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Palladium One Discovers New High-Grade Nickel - Copper Zone 3.5 kms from the Smoke Lake Zone, Tyko Nickel - Copper Project, Canada

Drill Results

Palladium One Discovers New High-Grade

Nickel - Copper Zone 3.5 kms from the Smoke

Lake Zone, Tyko Nickel - Copper Project,

Canada

Highlights

New High-Grade discovery ("Ember Zone") located 3.5 kilometers southwest of the

Smoke Lake Zone

Multiple near surface drill intercepts of high-grade nickel - copper mineralization

Including:

6.9 meters grading 1.1% Ni, 0.3% Cu

(Hole TK22-104)

Including

1.9 meters grading 2.0% Ni, 0.4% Cu

5.3 meters grading 0.7% Ni, 0.8% Cu

(Hole TK22-100)

Including

1.5 meters grading 2.0% Ni, 2.8% Cu

Ember Zone is located adjacent to a greater than six (6) kilometer long interpreted

Chonolith / Feeder Dyke that is on strike with the Cupa Lake Versatile Time Domain

Electromagnetic airborne ("VTEM") anomaly.

Cupa Lake also hosts coincident strong nickel and copper soil anomalies.

Chonolith / Feeder Dyke geological model continues to be confirmed.

Toronto, Ontario--(Newsfile Corp. - March 27, 2023) -

Palladium One Mining Inc.

(

TSXV: PDM

)

(

OTCQB: NKORF

) (

FSE: 7N11

) (the "

Company

" or "

Palladium One

") is pleased to report the

discovery of a new high-grade nickel - copper zone ("

Ember Zone

")

which is located 3.5 kilometers

southwest of the Smoke Lake Zone (Figure 1) on the Tyko nickel - copper project, in Ontario, Canada

("

Tyko Project

").

"The discovery of another high-grade nickel - copper zone at Tyko further supports our thesis that we

have a significant new nickel camp on our hands. The Ember Zone exhibits many similarities to the

nearby Smoke Lake Zone and other high-grade nickel - copper zones on the Tyko Project. Notably the

Ember Zone is adjacent to an extensive interpreted Chonolith, which is on strike with the Cupa Lake

VTEM / soil anomalies, suggesting Ember may be part of much larger mineralizing system," commented

Derrick Weyrauch, President and Chief Executive Officer.

The Ember Zone was first identified by a moderate two line VTEM anomaly in 2021 (see the Company's

news release dated

October 28, 2021

), reconnaissance soil sampling returned weakly anomalous nickel

values up to 42 parts per million ("

ppm

"), and copper values up to 30 ppm (Figure 2). The weak

geophysical and soil anomalies of the Ember Zone resulted in it being drill tested during Q4 2022, Its

discovery reinforces the notion that any VTEM anomaly and even weak soil anomalies can point to high-

grade nickel - copper mineralization on the Tyko Project.

Notably the Ember Zone is located just north of an interpreted lengthy east-west trending Chonolith /

Feeder Dyke structure which is on strike with the Cupa Lake VTEM / soil anomaly (Figure 2). Cupa Lake

represents a multi-line VTEM anomaly and a strong soil anomaly with values up to 132 ppm nickel and

512 ppm copper. Cupa Lake is a priority drill target which has an outstanding Exploration Permit

application.

The geometry of the Ember Zone is not fully delineated, drilling to date was focused on defining the zone

at shallow depths as the conductor's orientation was poorly defined by the airborne VTEM survey. Thus

far, the zone appears to form a southwest plunging body toward the interpreted Chonolith / Feeder Dyke

structure located to the South (Figure 3). Hole TK22-108 was drilled as a Bore Hole ElectroMagnetic

("

BHEM

") geophysical platform but deviated from the interpreted plunge of the zone. A BHEM survey is

planned in Q2 2023 to better define the VTEM conductor and search for potential conductors at depth.

The 2022 drill program consisted of 70 holes totaling 13,038 meters, of which 14 holes are pending

assay results.

The 2023 field season is currently underway, with a high-resolution magnetic survey having

been completed.

The survey was designed to refine the geometry of the interpreted feeder dykes /

chonoliths across the Tyko Project's 30-kilometer strike length prior to additional drill testing. The 2023

exploration program will continue to focus on these newly identified and interpreted Chonolith / Feeder

Dyke structures on the 30,000-hectare Tyko Project (Figure 1).

Figure 1.

Tyko Property map showing various mineralized zones and multi-line VTEM anomalies,

background is Calculated Vertical Gradient Magnetics ("

CVG

").

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

https://images.newsfilecorp.com/files/6502/159861_9c58986a9486b8ed_001full.jpg

Figure 2.

Ember Zone and Cupa Lake target showing drill holes, soil samples and recently staked

claims (see the Company's new release dated

January 26, 2023

) which cover the eastern extension of

the interpreted Chonolith / Feeder Dyke Structure.

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

https://images.newsfilecorp.com/files/6502/159861_9c58986a9486b8ed_002full.jpg

Figure 3.

Semi-massive to net-textured sulphide consisting of pentlandite, chalcopyrite, and pyrrhotite

hosted by pyroxenite in the Ember Zone (Hole TK22-100).

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

https://images.newsfilecorp.com/files/6502/159861_9c58986a9486b8ed_003full.jpg

Figure 4.

Ember Zone plan map and stylized cross section, with select significant intercepts looking

northwest.

Hole TK22-108 was drilled as a geophysical platform hole for a future BHEM survey. Hole

TK22-107 was drilled to test the interpreted Chonolith structure but failed to intersect any ultramafic

rocks or explain the strong magnetic anomaly, the Chonolith structure remains to be tested.

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

https://images.newsfilecorp.com/files/6502/159861_9c58986a9486b8ed_004afull.jpg

Figure 4.

Continued

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

https://images.newsfilecorp.com/files/6502/159861_9c58986a9486b8ed_004bfull.jpg

Table 1: Assay Results: Tyko 2022 Drill Results from New Ember Zone

Hole

From

(m)

To

(m)

Width

(m)

Ni

%

Cu

%

Co

%

TPM

g/t

Pd

g/t

Pt

g/t

Au

g/t

TK22-096

No significant values

TK22-097

54.9

56.3

1.4

0.52

0.26

0.01

0.06

0.02

0.04

0.00

TK22-098

No significant values

TK22-099

Abandoned due to hole deviation

TK22-100

51.3

56.6

5.3

0.71

0.85

0.02

0.09

0.03

0.05

0.00

53.3

54.8

1.5

2.01

2.85

0.04

0.26

0.11

0.14

0.01

TK22-101

No significant values

TK22-102

54.4

60.4

6.0

0.28

0.15

0.01

0.05

0.01

0.02

0.02

54.4

57.4

3.0

0.38

0.23

0.01

0.08

0.02

0.03

0.04

TK22-103

43.8

47.6

3.9

0.45

0.26

0.01

0.04

0.02

0.02

0.00

43.8

45.8

2.1

0.74

0.45

0.02

0.08

0.03

0.04

0.00

TK22-104

32.0

38.9

6.9

1.07

0.28

0.02

0.07

0.03

0.04

0.00

35.7

37.5

1.9

2.02

0.36

0.04

0.11

0.05

0.06

0.00

TK22-105

No significant values

TK22-106

12.2

20.4

8.2

0.24

0.14

0.01

0.02

0.01

0.01

0.00

14.2

19.3

5.1

0.30

0.17

0.01

0.02

0.01

0.01

0.00

TK22-107

No significant values

TK22-108

No significant values, drilled as a BHEM geophysical platform

Hole

From

(m)

To

(m)

Width

(m)

Ni

%

Cu

%

Co

%

TPM

g/t

Pd

g/t

Pt

g/t

Au

g/t

(1)

Reported widths are "drilled widths" not true widths.

Table 2: Drill Hole Locations for assay results from this News Release

Hole

Azimuth

Dip

Length

NAD83 z16 East

NAD83 z16 North

Elevation

TK22-096

160

-75

225

625080.7

5419729

376

TK22-097

30

-55

150

625102.4

5419695

372.4

TK22-098

30

-70

126

625093.5

5419670

371.9

TK22-099

35

-45

22

625089.8

5419670

376.8

TK22-100

35

-45

75

625093.5

5419670

371.9

TK22-101

65

-45

84

625090.4

5419660

373.8

TK22-102

0

-45

111

625091.1

5419667

372.9

TK22-103

20

-45

96

625088.4

5419680

372.8

TK22-104

48

-50

63

625090.6

5419674

372.9

TK22-105

350

-70

99

625089.2

5419672

372.7

TK22-106

45

-45

51

625125.9

5419706

373

TK22-107

330

-75

195

625218.8

5419494

370.7

TK22-108

350

-70

300

625024.1

5419609

373.8

QA/QC

The drilling program was carried out under the supervision of Neil Pettigrew, M.Sc., P. Geo., Vice

President of Exploration, and a Director of the Company.

Drill core samples were split using a rock saw by Company staff, with half retained in the core box and

stored onsite at the Tyko exploration camp core yard facility.

Samples were transported in secure bags directly from the logging facility at the onsite exploration

camp, to the Activation Laboratories Ltd. ("

Actlabs

") in Thunder Bay, Ontario. Actlabs, which is ISO

17025 accredited with CAN-P-1579 (Mineral Lab). In addition to ISO 17025 accreditation, Actlabs is

accredited/certified to ISO 9001:2015. All samples are crushed to 2 millimeters with a 250-gram split

pulverized to 105 microns. Analysis for PGEs is performed using a 30 grams fire assay with an ICP-

OES finish and for Ni, Cu, and Co using 0.25 grams by 4 acid digestion with ICP-OES finish. Ni, Cu and

Co samples over 1.0 wt% were re-analysed by ore grade methods using 4 acid digestion with ICP-OES

finish.

Certified standards, blanks and crushed duplicates are placed in the sample stream at a rate of one

QA/QC sample per 10 core samples. Results are analyzed for acceptance within the defined limits of the

standard used before being released to the public.

About Tyko Nickel - Copper - Cobalt Project

The Tyko Nickel - Copper - Cobalt Project, is located approximately 65 kilometers northeast of Marathon

Ontario, Canada. Tyko is a high sulphide tenor, nickel - copper (2:1 ratio) project and currently has six

known mineralized zones spanning over a 20 kilometer strike length.

Qualified Person

The technical information in this release has been reviewed and verified by Neil Pettigrew, M.Sc., P.

Geo., Vice President of Exploration and a director of the Company and the Qualified Person as defined

by National Instrument 43-101.

About Palladium One

Palladium One Mining Inc. (TSXV: PDM) is focused on discovering environmentally and socially

conscious metals for green transportation. A Canadian mineral exploration and development company,

Palladium One is targeting district scale, platinum-group-element (PGE)-copper-nickel deposits in

Canada and Finland. The Läntinen Koillismaa (LK) Project in north-central Finland, is a PGE-copper-

nickel project that has existing NI43-101 Mineral Resources, while both the Tyko and Canalask high-

grade nickel-copper projects are located in Ontario and the Yukon, Canada, respectively. Follow

Palladium One on

LinkedIn

,

Twitter

, and at

www.palladiumoneinc.com

.

ON BEHALF OF THE BOARD

"Derrick Weyrauch"

President & CEO, Director

For further information contact:

Derrick Weyrauch, President & CEO

Email:

[email protected]

Neither the TSX Venture Exchange nor its Market Regulator (as that term is defined in the

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

this release.

Information set forth in this press release may contain forward-looking statements. Forward-looking

statements are statements that relate to future, not past events. In this context, forward-looking

statements often address a company's expected future business and financial performance, and often

contain words such as "anticipate", "believe", "plan", "estimate", "expect", and "intend", statements

that an action or event "may", "might", "could", "should", or "will" be taken or occur, or other similar

expressions. These forward-looking statements include, but are not limited to, statements relating

the

2023 exploration program and its focus and results

; the pending results of the Company's previous

drilling; the standards of testing; and other statements that are not historical facts. By their nature,

forward-looking statements involve known and unknown risks, uncertainties and other factors which

may cause our actual results, performance or achievements, or other future events, to be materially

different from any future results, performance or achievements expressed or implied by such forward-

looking statements. Such factors include, among others, risks associated with project development;

the need for additional financing; operational risks associated with mining and mineral processing;

fluctuations in palladium and other commodity prices; title matters; environmental liability claims and

insurance; reliance on key personnel; the absence of dividends; competition; dilution; the volatility of

our common share price and volume; and tax consequences to Canadian and U.S. Shareholders.

Forward-looking statements are made based on management's beliefs, estimates and opinions on

the date that statements are made and the Company undertakes no obligation to update forward-

looking statements if these beliefs, estimates and opinions or other circumstances should change.

Investors are cautioned against attributing undue certainty to forward-looking statements.

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

https://www.newsfilecorp.com/release/159861