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LIFT.V ·

LIFT Announces Results of Exploration Activities at the Cali Lithium Project, NWT

Exploration Programs

LIFT Announces Results of Exploration

Activities at the Cali Lithium Project, NWT

Vancouver, British Columbia--(Newsfile Corp. - October 16, 2025) - LiFT Power Ltd.

(TSXV: LIFT)

(OTCQX: LIFFF) (FSE: WS0)

("

LIFT

" or the "

Company

") is pleased to announce results of exploration

activities at the Cali Lithium Project in the Northwest Territories, Canada (Figure 1).

Figure 1 - Location of LIFT's Cali Project in the NWT.

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

https://images.newsfilecorp.com/files/8766/270555_bc7fdbd944657beb_001full.jpg

Background

The Cali Project is located at the northwest extent of the Little Nahanni Pegmatite Group (LNPG), a

district-scale zone of parallel-trending spodumene pegmatites dykes that form a corridor 13 km long,

and hundreds of metres wide (Figure 2). The extensive rock exposures of dykes across LIFT's property

provide excellent conditions for evaluating the economic potential of the dyke corridor through systematic

mapping, prospecting, and channel sampling programs. In 2023, LIFT completed geological mapping

and sampling (158 rocks, Table 2) of pegmatite exposures in the southeastern part of the Cali property

(the "2023 work area" in Figure 2), defining an area of strong spodumene mineralization approximately

1 km by 1.5 km.

The 2025 field program builds on the 2023 work program with systematic channel sampling and

mapping targeting grade, width, and metallurgical recovery information. In addition, first-pass mapping,

and grab/channel sampling were carried out on LIFT's newly staked claims further to the northwest,

where helicopter-borne reconnaissance in 2024 identified multiple additional pegmatite occurrences

from the air (see Figure 2, NW-01 & NW-02).

Dyke exposures on the property occur both as bedrock outcrops and as fields of angular, frost-shattered

rock fragments. These broken and fragmented subcrops form directly above bedrock through freeze-

thaw processes, with little to no dispersion. This contrasts with "float" samples, which are completely

detached and transported tens to hundreds of metres from their source outcrops. For the purposes of the

channel sampling presented herein, the shattered subcrops are interpreted to accurately reflect the

underlying bedrock geology and are therefore treated as in-situ samples.

Figure 2 - Map showing results of 2025 and 2023 rock sampling. The inset figures show 2025 channel

sampling results.

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

https://images.newsfilecorp.com/files/8766/270555_bc7fdbd944657beb_002full.jpg

Results of 2025 work

A total of 43 rock samples were collected from surface dyke exposures, and 24 channels ranging from 2

to 23 m in length were cut, yielding 187 one-metre samples. In situ channel samples from outcrop and

frost-shattered sub crop were collected using a circular saw to cut two parallel grooves, 5-10 cm apart

and oriented broadly perpendicular to dyke contacts (Figures 3 & 4). Reported composites are

calculated using a 0.50% Li

O cut-off. Some composites include frost-shattered material, which can

make dyke margins difficult to define. In some cases, this may result in slightly narrower true widths than

those reported in Table 1.

In the 2023 work area, 160 one-metre samples were collected from 19 channels ranging between 2 and

19 m in length. Individual channel samples were assayed for lithium and subsequently combined into

composites, which are presented in Table 1 and shown in Figure 3. Select channel samples were also

submitted for metallurgical recovery test work, with results expected in Q1 2026. Of the 19 channels, 17

returned at least two consecutive metres grading above 0.8% Li

O, including a highlight of 1.9% Li

O

over 21 consecutive metres (Table 1; Figure 3). Geological mapping indicates the spodumene dykes in

this area are typically 1-5 m wide and are intercalated with barren metasedimentary country rock.

Mapping and prospecting in the previously staked northwest extension of the LNPG corridor (NW-01 and

NW-02 in Figure 2) have confirmed the 2024 helicopter-borne reconnaissance results, with six new

spodumene-bearing pegmatites confirmed and sampled in the field (Figure 4). These new dykes extend

the LNPG corridor, as defined by LIFT's 2023 work, by an additional 3 km to the northwest, with a

minimum width of 400 m. The corridor remains open for further widening to the southwest and for along-

strike extension to the northwest.

The NW-01 area hosts two in-situ spodumene dyke zones and two areas of spodumene-bearing

pegmatite float leading back to dyke outcrops higher up in the catchment. The largest dyke swarm in this

area is exposed over 450 m of strike and consists of several thin, sub-parallel dykes ranging from 1 to 5

m in width (Figure 4a). Twenty-three of the 34 rock samples collected were taken from this swarm, with

16 assaying above 1.0% Li

O and a peak grade of 2.9% Li

O (Table 2). An additional 11 samples

collected from other spodumene occurrence in the same area returned similar lithium concentrations

(Table 2).

An additional four new spodumene dykes were found in the NW-02 area (Figures 2 & 4b), with assays of

nine spodumene pegmatite samples returning six samples >1.0% Li

O and a maximum of 2.2% Li

O

(Table 2). No channel samples were taken from these dykes.

Figure 3 - Detailed maps and channel sample results for pegmatite dykes in the 2023 mapping area.

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

https://images.newsfilecorp.com/files/8766/270555_bc7fdbd944657beb_003full.jpg

Figure 4a-b - Location of newly discovered pegmatite dykes in the (a) NW-01 and (b) NW-02 areas, as

well as channel sampling results.

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

https://images.newsfilecorp.com/files/8766/270555_bc7fdbd944657beb_004full.jpg

Table 1: 2025 channel sampling composites

Area

Channel

Length (m)

Li20 (%)

2023 work Area

TR1A

2

0.78

TR1B

6

1.11

TR1C

6

1.34

TR3

No significant results

TR5A

5

1.54

TR5B

6

1.21

TR5C

5

1.42

TR6

2

1.88

TR7

3

1.49

TR08

20

0.97

TR08-B

8

1.22

TR12A

21

1.26

TR12B

9

1.25

TR13

21

1.04

TR24A

6

1.01

TR24B

4

0.99

TR27

No significant results

TR28

2

1.33

TR32

14

1.3

NW_01

TR33

3

1.45

TR34

3

2.43

TR35

5

0.91

TR36

8

0.65

TR37

No significant results

Table 2: Overview of 2025 rock sampling results

Area

Samples

% Li2O

<0.5

0.5-1.0

1.0-1.5

1.5-2.0

>2.0

Max

NW-01

34

18%

12%

24%

18%

29%

2.86

NW-02

9

11%

22%

33%

22%

11%

2.21

2025 Total

43

16%

14%

26%

19%

26%

2.86

2023 Area

158

6%

15%

41%

25%

14%

3.05

Francis MacDonald, President & CEO of LIFT comments, "The 2025 exploration program will

significantly advance the understanding and economic potential of the Cali Lithium Project. By

integrating channeling, metallurgical testing, and extensive prospecting across underexplored extensions

of the spodumene corridors, LIFT aims to position the project for potential future resource delineation."

Qualified Person

The disclosure in this news release of scientific and technical information regarding LIFT's mineral

properties has been reviewed and approved by Ron Voordouw, Ph.D., P.Geo., Partner, Director

Geoscience, Equity Exploration Consultants Ltd., and a Qualified Person as defined by National

Instrument 43-101 Standards of Disclosure for Mineral Projects (NI 43-101) and member in good

standing with the Northwest Territories and Nunavut Association of Professional Engineers and

Geoscientists (NAPEG) (Geologist Registration number: L5245).

About LIFT

LIFT is a mineral exploration company engaged in the acquisition, exploration, and development of

lithium pegmatite projects located in Canada. The Company's flagship project is the Yellowknife Lithium

Project located in Northwest Territories, Canada. LIFT also holds three early-stage exploration

properties in Quebec, Canada with excellent potential for the discovery of buried lithium pegmatites, as

well as the Cali Project in Northwest Territories within the Little Nahanni Pegmatite Group.

For further information, please contact:

Francis MacDonald

Chief Executive

Tel: + 1.604.609.6185

Email:

[email protected]

Website:

www.li-ft.com

Daniel Gordon

Officer Investor Relations

Tel: +1.604.609.6185

Email:

[email protected]

Cautionary Statement Regarding Forward-Looking Information

Certain statements included in this press release constitute forward-looking information or statements

(collectively, "forward-looking statements"), including those identified by the expressions "anticipate",

"believe", "plan", "estimate", "expect", "intend", "may", "should" and similar expressions to the extent

they relate to the Company or its management. The forward-looking statements are not historical facts

but reflect current expectations regarding future results or events. This press release contains forward

looking statements. These forward-looking statements and information reflect management's current

beliefs and are based on assumptions made by and information currently available to the company

with respect to the matter described in this new release.

Forward-looking statements involve risks and uncertainties, which are based on current expectations

as of the date of this release and subject to known and unknown risks and uncertainties that could

cause actual results to differ materially from those expressed or implied by such statements.

Additional information about these assumptions and risks and uncertainties is contained under "Risk

Factors" in the Company's latest annual information form filed on March 21, 2025, which is available

under the Company's SEDAR+ profile at

www.sedarplus.ca

, and in other filings that the Company has

made and may make with applicable securities authorities in the future. Forward-looking statements

contained herein are made only as to the date of this press release and we undertake no obligation to

update or revise any forward-looking statements whether as a result of new information, future events

or otherwise, except as required by law. We caution investors not to place considerable reliance on the

forward-looking statements contained in this press release.

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

news release.

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

https://www.newsfilecorp.com/release/270555