Troy Minerals Reports Analytical Results from Table Mountain Silica Project, Identifying Broad High-Purity Zones

Troy Minerals Reports Analytical Results from Table Mountain Silica

Project,

Identifying

Broad

High-Purity

Zones

Vancouver, B.C. – February 6, 2025 - Troy Minerals Inc. ("Troy" or the "Company") (CSE:

TROY;

OTCQB:

TROYF;

FSE:

VJ3)

is

pleased

to

announce

that

it

has

received

results

from

a

sampling

and

mapping

program

on

its

100%

owned

Table

Mountain

Silica

Project,

located

near

Golden,

British

Columbia,

Canada.

Key Highlights

●

Three

distinct

zones

of

high-purity

silica

mineralization

identified

within

the

Mount

Wilson

Quartzite

Formation.

●

98.86%

SiO₂

over

a

total

of

62.11

metres

of

channel

sampling

in

five

channels

at

the

main

Table

Mountain

Zone.

●

Outcrop

sampling

returned

98.18%

to

99.74%

SiO

2

from

45

samples

at

Table

Mountain

Zone,

97.83%

to

99.49%

SiO₂

from

13

samples

at

South

Zone,

and

95.82%

to

99.82%

SiO₂

from

29

samples

at

Southeast

Zone.

*

●

Very

low

deleterious

elements

identified

in

all

samples.

President of Troy Minerals Inc., Yannis Tsitos commented: "These comprehensive maiden

assay

results

validate

the

potential

of

Table

Mountain

as

a

key

high-purity

silica

asset.

Sampling

confirmed

the

exceptional

quality

and

consistency

of

silica

mineralization

across

the

Project.

With

grades

reaching

98

to

99%

SiO₂

across

multiple

zones

of

extensive

outcrop

exposure,

and

sampling

ranging

from

98.18%

to

99.74%

SiO₂

at

the

main

Table

Mountain

Zone,

we

are

rapidly

advancing

our

understanding

of

this

strategic

asset.

The

Project's

infrastructure

advantages

and

proximity

to

existing

silica

operations

further

enhance

its

potential

as

we

work

to

establish

Troy

as

a

significant

player

in

the

North

American

high-purity

silica

market,

positioning

the

Company

for

long-term

growth."

The sampling program consisted of both systematic grab samples and channel samples, with

a

total

of

110

grab

samples

(107

outcrop

and

3

float)

taken

within

the

property

area

and

70

channel

samples

collected

from

62.11

metres

within

74.16

metres

of

channels.

Figure 1. Index Map

Outcrop Sampling Results

Three main areas returned significant high-purity silica results: the Table Mountain Zone,

located

at

the

north

end

of

the

Property,

the

South

Zone,

and

the

Southeast

Zone.

The most extensively sampled zone was the Table Mountain Zone, which returned an

average

grade

of

98.90%

SiO₂

from

45

grab

samples

(42

outcrop,

3

float),

with

values

ranging

from

98.18%

to

99.74%

SiO₂.

Additionally,

from

these

samples

the

following

average

values

were

returned:

0.31%

Fe₂O₃,

0.01%

CaO,

0.14%

Al₂O₃,

0.02%

MgO,

0.01%

TiO₂,

0.01%

P₂O

₅

,

and

14ppm

boron.

See

Figure

2

and

Table

1

.

*

Figure 2. Table Mountain Zone Outcrop Sampling - %SiO

2

Table 1. Table Mountain Zone Outcrop Samples

Sample # Easting (m)

Northing (m)

SiO

2

(%)

Al

2

O

3

(%)

CaO (%)

Fe

2

O

3

(%)

MgO (%)

P

2

O

5

(%)

TiO

2

(%)

B (ppm) 299516 509114 5685249 99.41 0.11 0.02 0.39 0.01 <0.01 <0.01 6 299517 509193 5685166 98.84 0.14 0.01 0.23 0.02 <0.01 <0.01 8 299518 509314 5685171 99.20 0.10 0.01 0.25 0.02 <0.01 0.01 10 299519 509350 5685151 98.26 0.12 0.01 0.35 0.01 <0.01 0.01 15 299520 509369 5685129 99.20 0.13 0.01 0.21 <0.01 <0.01 0.03 16 299521 509395 5685107 99.17 0.15 0.01 0.27 0.02 <0.01 0.01 8 299522 509418 5685094 98.78 0.23 0.02 0.26 0.01 <0.01 0.01 12 299523 509442 5685075 98.59 0.14 0.02 0.26 <0.01 0.01 0.01 12 299524 509450 5685043 99.74 0.07 0.01 0.30 0.01 0.01 0.01 6 299525 509471 5685019 98.58 0.04 0.01 0.36 0.01 0.01 0.01 7 299526 509482 5684990 99.25 0.14 0.02 0.27 0.04 0.01 0.01 7 299527 509500 5684961 99.66 0.16 0.02 0.31 0.02 0.01 0.01 7 299528 509515 5684938 99.21 0.14 0.01 0.32 0.02 0.01 0.01 7 299529 509538 5684911 99.13 0.11 0.01 0.27 0.03 0.01 0.01 21 299530 509561 5684862 98.18 0.25 0.01 0.31 0.03 0.01 0.01 7 299531 509598 5684823 98.93 0.27 0.02 0.36 0.03 0.01 0.01 7 299532 509583 5684759 98.99 0.09 0.01 0.30 <0.01 0.01 0.01 7 299533 509619 5684743 98.72 0.16 0.01 0.35 0.02 0.01 0.01 14 299534 509641 5684726 98.18 0.30 0.01 0.33 0.04 0.01 0.02 15 299535 509712 5684697 99.41 0.13 0.01 0.30 0.02 0.01 0.01 7

299536 509736 5684685 99.27 0.11 0.01 0.33 0.02 0.01 0.01 7 299537 509764 5684670 98.58 0.13 0.02 0.36 0.03 0.01 0.02 8 299548 509306 5685510 99.32 0.14 0.01 0.29 0.01 0.01 0.01 18 299560 509476 5685127 98.99 0.13 0.01 0.32 0.03 0.01 0.02 27 299561 509472 5685107 99.01 0.05 0.01 0.32 0.01 0.01 <0.01 18 299562 509457 5685115 98.74 0.15 0.01 0.26 0.01 0.01 0.02 28 299563 509439 5685112 98.35 0.20 0.02 0.34 0.02 0.01 0.01 27 299564 509459 5685092 99.20 0.09 0.01 0.32 <0.01 0.01 0.01 21 299565 509487 5685107 99.49 0.09 0.01 0.28 0.03 0.01 0.02 28 299566 509490 5685083 98.48 0.25 0.02 0.35 0.01 0.01 0.01 26 299567 509503 5685071 99.03 0.11 0.02 0.34 0.02 0.01 <0.01 21 299568 509477 5685067 99.16 0.10 0.01 0.30 <0.01 0.01 <0.01 18 299569 509478 5685044 98.68 0.10 0.01 0.32 0.03 0.01 <0.01 20 299570 509506 5685041 98.46 0.43 0.02 0.32 0.06 0.01 0.01 29 299571 509523 5685054 98.81 0.13 0.01 0.31 0.03 0.01 0.01 22 299572 509382 5685160 98.42 0.09 0.01 0.29 0.01 0.01 0.01 23 299573 509397 5685160 98.92 0.11 0.01 0.36 <0.01 0.01 <0.01 18 299574 509406 5685142 99.12 0.09 0.01 0.30 0.02 0.01 <0.01 17 299575 509409 5685120 98.56 0.14 0.01 0.37 <0.01 0.01 <0.01 21 299581 509357 5685172 98.84 0.08 0.02 0.32 <0.01 0.01 0.01 18 299582 509429 5685142 98.87 0.15 0.01 0.29 <0.01 0.01 0.02 8 299583 509446 5685146 98.25 0.33 0.02 0.33 0.03 0.01 0.03 17 299584 509455 5685145 99.49 0.11 0.02 0.27 <0.01 0.01 0.01 5 299585 509473 5685142 98.66 0.08 0.01 0.36 <0.01 0.01 <0.01 6 299586 509493 5685133 98.52 0.05 0.01 0.29 <0.01 0.01 <0.01 <5

Note: 299548, 299584, and 299585 are float samples taken near outcrop.

The South Zone, comprising 13 high-grade quartzite outcrop grab samples averaged 98.80%

SiO₂

with

values

ranging

from

97.83%

to

99.49%

SiO₂.

These

samples

averaged

0.28%

Fe₂O₃,

0.13%

CaO,

0.13%

Al₂O₃,

0.02%

MgO,

<0.01%

TiO₂,

0.02%

P₂O

₅

,

and

6ppm

boron.

See

Figure

3

and

Table

2

.

*

Figure 3. South Zone Outcrop Sampling - %SiO

2

Table 2. South Zone Outcrop Samples

Sample # Easting (m)

Northing (m)

SiO

2

(%)

Al

2

O

3

(%)

CaO (%)

Fe

2

O

3

(%)

MgO (%)

P

2

O

5

(%)

TiO

2

(%)

B (ppm) 248351 511603 5682006 98.60 0.28 0.08 0.25 0.04 0.01 0.01 15 248352 511563 5681948 99.45 0.15 0.02 0.22 0.02 0.01 <0.01 6 248353 511552 5681948 99.01 0.19 0.03 0.29 0.04 0.01 0.01 9 248354 511551 5681951 99.09 0.11 0.02 0.22 0.03 0.01 0.01 6 248355 511530 5681940 98.74 0.09 0.02 0.23 <0.01 0.01 <0.01 6 248356 511522 5681942 98.82 0.08 0.01 0.31 <0.01 0.01 <0.01 <5 248357 511512 5681951 98.31 0.09 0.01 0.24 0.01 0.01 0.01 5 248358 511485 5681948 98.14 0.13 0.28 0.32 0.03 0.01 0.01 8 248359 511461 5681935 99.49 0.11 0.02 0.30 0.02 0.01 <0.01 10 248360 511436 5681932 99.06 0.03 0.05 0.25 0.01 0.02 <0.01 5 248361 511444 5681918 99.42 0.07 0.01 0.29 0.02 0.01 <0.01 6 248362 511440 5681942 97.83 0.32 0.73 0.36 0.03 0.03 0.01 8 248364 511374 5682002 98.43 0.09 0.43 0.36 <0.01 0.16 <0.01 <5

The Southeast Zone, comprising 29 high-grade quartzite outcrop grab samples, returned an

average

of

98.52%

SiO₂

with

values

ranging

from

95.82%

to

99.82%

SiO₂.

Average

values

for

other

constituents

were:

0.35%

Fe₂O₃,

0.07%

CaO,

0.30%

Al₂O₃,

0.06%

MgO,

0.02%

TiO₂,

<0.01%

P₂O

₅

,

and

26ppm

boron.

See

Figure

4

and

Table

3

.*

Figure 4. Southeast Zone Outcrop Sampling - %SiO

2

Table 3. Southeast Zone Outcrop Samples - %SiO

2

Sample # Easting (m)

Northing (m)

SiO

2

(%)

Al

2

O

3

(%)

CaO (%)

Fe

2

O

3

(%)

MgO (%)

P

2

O

5

(%)

TiO

2

(%)

B (ppm) 248384 513642 5680350 98.22 0.37 0.21 0.41 0.14 0.02 0.03 27 248385 513671 5680320 95.82 0.57 0.69 0.51 0.52 0.02 0.03 30 248386 513685 5680313 97.77 0.48 0.05 0.37 0.05 0.01 0.03 30 248387 513708 5680285 98.90 0.36 0.02 0.35 0.04 <0.01 0.03 30

248388 513735 5680261 98.11 0.32 0.03 0.31 0.04 <0.01 0.03 35 248389 513748 5680244 98.05 0.49 0.03 0.30 0.03 <0.01 0.01 28 248390 513654 5680223 98.91 0.13 0.01 0.27 0.04 <0.01 0.01 29 248391 513627 5680208 98.74 0.09 0.02 0.30 0.02 <0.01 0.02 27 248392 513600 5680217 99.52 0.06 0.02 0.32 0.03 <0.01 0.01 23 248393 513564 5680220 96.98 1.04 0.05 0.33 0.07 0.03 0.07 41 248394 513592 5680259 98.91 0.30 0.13 0.35 0.13 <0.01 0.02 31 248395 513390 5680466 99.26 0.11 0.02 0.35 0.03 <0.01 0.01 25 248396 513367 5680495 98.81 0.12 0.07 0.34 0.04 <0.01 0.01 25 248397 513332 5680531 99.25 0.08 0.02 0.37 0.01 <0.01 0.01 26

248398 513301 5680539 99.08 0.15 0.21 0.33 0.04 <0.01 0.01 27 248399 513283 5680559 98.76 0.07 0.09 0.36 0.02 <0.01 0.01 22 248400 513263 5680602 98.77 0.08 0.01 0.29 <0.01 <0.01 0.01 24 299501 513231 5680636 98.14 0.15 0.02 0.41 0.02 <0.01 0.01 26 299502 513188 5680660 99.05 0.20 0.02 0.27 <0.01 <0.01 0.01 27 299503 513160 5680700 99.07 0.16 0.02 0.31 0.02 <0.01 0.01 27 299504 513133 5680705 98.85 0.13 0.02 0.26 0.01 <0.01 0.01 26 299508 513834 5679986 98.68 0.15 0.03 0.26 0.02 <0.01 0.01 21 299509 513876 5679941 98.88 0.23 0.03 0.27 0.04 <0.01 0.03 34 299510 513904 5679907 99.08 0.05 0.02 0.29 <0.01 <0.01 0.01 11 299511 513968 5679864 99.82 0.15 0.02 0.27 0.02 <0.01 0.01 23 299512 514023 5679832 99.21 0.12 0.02 0.29 0.03 <0.01 0.03 10 299513 514070 5679980 97.08 1.11 0.02 0.75 0.09 0.01 0.05 18 299514 514081 5680011 96.66 1.27 0.02 0.43 0.05 0.01 0.07 26 299515 514075 5680039 98.58 0.26 0.07 0.45 0.07 0.01 0.03 14

The remainder of samples were either taken near the contacts of the adjacent units or from

non-quartzite

outcrops

of

the

adjacent

Glenogle

shale

(east

contact)

and

Beaverfoot

dolomite

(west

contact)

and

were

not

included

in

the

statistical

summary

of

the

quartzite

samples

taken.

Channel Sampling Results

Channel sampling was conducted at the Table Mountain Zone, with results consistently

similar

to

the

outcrop

sampling

results.

Sampling

procedure

consisted

of

continuous

chip

sampling

along

a

3-centimetre

cut

channel.

Samples

were

taken

continuously

over

1-metre

intervals

perpendicular

to

the

strike

orientation

of

the

outcrop,

with

the

sample

sequence

starting

from

the

southwest

end

of

the

channel.

Intervals

shorter

than

20

centimetres

were

combined

with

the

previous

interval.

66

continuous

chip

channel

samples

were

collected

over

62.11

metres

within

74.16

metres

in

five

channels,

returning

a

weighted

average

of

98.86%

SiO₂.

Four additional duplicates were taken as QA/QC checks and passed validation. Sample

density

is

sufficient

to

indicate

the

accurate

representation

of

the

underlying

mineralization.

See Figure 5 and Table 4 below.

Figure 5. Channel Sampling Locations - Table Mountain Zone

Table 4. Table Mountain Zone - Channel Sampling

Channel From (m)

To (m)

Interval (m)

SiO

2

(%)

Al

2

O

3

(%)

CaO (%)

Fe

2

O

3

(%)

MgO (%)

P

2

O

5

(%)

TiO

2

(%)

B (ppm) TM1 0.00 4.74 4.74 98.83 0.15 0.01 0.30 0.01 0.01 0.01 24

TM2

0.00 5.80 5.80 98.88 0.10 0.01 0.33 0.01 0.01 0.01 10 5.80 6.30 0.50 Overburden 6.30 8.83 2.53 98.90 0.10 0.01 0.30 0.01 0.01 0.02 7 8.83 9.38 0.55 Overburden 9.38 13.0 3.62 99.21 0.09 <0.01 0.35 0.01 0.01 0.02 11

TM3

0.00 7.60 7.60 99.03 0.11 <0.01 0.32 0.01 0.01 0.02 7 7.60 10.20 2.60 Overburden 10.20 11.00 0.80 99.08 0.11 <0.01 0.27 0.01 0.01 0.02 6 11.00 11.90 0.90 Overburden 11.90 18.00 6.10 98.79 0.11 <0.01 0.29 <0.01 0.01 0.02 10 TM4 0.00 5.22 5.22 99.09 0.09 <0.01 0.33 <0.01 0.01 0.02 12

TM5

0.00 3.80 3.80 98.82 0.15 <0.01 0.29 <0.01 0.01 0.04 15

3.80 4.50 0.70 Overburden 4.50 7.00 2.50 98.85 0.12 <0.01 0.31 0.02 0.01 0.02 20 7.00 10.20 3.20 Overburden

10.20 12.00 1.80 98.77 0.09 <0.01 0.34 0.01 <0.01 0.01 12

12.00 13.00 1.00 Overburden

13.00 17.50 4.50 98.30 0.15 0.09 0.34 0.02 <0.01 0.01 13

17.50 20.10 2.60 Overburden

20.10 33.20 13.10 98.81 0.11 <0.01 0.31 0.01 <0.01 0.01 9