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IP Survey Confirms Porphyry Exploration Target at Pacific Ridge's Redton Copper-Gold Project

Exploration Programs Sampling & Geoscience Results

IP Survey Confirms Porphyry Exploration

Target at Pacific Ridge's Redton Copper-Gold

Project

Vancouver, British Columbia--(Newsfile Corp. - October 15, 2024) - Pacific Ridge Exploration Ltd.

(TSXV: PEX) (OTCQB: PEXZF) (FSE: PQWN) ("Pacific Ridge" or the "Company") is pleased to

announce that the induced polarization ("IP") geophysical survey recently completed at its 100% owned

Redton copper-gold project ("Redton or the "Project") confirmed a porphyry exploration target within 3

km of NorthWest Copper Corp.'s ("NorthWest") Kwanika South Zone copper-gold-molybdenum porphyry

deposit. Redton is located in the prolific Quesnel terrane in northcentral British Columbia and adjoins the

eastern boundary of NorthWest's Kwanika (see Figure 1).

Highlights:

Redton is over 34 km

2

and adjoins the eastern boundary of NorthWest's Kwanika, which hosts two

deposits, the Kwanika South Zone copper-gold-molybdenum porphyry deposit and the Kwanika

Central Zone copper-gold porphyry deposit.

The 2024 Redton IP survey comprised 7.5 line-kilometers in three reconnaissance lines to test

three target areas in the northern half of the Project. The survey was conducted in early September

(see Figure 2).

The Project features a 5-km-long north-northwest trend of porphyry copper-gold targets located

within the Hogem intrusive suite, 3.5 km northeast of the NNW trend of the Kwanika deposits.

The middle line of the IP survey tested the Northeast Kwanika South ("NEX") target where

topography, AeroTEM, and 3D model inversions suggest there is a northeast trending cross-

structure extending onto Redton from the Kwanika South Zone deposit.

The NEX target lies at the intersection of this interpreted cross-structure with an NNW-trending

lithological contact boundary

1

that has Late Triassic mafic (gabbro-diorite) rocks on the west and

Early Jurassic monzonitic rocks on the east. The Kwanika deposits (200 Ma

2

; Early Jurassic) lie

on the western side of the Late Triassic mafic domain. NEX lies on its eastern side.

"I'm very pleased that the IP survey confirmed the presence of a compelling porphyry exploration

target within 3-km of the Kwanika deposits,"

said Blaine Monaghan, President and CEO of Pacific

Ridge

. "The results of the IP survey, combined with structural interpretation, models of airborne

magnetics, soil geochemistry and favourable geology, have increased our confidence that we have

identified an exploration target that could result in a new porphyry discovery. We plan to follow up with

additional infill survey lines and a possible drill program."

IP Survey at Redton

The 2024 Redton IP survey comprised three east-west lines (2.5 line-km each totaling 7.5 line-km) at

800 m line-spacing. These lines tested three target areas in the northern half of the Project including a

portion of the historical East Swan target, the historical Redton East target, and the more recently

defined NEX target, which is similar in size and orientation as the Kwanika Central Zone. The program

objective was to identify any IP geophysical signatures of interest that can be followed up with infill survey

lines and an initial drill test. In addition to the IP survey, 3D MVI modelling of the 2010 AeroTEM survey

aeromagnetics was completed to identify any relationships with the 2D IP inversion results.

Figure 1:

Location of Redton and Pacific Ridge's Other Porphyry Copper-Gold Projects in

Northcentral B>C.

To view an enhanced version of this graphic, please visit:

https://images.newsfilecorp.com/files/5460/226637_7359205a24273921_001full.jpg

Figure 2:

Redton 2024 Induced Polarization Survey Plan and Target Conceptualization

To view an enhanced version of this graphic, please visit:

https://images.newsfilecorp.com/files/5460/226637_7359205a24273921_002full.jpg

2024 Redton IP Survey results

Results of the IP survey suggest that NEX is a porphyry target area, particularly in the hanging-wall of the

interpreted NEX Fault and the footwall of an interpreted Late Triassic/Early Jurassic lithological contact.

This prospective zone may continue northward into the southern part of Redton East (see Figure 2).

L6800

L6800 is the northernmost line of the IP survey and tested the Redton East target, an 800 x 700 m

copper-in-soil anomaly on the northeastern side of the Property that was delineated from surface

sampling programs in 1972 and by Kiska Metals Corporation in 2011-2012.

The IP line features a large resistivity high domain (>3000 ohm-m) in Hogem intrusive suite. Most of the

resistivity high is within interpreted Early Jurassic monzonitic rocks. The domain appears to dip

moderately to the west, suggesting the Hogem intrusive suite is moderately tilted to the east (see Figure

3 inset). There is a large chargeability anomaly starting at about 200 m depth, becoming higher intensity

(>12 mV/V) by 300 m depth. Overburden is estimated at up to 100 m depth of glacial till material which

may be dampening the chargeability signature.

Figure 3:

2024 IP Survey Inversion Results for L6000 Across the NEX Target With Fault

Interpretation. Inset Map is DC Resistivity for the L6800 Redton East Section

To view an enhanced version of this graphic, please visit:

https://images.newsfilecorp.com/files/5460/226637_7359205a24273921_003full.jpg

Figure 4:

Top: 3D MVI Model on Section 6155950 N with Chargeability High Domain from IP Line

L6000. Bottom: Schematic Interpretation of NEX Target Geology Based on Geophysical Inversions

To view an enhanced version of this graphic, please visit:

https://images.newsfilecorp.com/files/5460/226637_7359205a24273921_004full.jpg

L6000

L6000 is the central line of the IP survey and tested NEX, a 1000 x 500 m target area identified in 2022

with a similar size and orientation as the Kwanika Central Zone depsoit. It lies at the eastern end of an

interpreted NE-trending cross-structure in the AeroTEM geophysical data (AeroQuest and

TechnoImaging, 2010) where it intersects with an NNW-trending lithological contact of interest in the

Hogem intrusive suite. NEX has anomalous molybdenum-in-soil over the geophysical feature and

anomalous copper and silver to the southeast (see Figure 2).

The IP line features a break in the resistivity high domain (see Figure 3) that aligns with an extension of

the interpreted NE-trending cross-fault that continues to the western property boundary. This structure is

now referred to as the NEX fault (see Figure 2). Again, this inversion section has a large chargeability

high domain (>12 mV/V) that comes as close as 100 m to surface in the NEX target area (see Figure 3).

The NEX fault, as interpreted from the DC resistivity inversion, intersects the chargeability high at depth,

as well as a large coincident magnetic high anomaly (see Figure 4 top) and provides an important

structural marker for future drill hole planning (se Figure 3).

L5200

L5200 is the southernmost line of the IP survey and tested the southern end of NEX where there is

anomalous copper, bismuth and silver in surface geochemistry (see Figure 2).

The IP line features a narrower (~350 m wide) west-dipping resistivity high domain (>3000 ohm-m)

underlying Early Jurassic rocks of the Hogem intrusive suite, again suggesting moderately northeast

tilted geology. The southern end of NEX lies in the hanging-wall of this resistivity high domain. The

chargeability high anomaly on this inversion section starts at greater depth (>500 m) but comes to

surface in a 100 m wide steeply dipping pipe or lens shape feature that is 200 m from the modelled

trace of NEX Fault at the western end of the section (see Figure 2), again attesting to the importance of

this structure.

About Redton

Owned 100% by Pacific Ridge, Redton is over 34 km

2

in size and adjoins the eastern boundary of

NorthWest's Kwanika. Several target areas exist at Redton: Redton North, East Swan, Redton East,

NEX, NEX South, and Catchment Basin. In 2022, after completing a targeted soil survey grid in the

northcentral part of the Project, the Company identified a surface geochemical target, the NEX zone,

which is of similar size and orientation as the Kwanika Central Zone. NEX is located 3-4 km east of

Kwanika following an interpreted arc-transverse lineament and an AeroTEM geophysical feature of

interest.

Chuchi South and Chuchi West Option Amendment

In March 2023, Pacific Ridge entered into an agreement with American Copper Development

Corporation ("ACDX") and Ronald Bilquist ("Bilquist") granting Pacific Ridge the option to acquire a

51% interest in the Chuchi South Property by making $250,000 in payments to Bilquist and completing

$4,000,000 in exploration expenditures by December 31, 2027 (the "First Option"). The Company has a

further option to increase its interest to 75% by issuing shares valued at $250,000 to ACDX by January

30, 2028, by making cash payments of $150,000 to ACDX, and completing an additional $4,000,000 in

exploration by December 31, 2029 (the "Additional Interest Option").

In addition to Chuchi South, ACDX granted Pacific Ridge the sole and exclusive right and option to

acquire a 51% interest in the Chuchi West Property in consideration of Pacific Ridge satisfying the First

Option on Chuchi South. The Chuchi West Property would then be included in the Additional Interest

Option for a 75% interest in Chuchi South and Chuchi West.

Earlier this year, the parties reached an agreement for Pacific Ridge to issue 550,000 common shares

of the Company in lieu of a $50,000 cash payment to Bilquist that was due on February 13, 2024 under

the First Option. This amendment remains subject to TSX Venture Exchange approval.

The parties have now agreed to a further amendment which removes the obligation for Pacific Ridge to

issue shares to exercise the Additional Interest Option. In lieu of such share issuance, Pacific Ridge

must make a cash payment of $250,000 to ACDX by no later than January 30, 2028.

1

Cui, Y., Miller, D., Schiarizza, P., and Diakow, L.J., 2017. British Columbia digital geology. British Columbia Ministry of Energy, Mines and Petroleum

Resources, British Columbia Geological Survey Open File 2017-8, 9p. Data version 2019-12-19.

2

Age date for Kwanika deposit is from Logan, J.M., and Mihalynuk, M.G., 2014. Tectonic controls on Early Mesozoic paired alkaline porphyry deposit

belts (Cu-Au ± Ag-Pt-Pd-Mo) within the Canadian cordillera. Economic Geology, 109, p. 827- 858.

About Pacific Ridge

Our goal is to become B.C.'s leading copper-gold exploration company. Pacific Ridge's flagship asset

is its 100% owned Kliyul copper-gold project, located in the Quesnel terrane close to existing

infrastructure. In addition to Kliyul, the Company's project portfolio includes the Chuchi copper-gold

project, the 100% owned RDP copper-gold project, the 100% owned Onjo copper-gold project, and the

100% owned Redton copper-gold project, all located in British Columbia. The Company would like to

acknowledge that its B.C. projects are located in the traditional, ancestral and unceded territories of the

Gitxsan Nation, McLeod Lake Indian Band, Nak'azdli Whut'en, Takla Nation, and Tsay Keh Dene Nation.

On behalf of the Board of Directors,

"Blaine Monaghan"

Blaine Monaghan

President & CEO

Pacific Ridge Exploration Ltd.

Investor Relations:

Tel: (604) 687-4951

Email:

[email protected]

Website:

www.pacificridgeexploration.com

LinkedIn:

https://www.linkedin.com/company/pacific-ridge-exploration-ltd-pex-/

Twitter:

https://twitter.com/PacRidge_PEX

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

policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this

release.

The technical information contained within this News Release has been reviewed and approved by

Danette Schwab, P.Geo., Vice President Exploration, and a Qualified Person as defined by National

Instrument 43-101 policy.

Forward-Looking Information:

This release includes certain statements that may be deemed

"forward-looking statements". All statements in this release, other than statements of historical facts,

which address exploration drilling and other activities and events or developments that Pacific Ridge

Exploration Ltd. ("Pacific Ridge") expects to occur, are forward-looking statements. Forward looking

statements in this news release include additional infill survey lines and a possible drill program at

Redton. Although Pacific Ridge believes the expectations expressed in such forward-looking

statements are based on reasonable assumptions, such statements are not guarantees of future

performance and actual results or developments may differ materially from those forward-looking

statements. Factors that could cause actual results to differ materially from those in forward looking

statements include market prices, exploration successes, and continued availability of capital and

financing and general economic, market or business conditions. These statements are based on a

number of assumptions including, among other things, assumptions regarding general business and

economic conditions, that one of the options will be exercised, the ability of Pacific Ridge and other

parties to satisfy stock exchange and other regulatory requirements in a timely manner, the

availability of financing for Pacific Ridge's proposed programs on reasonable terms, and the ability of

third party service providers to deliver services in a timely manner. Investors are cautioned that any

such statements are not guarantees of future performance and actual results or developments may

differ materially from those projected in the forward-looking statements. Pacific Ridge does not

assume any obligation to update or revise its forward-looking statements, whether because of new

information, future events or otherwise, except as required by applicable law.

To view the source version of this press release, please visit

https://www.newsfilecorp.com/release/226637