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Southern Silver Reports Enriched Rare Earth Elements in Hole OR22-012; Extends Claims to Cover New Copper and REE Skarn/CRD Targets at the Oro Project, New Mexico; and Provides Corporate Update

Property Options & Staking

Southern Silver Reports Enriched Rare Earth

Elements in Hole OR22-012; Extends Claims to

Cover New Copper and REE Skarn/CRD

Targets at the Oro Project, New Mexico; and

Provides Corporate Update

Vancouver, British Columbia--(Newsfile Corp. - November 14, 2023) -

Southern Silver Exploration

Corp. (TSXV: SSV) ("Southern Silver" and the "Company")

reports that it has verified enriched

Rare Earth Elements (REEs) in reconnaissance hole OR22-012, which was part of the Company's 2022

drilling program at its wholly owned Oro property, located in the Laramide-age, porphyry copper belt of

southwestern New Mexico, USA. The Company has staked 62 new claims during 2023 to cover the

western extension of the buried porphyry/CRD/Skarn system associated with hole OR22-012. The new

claims increase the total Oro land package to 334 company-owned and seven leased Federal lode

mining claims; two leased New Mexico State parcels; and company-owned private surface and mineral

titles covering an area of about 36 square kilometres.

Rare-Earth Element Results

The Company reports that a review of select light Rare Earth Elements (LREEs) from the earlier MS-ICP

analyses from hole OR22-012 identified strong LREE enrichment. Thirty-nine pulps were selected from

three enriched LREE zones for re-analyses by the more robust analytical method of fusion/ICPMS to

confirm the initial test results and returned:

0.104% TREO (1,045 ppm) over 10.9m starting at 613.9m,

0.091% TREO (913 ppm) over 33.8m starting at 647.4m, and

0.128% TREO (1,285 ppm) over 24.4m starting at 794.0m.

All three zones occur within a 427.2m interval of strongly enriched copper mineralization, which was

previously reported in NR-02-23, dated April 03,2023, and described below. The three zones (see Table

below) average greater than 0.05% Total Rare Earth Oxides (TREOs).

Light REO

ppm

Heavy REO

ppm

From

m

To m

Interval

m

TLREO

%

La2O3

CeO2

Pr2O3

Nd2O3

Sm2O3

Eu2O3

Gd2O3

Tb2O3

Dy2O3

Ho2O3

Er2O3

Tm2O3

Yb2O3

Lu2O3

Y2O3

THREO

%

TREO

%

613.9

615.7

1.7

0.050

195

226

16.4

46.8

7.2

2.1

5.4

0.78

4.6

0.81

2.4

0.32

1.9

0.28

25

0.004

0.053

615.7

618.7

3.0

0.056

233

256

17

44.8

6.4

2.4

5.1

0.66

3.8

0.69

1.8

0.26

1.7

0.24

20

0.003

0.059

618.7

621.8

3.0

0.049

203

219

14

37.3

5.9

2.1

4.6

0.66

3.8

0.79

2.1

0.27

1.8

0.2

22

0.003

0.052

621.8

624.8

3.0

0.227

1005

1045

63

137

10.6

2.8

7.4

1.01

5.6

0.97

2.9

0.34

2.3

0.32

30

0.004

0.231

Interval

(m)

10.9

Average

0.104

647.4

648.9

1.5

0.039

148

177

13.5

39.9

6.4

1.7

6

0.84

4.5

0.87

2.4

0.29

2.2

0.27

27

0.004

0.043

648.9

650.4

1.5

0.086

359

396

26.1

63

8.8

1.9

5.6

0.78

4.5

0.85

3

0.31

2

0.3

25

0.004

0.090

650.4

651.5

1.1

0.074

317

334

21.7

54.8

7.1

1.9

6.1

0.96

5.6

1.15

3.5

0.55

3.3

0.45

37

0.005

0.080

651.5

654.4

2.9

0.069

289

316

20.9

53.9

6.7

2

5.2

0.75

4

0.86

2.2

0.3

1.8

0.22

24

0.003

0.073

654.4

657.4

3.0

0.009

23

37

3.7

14

4.2

1.2

4.1

0.61

3.7

0.73

1.9

0.32

1.8

0.3

22

0.003

0.012

657.4

658.9

1.5

0.005

12

23

2.3

8.7

2.6

0.8

3.1

0.49

2.9

0.65

1.6

0.26

1.7

0.27

19

0.003

0.008

658.9

660.5

1.5

0.016

61

69

4.8

15.3

3.8

1

4.5

0.7

4.4

0.85

2.4

0.34

2.4

0.33

28

0.004

0.020

660.5

662.6

2.1

0.106

461

485

29.8

68.4

8.1

2.1

6.7

0.94

5.4

0.96

2.7

0.38

2.3

0.28

29

0.004

0.110

662.6

664.4

1.8

0.147

645

678

41.5

91.4

9.9

2.1

6.6

0.86

4.7

0.92

2.7

0.33

2.3

0.24

29

0.004

0.152

664.4

665.5

1.1

0.067

287

307

19

45.4

5.5

1.4

4.7

0.7

4.1

0.8

1.9

0.29

1.7

0.19

22

0.003

0.070

665.5

666.0

0.5

0.007

22

29

2.7

9.7

2.3

0.7

2.7

0.38

2.3

0.5

1.6

0.23

1.3

0.16

15

0.002

0.009

666.0

666.6

0.7

0.087

399

397

21.8

42.7

4.1

1.2

3.7

0.53

3.1

0.58

1.7

0.22

1.6

0.16

20

0.003

0.090

666.6

669.0

2.4

0.378

1770

1725

92.8

171.5

11

2.4

6.7

0.96

4.9

0.95

2.6

0.34

2

0.3

29

0.004

0.382

669.0

670.5

1.5

0.135

609

611

34.9

76.4

7.7

2

6.2

0.79

4.9

0.93

2.4

0.29

2

0.31

28

0.004

0.139

670.5

672.1

1.5

0.031

129

140

9.1

24.6

4.4

1.2

3.8

0.58

3.2

0.69

1.7

0.22

1.5

0.18

20

0.003

0.034

672.1

673.6

1.5

0.011

35

42

3.7

16.4

4.9

1.4

4.8

0.78

4.7

0.9

2.5

0.32

2.2

0.28

28

0.004

0.015

673.6

675.1

1.5

0.033

115

154

12.5

38.7

5.8

1.6

4.4

0.64

3.8

0.73

1.9

0.26

1.7

0.24

22

0.003

0.036

675.1

678.1

3.0

0.105

446

490

30.7

69.6

7.1

2.1

4.8

0.7

3.9

0.72

2.3

0.27

1.6

0.2

23

0.003

0.108

678.1

681.2

3.0

0.091

409

419

23.3

48.5

4.1

0.9

2.7

0.36

2.1

0.37

0.9

0.14

0.8

0.08

11

0.002

0.092

Interval

(m)

33.8

Average

0.091

794.0

797.0

3.0

0.265

1170

1240

72.3

151

11.4

1.9

6

0.78

4

0.72

1.9

0.24

1.6

0.23

23

0.003

0.269

797.0

800.1

3.0

0.069

294

322

19.9

46.3

5.7

1.4

4.7

0.62

3.4

0.7

1.6

0.21

1.5

0.25

20

0.003

0.072

800.1

803.1

3.0

0.092

388

424

26

62.2

7.9

2

6.3

0.83

4.5

0.79

2.3

0.31

1.8

0.24

25

0.004

0.095

803.1

806.2

3.0

0.177

793

825

44.7

87.1

8.1

1.7

5.5

0.73

4

0.78

1.8

0.27

1.8

0.28

23

0.003

0.180

806.2

809.2

3.0

0.202

927

935

50.4

94.6

8.2

1.7

5.6

0.74

4

0.71

1.9

0.29

1.7

0.23

22

0.003

0.205

809.2

812.3

3.0

0.087

373

404

24.6

56.7

7.4

1.6

5.8

0.9

4.8

0.88

2.5

0.35

2.3

0.3

27

0.004

0.091

812.3

815.3

3.0

0.048

161

226

18.7

58.8

9.6

1.7

7.7

0.98

6.3

1.24

3.5

0.46

2.8

0.44

34

0.005

0.053

815.3

816.6

1.3

0.067

247

316

23.4

67.2

10.7

1.9

8.1

0.93

6.1

1.16

3.3

0.48

2.8

0.44

34

0.005

0.072

816.6

818.3

1.7

0.052

220

242

14.7

34.5

5.1

1.2

3.7

0.4

3.1

0.65

1.9

0.27

1.7

0.26

20

0.003

0.055

Interval

(m)

24.4

Average

0.128

Table of REO values from three REE-enriched zones in core hole OR22-012. Fusion/ICPMS.

Consultant Joe Kizis commented,

"The mineralization in hole OR22-012 was initially very encouraging

to us because it demonstrates the importance of favorable carbonate host rocks in developing strong

copper mineralization. Perhaps importantly, REEs are not enriched in other portions of the Oro

property, even within well zoned, but weak, copper porphyry -style mineralization and may thus

indicate the porphyry system we believe lies to the west of OR22-012 is unique compared to other

porphyries on the property.

More study will be required before we know if there is potential for byproduct REE's at Oro. There are

16 separate rare earth elements contained within at least 245 separate minerals, so metallurgy is very

important to understanding the economic possibilities of these potential byproducts. One easily

leached REE deposit in the US reports an average grade of 0.06% TREO and is being considered for

economic development. However, these lowest grade deposits have a higher percentage of HREEs

than we have seen at Oro to date, as well as other coproducts. REEs have many uses, ranging from

additives to batteries, magnets, automobile windshields, and ceramics to processing petroleum. With

about 90% of REEs being sourced from China, it's not surprising that the US, Canada, and other parts

of the world consider REEs as Critical Minerals. With the newly acquired ground, we now have the

room to develop these exciting targets."

Drill Hole OR22-012

Drill hole OR22-012

tested a strong ZTEM geophysical anomaly in an area believed to be relatively

high in the metal system where mapping, geochemistry and geophysical data suggests a porphyry

system lies at depth to the west on the newly stake ground.

The REE-enrich intervals occur within a broad 427.7m* Cu-enriched mineralized zone averaging 0.15%

CuEq* (0.08% Cu, 0.01% Mo, and 1.4g/t Ag) and starting at 578.6m downhole (see NR-02-23, dated

April 03, 2023).

Within the broader mineralized zone, OR22-012 intersected veins with strongly

anomalous gold (

12.4 g/t over 0.8 metres* at 495.7 metres depth

) in a banded anhydrite + pyrite +

calcite breccia vein and, deeper in the hole, intersected anomalous silver and lead (

908 g/t Ag and

10.4% Pb over 0.2 metres* at 594.6 metres depth

) in a barite + galena vein, consistent with expected

metal zoning. Favourable carbonate host rocks were intersected with abundant sulphide minerals below

a 6-metre-thick massive anhydrite vein at roughly 590-metres depth. The strongest mineralization is

9.1

metres* of 0.59% Cu, 0.01% Mo, 0.3 g/t Au, and 2.3g/t Ag (0.92% CuEq*)

from 834.5 to 843.7

metres in a carbonate replacement zone with abundant magnetite, specular hematite, and epidote with

minor pyrite, calcite, and anhydrite. Dikes ranging from unaltered to strongly altered are common

throughout the hole.

*Note- Estimated true thickness is unknown at this time. Equivalent values are calculated based on

prices of $1700/oz Au, $20/oz Ag, $3.25/oz Cu, $1/lb Pb, $1.2/lb Zn and $18/lb Mo assuming 100%

metal recoveries.

QA/QC Procedures

Core was logged and marked for cutting and sampling at Southern Silver's Hachita secure core shed,

then picked up by Skyline Assayers & Laboratories and delivered to their Tucson, Arizona facility where

the core was cut and analyzed. Gold was analyzed by Fire Assay-AAS or gravimetric if overlimit (FA-01

or FA-02) with 47-element ICP/MS multi-acid digestion (TE-5). A QA/QC standard or blank was inserted

at least every 20 samples and 10% of the samples were assayed in duplicate. No issues were identified

in quality control.

Pulps from three intervals averaging +0.05% La + Ce + Y and shoulder samples were submitted to ALS

Chemex in Reno, Nevada and Vancouver, BC where they were homogenized (HOM-01m) and then

assayed for High-grade REE by fusion/ICPMS (ME-MS8h). Comparison of Fusion/ICPMS values to

MS/ICP values of La + Ce + Y only in the three zones are 0%, +22% and +27%, with individual sample

pairs showing more variation. The higher values in the High-grade REE by fusion method reflects the

effect of complete digestion of samples and the addition of Pr and Nd contributions, which were not

analyzed by the non-fusion method.

Land map showing new claims staked at Oro Project, New Mexico

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

https://images.newsfilecorp.com/files/5344/187352_9515484fa4270b31_003full.jpg

Corporate Update

The Company also reports that it is pleased to announce the appointment of Jay Oness as Vice

President, Corporate Development. Mr. Oness has over 25 years of corporate communications,

strategic marketing and corporate development experience and has been a director and officer of

numerous publicly traded North American resource companies. Mr. Oness will be responsible for

general corporate development, and supporting management to evaluate and execute new investment

opportunities.

He is currently serving as the VP of Corporate Development at Malaspina-Manex Group where he is

responsible for overseeing, implementing, and managing various corporate functions and shareholder

programs for public and private companies.

About Oro

The Oro property consists of patented land, New Mexico State leases, and Federal/BLM mineral claims

acquired by purchase, staking and lease over the past several years. Several historic mines produced

copper, lead, zinc, silver, and gold from discrete portions of the amalgamated property. The property

covers a large, well-zoned Laramide-age mineral system consisting of a ring of Carbonate Replacement

Deposits (CRDs) around a core of intense sericite-pyrite alteration, which clay mineralogy indicates is

the lithocap overlying unexposed porphyry centres. Targeting for copper mineralization is based upon

3D modelling of data generated by geologic mapping, historic drill holes, geochemical zoning studies,

alteration clay zoning studies, and geophysical surveys.

Surrounding the CRD zone are distal-disseminated, sediment-hosted, gold showings, such as at the

Stockpond target, where the Company has conducted limited exploratory drilling. The drilling

encountered strongly oxidized, disseminated gold mineralization beneath shallow gravel cover that was

limited by a post-mineral fault which buried potential extensions beneath a thick cover of gravel, and

which remains open for further exploration.

About Southern Silver Exploration Corp.

Southern Silver Exploration Corp. is an exploration and development company with a focus on the

discovery of world-class mineral deposits either directly or through joint-venture relationships in mineral

properties in major jurisdictions. Our specific emphasis is the 100% owned Cerro Las Minitas silver-

lead-zinc project located in the heart of Mexico's Faja de Plata, which hosts multiple world-class mineral

deposits such as Penasquito, Los Gatos, San Martin, Naica and Pitarrilla. We have assembled a team

of highly experienced technical, operational, and transactional professionals to support our exploration

efforts in developing the Cerro Las Minitas project into a premier, high-grade, silver-lead-zinc mine. Our

property portfolio also includes two projects in southern New Mexico: the Oro porphyry/CRD copper-gold

project; and the Hermanas gold-silver vein project, where an application has been submitted for a drilling

program.

Robert Macdonald, MSc. P.Geo, is a Qualified Person as defined by National Instrument 43-101 and

has reviewed and approved the technical disclosure in this news release. Joe Kizis, also a Qualified

Person as defined by National Instrument 43-101, supervised directly the collection of the data from the

Oro project that is reported in this disclosure and is responsible for the presentation of the technical

information in this disclosure.

On behalf of the Board of Directors

"Lawrence Page"

Lawrence Page, K.C.

President & Director, Southern Silver Exploration Corp.

For further information, please visit Southern Silver's website at;

https://www.southernsilverexploration.com

or contact us at 604.641.2759 or by email at

[email protected]

.

Neither 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.

This news release contains forward-looking statements. Forward-looking statements address future

events and conditions and therefore involve inherent risks and uncertainties. Actual results may differ

materially from those currently anticipated in such statements. Factors that could cause actual results

to differ materially from those in forward looking statements include the timing and receipt of

government and regulatory approvals, and continued availability of capital and financing and general

economic, market or business conditions.

Southern Silver Exploration Corp. does not assume any

obligation to update or revise its forward-looking statements, whether as a result of new information,

future events or otherwise, except to the extent required by applicable law.

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

https://www.newsfilecorp.com/release/187352