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Rackla Metals Closing in on a Reduced Intrusion-related Gold System (RIRGS) on the HIT Property, Yukon

Corporate Updates

Rackla Metals Closing in on a Reduced Intrusion-related Gold System (RIRGS) on

the HIT Property, Yukon

Vancouver, British Columbia – October 31, 2023 – Rackla Metals Inc. (TSX -V: RAK) (the “Company”) is

pleased to announce that the Company has intersected significant gold mineralization from its maiden

diamond drill program on its 100% owned HIT property in Yukon . The HIT property is located in the

Tombstone Gold Belt at the Yukon-NWT border and is accessible from the North Canol road.

The prope rty is centered around the Canol Trail Stock, a monzogranite intrusion belonging to the

Cretaceous-aged Tungsten Suite intrusions. Cretaceous intrusions in the Tombstone Gold Belt host

significant gold deposits such as the Fort Knox Mine in Alaska (12.1 Moz gold), the Eagle Mine in Yukon

(7.8 Moz gold) and the newly discovered Valley gold occurrence belonging to Snowline Gold Corp.

Rackla completed a comprehensive program at HIT in 2023, including stream sediment, soil, talus and rock

sampling, prospecting , geological mapping, and airborne geophysics to define drill targets. The 2023

program culminated with the drilling of 997 m in 5 holes on 4 separate targets. Theses were the first holes

ever drilled into the Canol Trail Intrusive stock. Below is a summary of significant drill intercepts:

Table 1: Hit Property – significant intercepts of the 2023 drill program.

Holes HIT-003 and HIT-004 were drilled from the same pad, in opposite d irections in the vicinity of the

Mehitabel Prospect, which was historically identified as a copper -gold skarn mineral occurrence in the

sedimentary rocks at the margin of the Canol Trail Stock. The work by Rackla has shown that there is much

more to the occurrence. Mapping and prospecting on surface identified an abundance of sheeted quartz-

sulphide veining in the intrus ion that has been mapped in exposed outcrop over an area that measures

2.2 km by 1.2 km (see September 26, 2023 press release) . Soil and talus sampling in the area of the

occurrence has defined a gold-bismuth-arsenic anomaly that measures 1.5 km by 1.0 km and is open to

the northwest and to the southeast.

Historic and current rock sampling has returned an abundance of samples with greater than 1.0 g/t gold

in the area of the Mehitabel occurrence and in the area of the soil and talus geochemical anomalies

(Figure 1).

From (m) To (m) Interval (m) Au (g/t) As (ppm) Bi (ppm) Te (ppm)

HIT-001 no significant intercepts

HIT-002 no significant intercepts

6.09 135.88 129.79 0.248 52 9 0.6

includes 45.44 61.94 16.50 0.668 28 18 1.7

and 104.86 118.36 13.50 0.607 15 15 1.4

and 134.38 135.88 1.5 2.560 13 97 8.7

131.50 176.96 45.46 0.516 284 12 1.0

includes 164.39 170.30 5.91 2.325 1628 25 1.4

HIT-005 no significant intercepts

HIT-003

HIT-004

Drill Hole

Suite 650 – 200 Burrard Street

Vancouver BC Canada V6C 3L6

www.racklametals.com

T 604.801.5432

F 604.662.8829

TF 1.888.627.9378

RAK:TSX.V

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Figure 1: Hit Property compilation map with 2023 drill hole locations.

The airborne geophysical survey returned the characteristic magnetic signature of Tombstone Gold Belt

RIRGS occurrences: a magnetic low overlying the centre of the intrusion, with magnetic high shoulders

around the margins of the intrusion where the sedimentary country rock has been metasomatized and

the hornfelsed aureole is enriched in the magnetic mineral pyrrhotite.

Rackla is encouraged by the density of sheeted quartz-sulphide veins observed on surface and in the drill

core in holes HIT-003 and HIT-004, which is as high as 55 veins per metre. The veins have variable, but in

some instances wide sericite-carbonate alteration halos. These holes were drilled across the strike of the

veins, with veins striking 135 o and dipping steeply to the west. The cross section in Figure 2 below

illustrates that sheeted quartz-sulphide veins occur throughout both holes and across a total width of 273

m with both holes ending in the vein system. An example of the sheeted veins in drill core from hole HIT-

004 is shown in Figure 3 below and photographs with gold assays indicated on the core for holes HIT-003

and HIT-004 can be viewed at https://racklametals.com/projects/tombstone-gold-belt-properties/#core-

photos .

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Figure 2: Cross Section of drill holes HIT-003 and HIT-004 showing vein density and gold-bearing intervals.

Figure 3: Drill core from hole HIT-004 showing sheeted quartz veins with sericite-carbonate alteration halos around the veins.

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The analytical results of the drill core and surface samples shows a geochemical correlation of gold with

bismuth, tellurium +/-arsenic, which is a further indication of the mineralization at HIT being related to a

Reduced Intrusion-related Gold System.

The Company has completed one field season of work at HIT . Rackla is very excited with these results,

particularly considering how rapidly the target has advanced. The results from the 2023 program will be

used to vector towards the heart of the RIRGS target at HIT. Over the next few months, the Company will

complete a thorough review of the data collected and formulate plans for follow-up drilling in 2024. Rackla

is well funded and has sufficient cash for the commencement of the 2024 drill campaign.

Simon Ridgway, Rackla Metals CEO, commented: “Broad and dense sheeted quartz veining is a

characteristic of the plumbing system for prolific deposits in the Tombstone Gold Belt . Our team is

encouraged by both the vein density and geochemistry intercepted in holes HIT-003 and HIT-004. We are

certainly in or proximal to the carapace of a reduced intrusive that is host to significant sheet ed veining,

much of which is gold bearing. Management is of the opinion there is real potential for an economic RIRGS

deposit to be present within the Canol Trail stock. A significant drill program is planned for the project in

the 2024 season.”

Analytical Procedure

Drilling was generally performed with NQ2-sized equipment. Occasionally drill holes were collared with

HQ2-sized equipment if ground conditions were difficult. Drill core was systematically logged for geological

attributes, photographed and sample intervals identified by a geologist at Rackla’s field camp. Sample s

were generally sampled at 1.5 m intervals, but occasionally shorter intervals were sampled to isolate

features of interest. Samples were collected by cutting the c ore in half along the axis of the core. Field

duplicates were collected at regular intervals by cutting the half core to be sent to the lab into two ¼ core

samples, each with unique sample numbers leaving a consistent record of half core material in the core

box. Standard reference materials were inserted by Rackla personnel at regular intervals into the sample

stream. Samples were delivered by expeditor to ALS Global preparatory facility in Whitehorse, Yukon.

Sample preparation was completed in Whitehorse, with analyses completed in North Vancouver, BC. ALS

Global is an accredited ISO/IEC 17025 and ISO9001 laboratory for quality management.

At the lab, drill core s amples were crushed by ALS to >75% passing below 2 mm and split using a riffle

splitter. 250 g splits were pulverized to >85% passing below 75 microns. 0.5 g of the s ample pulps were

digested with a qua regia and analyzed by an inductively coupled plasma mass spectroscopy and

inductively coupled plasma atomic absorption spectroscopy (ICP-MS+ICP-AES) finish for 5 1-element

analysis (ALS code: ME-MS41). All samples were analysed for gold content by fire assay with a gravimetric

finish on 50 g samples (ALS code: Au-GRA22).

For the purposes of this release, mineralized intervals are defined as runs of mineralization >0.1 g/t Au.

Qualified Person

Scott Casselman, B.Sc., P.Geo., Vice-President Exploration of the Company, is a member of the Association

of Professional Engineers and Geoscientists of British Columbia and is the Company’s Qualified Person as

defined by National Instrument 43 -101. Mr. Casselman has reviewed and approved the technical

information contained in this news release.

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About Rackla

Rackla Metals Inc. (TSX -V: RAK) is a Vancouver, Canada based junior gold exploration company. The

Company is targeting Reduced Intrusion-Related Gold Systems (RIRGS) mineralization on the southeastern

part of the Tombstone Gold B elt in eastern Yukon and we stern Northwest Territories. Management

believes that this area, which is underexplored for R IRGS deposit types, has the potential to be the next

frontier for their discovery.

ON BEHALF OF THE BOARD

Simon Ridgway,

CEO and Director

Tel: (604) 801-5432; Fax: (604) 662-8829

Email: [email protected]

Website: www.racklametals.com

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

TSX Venture Exchange) accept responsibility for the adequacy or accuracy of this press release.

Forward-Looking Information

Certain statements contained in this news release constitute forward -looking statements within the meaning of

Canadian securities legislation. All statements included herein, other than statements of historical fact, are forward-

looking statements and include, without limitation, statements about the Company’s proposed exploration

activities. Often, but not always, these forward looking statements can be identified by the use of words such as

“estimate”, “estimates”, “estimated”, “potential”, “open”, “future”, “assumed”, “projected”, “used”, “detailed”,

“has been”, “gain”, “upgraded”, “offset”, “limited”, “contained”, “reflecting”, “containing”, “remaining”, “to be”,

“periodically”, or statements that events, “could” or “should” occur or be achieved and similar expressions, including

negative variations.

Forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause the

actual results , performance or achievements of the Company to be materially different from any results,

performance or achievements expressed or implied by forward -looking statements. Such uncertainties and factors

include, among others, changes in general economic cond itions and financial markets; the Company or any joint

venture partner not having the financial ability to meet its exploration and development goals; risks associated with

the results of exploration and development activities, estimation of mineral resour ces and the geology, grade and

continuity of mineral deposits; unanticipated costs and expenses; and such other risks detailed from time to time in

the Company’s quarterly and annual filings with securities regulators and available under the Company’s prof ile on

SEDAR at www.sedar.com. Although the Company has attempted to identify important factors that could cause

actual actions, events or results to differ materially from those described in forward -looking statements, there may

be other factors that cause actions, events or results to differ from those anticipated, estimated or intended.

Forward-looking statements contained herein are based on the assumptions, beliefs, expectations and opinions of

management, including but not limited to: that the Company ’s stated goals and planned exploration activities at its

properties will be achieved; that there will be no material adverse change affecting the Company or its properties;

and such other assumptions as set out herein. Forward -looking statements are made as of the date hereof and the

Company disclaims any obligation to update any forward -looking statements, whether as a result of new

information, future events or results or otherwise, except as required by law. There can be no assurance that

forward-looking statements will prove to be accurate, as actual results and future events could differ materially from

those anticipated in such statements. Accordingly, investors should not place undue reliance on forward -looking

statements.