and results from the lower part of

hole 21) and the boundaries of known mineralization have been expanded. Mineralization is

dominated by tenorite as fracture infill, veinlets and clusters, as well as chrysocolla and

occasionally cuprite, chalcocite, and minor native copper.

Diamond drilling is ongoing in the Southwest Area, and RC drilling in the Northern Area at Buen

Retiro is anticipated to start soon.

Drilling at Buen Retiro (23, 25, 26, and 27) were angled holes, drilled towards the northeast to

test the strike potential of the Southwest Area. Hole 24 was set-back to the southwest to test the

western limits of the system given that several holes along the main trend had started in

mineralization underneath gravel cover. Drill hole 21 was extended from the South Area over to

the Southwest Area at depth (see Figure 1).

Figure 1. Buen Retiro, Southwest and South Areas – drill holes and total field magnetic map

BRT-DDH027

Drill hole 27 was a 110 m step-out to the southeast of hole 10 and was located on the fringe of a

coincident IP and magnetic anomaly, returning 119 m at 0.53% Cu from 49 metres. Younger

gravels increase in thickness to the southeast, and drill hole 27 was mineralized directly from

bedrock at a downhole depth of 49 m, starting with a grade of 0.57% Cu. The host rock is a highly

altered and brecciated andesite with strong albite alteration. The white coloration of albite

alteration is a recognised feature of IOCG mineralisation in the wider Candelaria-Punta-del-Cobre

District. In places hematite and magnetite breccias dominate, sometimes forming massive veins.

Mineralization in hole 27 is very consistent to a downhole depth of 168 m. At a downhole depth

of 110 m, a zone with abundant tenorite and several veins of native copper returned 26 m @

0.91% Cu. Beyond 180 m, the andesites were markedly less albitized although still punctuated by

breccias and occasional massive hematite or magnetite veins. The angled hole crossed the main

sub-vertical target and into surrounding wall-rock. Interestingly, as the hole progressed through

wall-rock, disseminated chalcopyrite was occasionally evident, returning mineralized zones of 52

m @ 0.20% Cu from 175 m; 23 m @ 0.50% Cu from 247 m; and 15 m @ 0.22% from 299 metres

(see Figure 2).

Mineralization in drill hole 27 confirms the good widths of oxide and transition copper minerals

to a vertical depth of about 150 metres. The identification of mineralization on the fringes of the

main geophysical anomalies (see Figure 1) and in surrounding wall-rock is a positive development

as it increases the prospectivity of the Buen Retiro concessions. The intersection of sulphide

mineralization to a downhole depth of more than 300 m highlights the scale-potential of the Buen

Retiro IOCG system.

Figure 2. Cross-section of BRT-DDH027

BRT-DDH023, BRT-DDH025, and BRT-DDH026

Drill holes 23, 25, and 26 were drilled in the northwest end of the Southwest Area (see Figure 1).

Hole 25 intersected 32 m @ 0.90% Cu from 2 m, including 11 m @ 2.28% Cu from 11 m, and

various less-significant copper mineralized zones, including 24 m @ 0.14% Cu from 72 metres.

Hole 26 intersected 27 m @ 0.35% from 10 m, followed by sporadic isolated copper mineralized

sections. Hole 23 was the least mineralized hole in the Southwest Area to date, returning 6 m @

0.30% Cu from 191 metres.

BRT-DDH021 and BRT-DDH024

In the Company’s news release from June 6, 2025, partial results were published from hole 21.

Subsequent to that date, the drill hole was re-entered, and continued to a downhole depth of 340

metres. The prior published intersection was 35 m @ 0.30 % Cu from 115 metres. Fitzroy now

reports an intersection of 77 m @ 0.33% Cu from 115 m, including 11 m @ 0.86% Cu from 180

metres. Hole 24, collared to the west of the main trend, intersected two zones of copper

mineralization: 20 m @ 0.24% Cu from 23 m, and 43 m @ 0.22% Cu from 65 metres.

Figure 3. Cross-section of Diamond holes BRT-DDH024, BRT-DDH010, and BRT-DDH021

Holes 21 and 24 flank hole 10 which was drilled in 2024. Hole 10 returned 124 m @ 0.32% Cu from

the start of bedrock at 22.5 m, including 57.5 m @ 0.51% Cu from 32 m. Altogether, the three

holes are almost all on the same section line and demonstrate over 360 m of mineralization in a

broadly east-northeast to west-southwest direction across the main strike direction of the

Southwest Area (see Figures 1 and 3 for plan view and cross-section, respectively).

The geology of the Southwest Area is highly dynamic, with a significant amount of high-energy

brecciation evident in the rocks. Within these mega-breccias, there is also a large amount of

faulting of various ages. Fitzroy is still building a picture of the tectonic evolution of the Southwest

Area, and it is possible that the wider zone of surface mineralization may represent structural

repetition. Notwithstanding its origins, it is encouraging to see such a wide and shallow zone of

copper mineralization.

Next Steps

Diamond drilling continues at Buen Retiro with an emphasis on testing extensions and limits to

known mineralization in the Southwest Area. Assays for holes 28 to 33 are pending and results

will be released shortly.

In separate developments, the Company is in the final stages of contract negotiations on a RC

drilling program of at least 5,000 metres. As soon as the rig is mobilized, it will be deployed into

the Sierra Fritis targets, followed by work in the North Area, targeting shallow hanging-wall copper

oxide mineralization on a multi-kilometre geophysical anomaly that is interpreted to be shear

zone related.

Table 1. Selected Phase 2 drill core assay results from BRT-DDH021 and BRT-DDH023 to BRT-DDH027,

Buen Retiro Copper Project, Copiapó, Chile*

Drill Hole East (m)

(WGS84)

North (m)

(WGS84)

**Azimuth /

Dip

From

(m)

To

(m) ***Interval (m) Cu (%)

BRT-DDH021 345321 6920903 267/-45 114 191 77 0.33

including 180 191 11 0.86

BRT-DDH023 344712 6921381 075/-45 191 197 6 0.30

BRT-DDH024 344907 6920835 080/-48 23 43 20 0.24

and 65 108 43 0.22

BRT-DDH025 344695 6921497 081/-45 2 34 32 0.90

including 11 22 11 2.28

and 72 96 24 0.14

BRT-DDH026 344656 6921645 081/-45 10 37 27 0.36

BRT-DDH027 345049 6920739 077/-45 49 168 119 0.53

including 110 136 26 0.91

and 175 227 52 0.20

and 247 270 23 0.50

and 299 314 15 0.22

*Minimum thickness of 5 m and minimum average grade of 0.15% Cu.

**measured at the collar

***True width estimated to be 70% of drill hole interval.

Sampling Procedures, Laboratory and QA/QC

Drill core in labelled and secured wooden core trays is picked up by Company personnel and

transported by truck from the drill rig to the core processing facility in Copiapó. Core depths are

checked, after which geotechnical logging is performed.

Using a core cutting diamond blade saw, primary half core samples are collected from HQ or NQ-

sized drill core with the remaining half-core stored in the original wooden core trays at the rented

core storage warehouse in Cuesta Cardones, south of Copiapó. Silica blank are inserted every 20

samples (~20 m); a blank is always inserted immediately after a section that contains native

copper. Pulp duplicates are randomly selected in proportion to the number of samples from each

drill hole and inserted into the sample stream along with high-, medium-, and low-grade copper

standards. Sample identifications are changed and coded by the Company. The QA/QC samples

prepared by the Company represent about 12% of the total primary core samples.

The three copper standards (both oxide and sulphide), acquired from Chilean company Instituto

Nacional de Technologia Estandarizacion y Metrologia Ltda. (“ INTEM”) all have international

standard certification. The certified standards are used to evaluate the accuracy (approximation

versus true value) of the laboratory analysis. Blanks are used to evaluate the quality of the

laboratory preparation and identify possible contamination. Pulp duplicates are used to test

analytical accuracy (repeatability). No secondary laboratory (referee lab) samples were

completed in this round of drilling; however, the next stage and subsequent stages of drilling will

put in place laboratory replicate procedures.

Once prepared, the core samples are bagged, tagged, and transported to the laboratory by the

project team. At the laboratory reception, the samples and their identification codes are verified

and accepted once the physical inventory matches the assay request form.

The pulps and rejects of crushed samples are collected from the ALS-Patagonia laboratory in

Copiapó every 3 months. The rejects are stocked in closed drums, identified with the

corresponding batches and sample ranges, while the pulps are stocked in boxes and in shelves

inside a container separated for this purpose. Both are located in the same warehouse facilities.

A visual review of the QA/QC results from the standards and blanks inserted by the Company and

the laboratory’s internal QA/QC information was completed by the Company and no significant

issues were identified.

Qualified Person

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

43-101 and independent geological consultant to the Company, has reviewed and approved the

technical information provided in this news release, including the sampling, analytical and test

data underlying the technical information contained in this news release. Specifically, the QP

verified laboratory assay certificates against the reported drill core intervals as well as drill core

logs against the geology, as supplied by the Company.

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 Buen Retiro

Copper Project located near Copiapó, Chile, the Caballos Copper and Polimet Gold-Copper-Silver

projects located in Valparaiso, Chile, the Taquetren Gold Project located in Rio Negro, Argentina,

and 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]

+447803712280

For more information on Fitzroy Minerals, please visit the Company's website:

www.fitzroyminerals.com

Neither Exchange nor its Regulation Services Provider (as that term is defined in the policies of

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

CAUTIONARY STATEMENT REGARDING FORWARD-LOOKING INFORMATION

This news release includes certain statements and information that constitute forward-looking

information within the meaning of applicable Canadian securities laws. All statements in this news

release, other than statements of historical facts are forward-looking statements. Such forward-

looking statements and forward-looking information specifically include, but are not limited to,

statements that relate to the potential mineralization on the Company’s mineral properties, future

exploration plans on the Company’s mineral properties and the timing and results of future

exploration.

Statements contained in this release that are not historical facts are forward-looking statements

that involve various risks and uncertainty affecting the business of the Company. Such statements

can generally, but not always, be identified by words such as "expects", "plans", "anticipates",

"intends", "estimates", "forecasts", "schedules", "prepares", "potential" and similar expressions,

or that events or conditions "will", "would", "may", "could" or "should" occur. All statements that

describe the Company's plans relating to operations and potential strategic opportunities are

forward-looking statements under applicable securities laws. These statements address future

events and conditions and are reliant on assumptions made by the Company's management, and

so involve inherent risks and uncertainties, as disclosed in the Company's periodic filings with

Canadian securities regulators, including without limitation, the dangers inherent in exploration,

development and mining activities; actual exploration or development plans and costs differing

materially from the Company’s estimates; the ability to obtain and maintain any necessary

permits, consents or authorizations required for mining activities; environmental regulations or