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Nevada KING Intercepts 3.41 G/T Au over 54.9M, 2.65 G/T Au over 50.3M, and 2.23 G/T Au over 51.8M, IN Oxide, at Its Atlanta GOLD MINE

Drill Results

NEVADA KING INTERCEPTS 3.41 G/T AU

OVER 54.9M, 2.65 G/T AU OVER 50.3M, AND

2.23 G/T AU OVER 51.8M, IN OXIDE, AT ITS

ATLANTA GOLD MINE

VANCOUVER, BC

,

Oct. 18, 2022

/CNW/ -

Nevada King Gold Corp.

(TSXV: NKG) (OTCQX:

NKGFF) ("

Nevada King

" or the "

Company

") is pleased to announce assay results from 32 reverse

circulation ("

RC

") holes recently completed at its Atlanta Gold Mine Project located 264km northeast

of

Las Vegas, Nevada

, in the prolific Battle Mountain Trend. This drilling includes eight holes

designed to further define the high-grade Atlanta Mine Fault Zone ("

AMFZ

") at the bottom of the

historical

Atlanta

pit, together with 24 shallow holes drilled to test waste dumps from previous mining

north and west of the historical pit.

AMFZ Expansion Drilling Highlights:

Hole No.

From

(m)

To (m)

Interval

(m)

Au (g/t)

AT22NS-46

4.6

59.5

54.9

3.41

AT22NS-59

4.6

54.9

50.3

2.65

AT22NS-43

0

27.4

27.4

1.97

AT22NS-61A

^

6.1

57.9

51.8

2.23

Table 1: Highlight assays from eight expansion holes at Atlanta Gold Mine Project.

^

Denotes angle hole. True widths are unknown at this time.

These four high-grade intercepts in oxide have conclusively defined the footwall contact of the

high-grade AMFZ, including its steep westward dip (Figures 1, 2, and 3). These holes were

collared at the bottom of the historical pit roughly

10m

east of the north-south fence of high-

grade holes drilled by the Company in 2021, which intercepted

54.9m

of 5.34 g/t Au

in AT21-

62,

41.2m

of 3.94 g/t Au

in AT21-63,

64.1m

of 3.94 g/t Au

in AT21-64, and

48.8m

of 2.32 g/t

Au

in AT21-65

,

also starting at or near surface from within the

Atlanta

pit (

see

January 20, 2022

release

).

Drilling is currently underway on benches to the west of the pit floor, stepping out further down-

dip on this high-grade zone, which remains open both to depth and along strike.

Waste Dumps Drilling Highlights:

Hole No.

From

(m)

To (m)

Interval

(m)

Au (g/t)

AT22D-14

0

16.8

16.8

0.75

AT22D-23

4.6

13.7

9.1

1.21

AT22D-31

0

16.8

16.8

0.61

AT22D-33

0

15.2

15.2

0.78

AT22NS-22

6.1

30.5

24.4

0.47

Table 2: Highlight assays from 24 shallow holes testing waste dumps at Atlanta Gold Mine Project.

Today's release also includes results from 24 shallow holes drilled into mine dumps located

immediately to the north and west of the historical open pit (Figure 1). In total, these 24 holes

average

0.49 g/t Au over a

10.8m

thickness within a contiguous area encompassing

59,000m

2

(5.9 hectares) and demonstrate a significant amount of gold mineralization in this area.

This dump-hosted gold mineralization could play an important role in any future mining scenario

as an expansion of the Atlanta Pit to the west would necessitate relocating the material. Based

on the grades and widths identified in this first pass of drilling, the Company believes there is

good potential that a significant portion of this material could be heap leached in any future

operations. Additional drilling is planned to further define this mineralization, along with

metallurgical testwork to assess its economic potential.

Cal Herron

, Exploration Manager of

Nevada King

, stated, "As reported today, the RC holes located

at the bottom of the Atlanta Pit were positioned to firmly establish the location and attitude of the

AMFZ's eastern boundary, prior to initiating the deeper drilling now underway to the west on the

high-grade zone's down-dip extension. We now have a much better understanding of how the

Atlanta

gold deposit formed, of the host geology and of the controls on the spatial distribution of gold

mineralization (see detailed discussion below) that is significantly enhancing our drill targeting. The

Company has been rehabilitating benches in the historical pit over the past four months, work that

will facilitate drilling of critical structures that were inferred from deep angle holes drilled by previous

operators from sites west of the pit. Drilling these structures with predominantly vertical holes will

make for a much more accurate structural interpretation and be significantly more cost effective

compared to the historical angle holes. Many of the historical holes suffered from poor recovery or

failed to fully penetrate the mineralized zones and vertical drilling from these sites should significantly

improve recovery particularly in high-grade target areas. Prior operators were likely impeded by

access and core recovery issues and we are looking at more thoroughly testing these high-grade

target areas."

Figure 1. Location map for holes reported in this news release relative to the perimeter of the

historical Atlanta Pit and 2020 Gustavson pit shell. (CNW Group/Nevada King Gold Corp.)

Figure 2. Cross section C-C’ looking north across centre of historical Atlanta pit illustrating normal

fault displacement on the steeply-dipping Atlanta Mine Fault and progressive down-drop across

parallel faults to the west. The Eureka Quartzite is shown in fault contact with silica breccia and

dolomite units and appears to cut off the Atlanta Fault at depth, but this interpretation is based on 1

historical drill hole, and in other sections the Atlanta Fault clearly displaces quartzite contact. (CNW

Group/Nevada King Gold Corp.)

Figure 3. Cross section D-D’ looking north across the south-central part of the historical Atlanta pit

showing progressive down-drop of the mineralized silica breccia zone and the basal quartzite contact

along a series of parallel faults comprising the Atlanta Mine Fault Zone. Note the start of gold

mineralization in the volcanic/sedimentary package above the silica breccia horizon at the left side of

the section. (CNW Group/Nevada King Gold Corp.)

Hole #

Type of Hole

From (m)

To (m)

Interval (m)

Au (g/t)

AT22NS-43

Resource Hole

0.0

27.4

27.4

1.97

AT22NS-43A

Resource Hole

3.0

30.5

27.4

1.02

AT22NS-46

Resource Hole

4.6

59.5

54.9

3.41

AT22NS-59

Resource Hole

4.6

54.9

50.3

2.65

AT22NS-60

Definition Hole

0.0

30.5

30.5

<0.20

AT22NS-61

Definition Hole

0

18.3

18.3

<0.10

AT22NS-61A

Resource Hole

6.1

57.9

51.8

2.23

AT22NS-72

Definition Hole

0.0

76.2

76.2

<0.05

AT22D-1

Dump Hole

15.2

19.8

4.6

0.29

AT22D-2

Dump Hole

16.8

25.9

9.1

0.39

AT22D-3

Dump Hole

0

6.1

6.1

0.27

AT22D-4

Dump Hole

7.6

27.4

19.8

0.26

AT22D-5

Dump Hole

15.2

25.9

10.7

0.16

AT22D-8

Dump Hole

7.6

9.1

1.5

0.37

AT22D-9

Dump Hole

7.6

16.8

9.1

0.72

AT22D-10

Dump Hole

9.1

21.3

12.2

0.62

AT22D-11

Dump Hole

18.3

25.9

7.6

0.57

AT22D-14

Dump Hole

0.0

16.8

16.8

0.75

AT22D-18

Dump Hole

0

10.7

10.7

0.36

AT22D-20

Dump Hole

3.0

24.4

21.3

0.16

AT22D-23

Dump Hole

4.6

13.7

9.1

1.21

AT22D-28

Dump Hole

0.0

13.7

13.7

0.19

AT22D-29

Dump Hole

12.2

13.7

1.5

0.22

AT22D-30

Dump Hole

0.0

21.3

21.3

0.20

AT22D-31

Dump Hole

0.0

16.8

16.8

0.61

AT22D-33

Dump Hole

0.0

15.2

15.2

0.78

AT22D-34

Dump Hole

0.0

12.2

12.2

0.54

AT22D-43

Dump Hole

3.0

10.7

7.6

0.28

AT22D-45

Dump Hole

10.7

13.7

3.0

0.25

AT22NS-22

Dump/Pre-Collar

6.1

30.5

24.4

0.47

AT22NS-26

Dump/Pre-Collar

0.0

4.6

4.6

0.47

AT22NS-28

Dump/Pre-Collar

0.0

1.5

1.5

0.26

Table 3: Full list of eight expansion and 24 mine dump holes released today

.

Detailed Discussion

Based on our recent drilling the AMFZ's eastern contact with massive dolomite is a northerly

trending, curvilinear plane dipping 75

o

to 85

o

west. This major structural boundary defines the

eastern limit of the much broader mineralized fault zone that incorporates multiple sub-parallel

strands exhibiting vertical displacements ranging up to

75m

across individual faults (see Figures 2

and 3). Both normal and reverse displacements are noted. Most of the gold mineralization at

Atlanta

is hosted within a densely silicified breccia zone that developed along an unconformable contact

separating a basal carbonate sequence of Paleozoic-age limestone and dolomite from an overlying

Tertiary-age, caldera-related volcanic package consisting of felsic to intermediate composition tuff,

volcaniclastics, and epiclastic sediments. This major contact dips 20

o

to 30

o

northwestward and

generally ranges in thickness from

10m

to

40m

, although mineralization does extend downward into

decalcified dolomite (Figure 2) and upward into the volcanic sequence (Figure 3) in places

throughout the deposit. Residual sulfides containing gold are occasionally encountered, but gold

mineralization for the most part is strongly oxidized down to depths of

350m

. Sulfides do occur in

strongly altered volcaniclastics and sediments overlying the mineralized silica breccia zone, but

pyritic rock does not generally host gold values greater than 0.1 g/t and appears to be an early

stage hydrothermal event that was over-printed by an oxide-dominant gold stage. High-angle,

northerly and easterly-trending faults cutting up through both rock sequences served as "feeder

structures" for ascending epithermal fluids and channeled gold-bearing solutions into the very porous

and receptive silica breccia zone. Higher gold grades tend to be concentrated around the

intersections of these high-angle faults with the low-angle silica breccia zone. The strongly argillized

volcanic sequence overlying the silica breccia served as a effective seal or cap on top of the

hydrothermal system that contained the metalliferous fluid within the breccia zone, thus concentrating

the gold mineralization. Rhyolitic dikes and sills were injected into the deposit along the high-angle

feeder faults and low-angle breccia zone at about the same time as the gold mineralization, and

shallow explosive venting of these intrusions created the distinctive "tuff dikes" that are closely

associated both in space and time with the gold event.

Qualified Person

The scientific and technical information in this news release has been reviewed and approved by

Calvin R. Herron

, P.Geo., who is a Qualified Person as defined by National Instrument 43-101 ("

NI

43-101

").

About Nevada King Gold Corp.

Nevada King

is the third largest mineral claim holder in the

State of Nevada

, behind

Nevada Gold

Mines

(Barrick/Newmont) and

Kinross Gold

. Starting in 2016 Company has staked large project

areas hosting significant historical exploration work along the

Battle Mountain

trend located close to

current or former producing gold mines. These project areas were initially targeted based on their

potential for hosting multi-million-ounce gold deposits and were subsequently staked following a

detailed geological evaluation. District-scale projects in

Nevada King's

portfolio include (1) the 100%

owned Atlanta Mine, located 100km southeast of

Ely

, (2) the Lewis and Horse Mountain-Mill Creek

projects, both located between

Nevada Gold Mines'

large

Phoenix

and Pipeline mines, and (3) the

Iron Point project, located 35km east of

Winnemucca, Nevada

.

The Company is well funded with cash of approximately

$17 million

as of October 2022.

The Atlanta Mine is a historical gold-silver producer with a NI 43-101 compliant pit-constrained

resource of 460,000 oz Au in the measured and indicated category (

11.0M

tonnes at 1.3 g/t) plus an

inferred resource of 142,000 oz Au (

5.3M

tonnes at 0.83 g/t). See the NI 43-101 Technical Report

on Resources titled "Atlanta Property,

Lincoln County, NV

" with an effective date of

October 6,

2020

, and a report date of

December 22, 2020

, as prepared by Gustavson Associates and filed

under the Company's profile on SEDAR (

www.sedar.com

).

NI 43-101 Mineral Resources at the Atlanta Mine

Resource

Category

Tonnes

(000's)

Au Grade

(ppm)

Contained Au Oz

(000's)

Ag Grade

(ppm)

Contained Ag Oz

(000's)

Measured

4,130

1.51

200

14.0

1,860

Indicated

6,910

1.17

260

10.6

2,360

Measured + Indicated

11,000

1.30

460

11.9

4,220

Inferred

5,310

0.83

142

7.3

1,240

Please see the Company's website at

www.nevadaking.ca

.

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.

Cautionary Statements Regarding Forward Looking Information

This news release contains certain "forward-looking information" and "forward-looking statements"

(collectively "forward-looking statements") within the meaning of applicable securities legislation.

All statements, other than statements of historical fact, included herein, without limitation,

statements relating the future operations and activities of

Nevada King

, are forward-looking

statements. Forward-looking statements are frequently, but not always, identified by words such as

"expects", "anticipates", "believes", "intends", "estimates", "potential", "possible", and similar

expressions, or statements that events, conditions, or results "will", "may", "could", or "should"

occur or be achieved. Forward-looking statements in this news release relate to, among other

things, exploration plans and the Company's ability to potentially expand mineral resources and the

impact thereon. There can be no assurance that such statements will prove to be accurate, and

actual results and future events could differ materially from those anticipated in such statements.

Forward-looking statements reflect the beliefs, opinions and projections on the date the statements

are made and are based upon a number of assumptions and estimates that, while considered

reasonable by

Nevada King

, are inherently subject to significant business, economic, competitive,

political and social uncertainties and contingencies. Many factors, both known and unknown, could

cause actual results, performance or achievements to be materially different from the results,

performance or achievements that are or may be expressed or implied by such forward-looking

statements and the parties have made assumptions and estimates based on or related to many of

these factors. Such factors include, without limitation, the ability to complete proposed exploration

work given the global COVID-19 pandemic, the results of exploration, continued availability of

capital, and changes in general economic, market and business conditions. Readers should not

place undue reliance on the forward-looking statements and information contained in this news

release concerning these items.

Nevada King

does not assume any obligation to update the

forward-looking statements of beliefs, opinions, projections, or other factors, should they change,

except as required by applicable securities laws.

SOURCE

Nevada King Gold Corp.

View original content to download multimedia:

http://www.newswire.ca/en/releases/archive/October2022/18/c5562.html

%SEDAR: 00015775E

For further information:

Collin Kettell at [email protected] or (301) 744-8744.

CO: Nevada King Gold Corp.

CNW 07:30e 18-OCT-22