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Rokmaster intersects 6.32 g/t AuEq over 4.25 m and extends the Main Zone 415 m to the southeast on the Revel Ridge Project

Drill Results

Rokmaster intersects 6.32 g/t AuEq over 4.25

m and extends the Main Zone 415 m to the

southeast on the Revel Ridge Project

VANCOUVER, BC

,

Aug. 29, 2022

/CNW/ - Rokmaster Resources Corp. (TSXV: RKR) (OTCQB:

RKMSF) (FSE: 1RR1) ("Rokmaster" or "the Company") is pleased to announce the complete assay

results of the spring 2022 underground diamond drill program at the Revel Ridge Project ("Revel

Ridge" or "the Project").

Spring Underground Drill Program and Mineral Resource Estimate - Longitudinal Section (CNW

Group/Rokmaster Resources Corp.)

The drill program totaled 3,246 metres cored in ten drillholes, all of which successfully intersected

the Revel Ridge Main Zone ("RRMZ"). The drill program was designed to test the limits of, and

extend, the volume of the Revel Ridge Main Zone and other zones, as defined by the 2021 NI 43-

101 Mineral Resource Estimate (

Fig.1

):

Measured & Indicated (M&I): 1.36 million gold equivalent ("AuEq") ounces contained within 6.73

million tonnes with an average grade of 6.27 g/t AuEq.*

Inferred (Inf): 1.22 million AuEq ounces contained within 6.00 million tonnes at an average grade

of 6.33 g/t AuEq.*

A surface drill program is currently testing the RRMZ and Yellowjacket Zones to the northwest,

down-dip from certain 2021 surface drillholes. The program will also further test the southeastern

portion of the RRMZ, including the Zinc Creek Showing which occurs along strike approximately

950

m

to the southeast of historical drilling and is highly characteristic of the RRMZ (

Figure 1 – Long section with Resource + RRMZ plane

).

Drillhole RR22-94 tested an area of the RRMZ prospective for structurally enhanced mineralization

and achieved a strong intersection of 6.32 g/t AuEq over

4.25 m

(

Fig. 2 – Cross Section

). This

drillhole also intersected

12 m

of well-developed sphalerite mineralization hosted in black silicified

siltstone adjacent to the RRMZ which has similarities to the "28 Zone" encountered in drillhole RR21-

28 (4.53 g/t AuEq over

26.20 m

; see

March 29, 2021

News Release). Notably, RR22-94 and RR21-

28 are separated by a distance of 300 metres. Drillhole RR22-95 intersected 5.77 g/t AuEq over

1.95 m

in the RRMZ ~122 m to the southeast of RR22-94.

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR22-88

268.70

269.42

0.72

1.71

1.31

12.00

0.42

0.32

RRMZ

RR22-88

300.20

300.75

0.55

1.20

1.12

5.00

0.05

0.01

RRFZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR22-89

481.50

482.10

0.60

3.28

3.24

0.50

0.04

0.06

RRMZ

RR22-89

487.40

487.88

0.48

1.87

0.01

8.00

0.51

4.50

RRMZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR22-90

304.60

305.90

1.30

3.02

2.48

8.95

0.35

0.90

RRMZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR22-91

459.70

460.50

0.80

0.44

0.28

6.00

0.19

0.07

RRMZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR22-92

338.30

339.45

1.15

2.45

2.39

1.87

0.02

0.09

RRMZ

including

338.95

339.45

0.50

5.40

5.29

3.00

0.03

0.19

RRMZ

RR22-92

393.75

394.25

0.50

2.17

1.93

4.00

0.29

0.25

RRFZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR22-93

386.68

388.10

1.42

2.08

0.18

51.54

1.29

2.37

RRMZ

including

386.68

387.20

0.52

5.39

0.27

139.00

3.43

6.41

RRMZ

RR22-93

403.90

405.45

1.55

2.20

1.20

51.68

0.78

0.29

RRFZ

including

404.65

405.45

0.80

3.43

1.73

87.00

1.31

0.56

RRFZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR22-94

296.90

319.60

22.70

1.68

1.01

9.92

0.47

1.12

RR28Z

including

315.35

319.60

4.25

6.32

4.98

28.17

1.34

1.52

RRMZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR21-38EXT

461.20

461.90

0.70

4.89

1.96

44.00

1.69

5.13

RRMZ

RR21-38EXT

486.50

487.40

0.90

2.52

2.28

13.00

0.14

0.10

RRFZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR21-39EXT

564.10

564.90

0.80

8.38

6.52

20.00

0.59

4.02

RRMZ

DDH

From

(m)

To (m)

Length

(m)

AuEq

g/t

Au g/t

Ag g/t

Pb %

Zn %

Zone

RR22-95

349.15

351.10

1.95

5.77

4.88

10.00

0.30

1.90

RRMZ

Footnote 1. Reported widths of mineralization are drill hole intervals or core lengths recovered. Insufficient data exists to permit the calculation of true width of the reported

mineralized intervals.

Footnote 2. Mineralized Zone abbreviations: RRMZ: Revel Ridge Main Zone,

Footnote 3. AuEq calculations use: Metal prices of Au US$1,625/oz, Ag US$22/oz, Pb US$0.95/lb, Zn US$1.20/lb; RRMZ process recoveries of Au 92%, Ag 88%, Pb 80%, Zn

72%; RRMZ AuEq = Au g/t + (Ag g/t x 0.012) + (Pb% x 0.347) + (Zn% x 0.353);

Six drillholes broadly tested the RRMZ to the southeast from the historic limit of the

830 m

level

underground development. RR22-88 to RR22-93 have an average spacing of

167 m

along the Main

Zone plane and all successfully intersected the Main Deformation Zone structure over metre-scale

intervals with variable degrees of banded massive sulphide mineralization. The distance between

historical drillhole 12-16 and RR22-89 is approximately 415 metres which is a significant expansion

of the RRMZ to the southeast (

Figure 1

). In these drillholes the RRMZ was dominantly hosted by

calcareous phyllites. This incompetent rock unit typically develops only weak dilatant sites within the

RRMZ, and as a consequence, wide mineralized intersections were not obtained. Technical data

suggests that this incompetent rock unit is thinning significantly to the southeast and that a return to

more competent host rocks to the RRMZ may lead to stronger mineralized intervals.

An additional objective of the program was to extend 2021 drillholes RR21-38 and RR21-39. Later

drilling data in the area adjacent to these drillholes indicated that they have ended prior to

intersecting the RRMZ. In this area, and below

460 m

elevation the RRMZ steepens in dip which

produced an apparent decrease in the grade and continuity of the RRMZ (

Figure 1

). The company is

pleased to report that after extending RR21-38 by

38.0 m

and RR21-39 by

31.1 m

, both drillholes

successfully encountered RRMZ massive sulphide mineralization.

In July of 2022, at the beginning of the current surface drill program, several channel samples were

cut using a diamond saw from a newly discovered Main Zone surface exposure approximately 125

metres southeast of the southernmost historical drillholes 91-73 and 91-74 (

Figure 1

). Strong

sulphide mineralization hosted in sericite-altered quartzite is exposed in outcrop and two separate

channel samples with a spacing of approximately 10 metres returned assay results of 6.00 g/t AuEq

over

2.0 m

and 2.74 g/t AuEq over

4.0 m

. The strong grade and width relationships, from these

surface channel samples, conclusively demonstrates that significant gold mineralization in the RRMZ

continues to the southeast, past historical surface diamond drillholes.

John Mirko

, President and CEO of Rokmaster stated:

"The spring 2022 underground drill program at Revel Ridge successfully achieved the goals of

testing structurally favorable targets, extending the Main Deformation Zone structure to the

southeast, and proving the remarkable continuity of the RRMZ. Drillholes RR22-94 and RR22-95

highlight that there exists local structurally enhanced zones of mineralization with significant width

within the currently defined Main Deformation Zone. Rokmaster's previous and current vigorous

resource expansion drilling phases at Revel Ridge have dramatically grown the size of the RRMZ,

within which there is the opportunity to locate additional structurally enhanced zones. Historical

drillholes along with channel sampling on surface indicates that the southeastern extension of the

RRMZ is an exciting target that the team will continue testing. The successful RRMZ intersections

achieved by extending drillholes RR21-38 and RR21-39 solidify that the RRMZ is an impressively

consistent and extensive zone of high-grade polymetallic mineralization.

These results, along with the ongoing summer 2022 drill program, will be compiled with historical

drilling for a resource update which is planned for 2023."

Quality Assurance/Quality Control.

Dr.

Jim Oliver

, P. Geo. supervised all aspects of the drilling

and sampling undertaken in the 2021 and 2022 underground and surface diamond drill programs. All

drill core assay samples have been collected from ½ NQ core, sawn with a diamond saw with the

sample intervals marked by technical personnel. A full QAQC program using blanks, standards and

duplicates was utilized to monitor analytical accuracy and precision. QAQC samples are submitted

approximately at every 20th sample, or a minimum of 5% of the total sample stream. Appropriate

standards are used to provide quality control information on high grade and medium to low grade

samples. A limestone blank is inserted after select samples that have macroscale characteristics of

higher-grade mineralization. Duplicate samples are repeat analysis of designated primary sample

pulps. The samples were sealed on site and shipped to MSALABS in

Langley, British Columbia

.

MSALABS is an ISO 17025 (Testing and Calibration Laboratory) and an ISO 9001 (Quality

Management System) Certified Laboratory. Drill core samples were crushed to 2 mm and a 500-

gram sub sample was pulverized with 85% of the sample passing 75 microns. The sub-sample was

analysed using a combination of MSALABS FAS211 for Au and ICP–240 (4 acid digestion) for silver,

base metals and other trace elements. FAS211 for gold is an ore grade fire assay of a 50 g pulp

with an AAS finish with a detection range between 0.01 and 100 ppm). ICP-240 utilizes four acid

digestion and provides ore grade analytical data on silver, base metals and 26 other elements.

The technical information in this news release has been prepared in accordance with Canadian

regulatory requirements as set out in National Instrument 43-101 and reviewed and approved by

Eric

Titley P.Geo

., who is independent of Rokmaster and who acts as Rokmaster's Qualified Person.

website:

www.rokmaster.com

*(Technical Report and Updated Mineral Resource Estimate of the Revel Ridge Polymetallic

Property Revelstoke Mining Division,

British Columbia, Canada

,

William Stone

, Ph.D., P.Geo.

Fred

Brown

, P.Geo.

Jarita Barry

, P.Geo.

David Burga

, P.Geo.

Eugene Puritch

, P.Eng., FEC, CET Stacy

Freudigmann, P.Eng. F.Aus.IMM. P&E Mining Consultants Inc. Report 411 Effective Date:

November 15, 2021

Signing Date:

January 17, 2022

filed on SEDAR.)

On Behalf of the Board of Directors of

Rokmaster Resources Corp.

John Mirko

,

President & Chief Executive Officer.

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term in defined in the

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

press release.

About Rokmaster

Rokmaster controls a portfolio of three significant exploration and development projects all of which

are located in southern

British Columbia

in regions of excellent infrastructure. The three projects

include:

1

.

Revel Ridge.

Rokmaster is currently conducting an underground drill program at the Revel

Ridge Project located in southeastern

British Columbia

35 km's north of the

City of Revelstoke

.

Revel Ridge is host to a high-grade gold and polymetallic orogenic sulphide deposit which has

been the subject of a PEA Technical Report dated

December 8, 2020

and a Technical Report

of an Updated Mineral Resource Estimate on the Revel Ridge Property, dated

January 17,

2022

.

2

.

Big Copper.

Rokmaster controls the Big Copper Property in the

Kimberley

area of southern

British Columbia

. Big Copper is a high-grade copper-silver occurrence hosted in mid-Proterozoic

rocks. Copper-silver mineralization has been traced for 4.5 km along strike and is exposed in a

series of adits and trenches over approximately

500 m

of vertical relief. Big Copper likely

belongs to a class of stratabound replacement copper-silver deposits hosted within mid –

Proterozoic quartzitic sediments. The style and stratigraphic setting of mineralization at Big

Copper may be analogous to similar stratabound silver-copper deposits in

NW Montana

, e.g.,

the Troy Mine (a significant past producer of copper and silver) and

Hecla's

Montanore pre-

development project, with, 112 million tonnes Inferred at 54.8 g/t Ag and 0.7% Cu*. (

Hecla

,

2020 Annual Report, Pg. 119.

www.hecla-mining.com

).

1

3

.

Duncan Lake Zinc.

Duncan is a carbonate hosted silver-lead-zinc deposit located near Duncan

Lake in southern

British Columbia

. The deposit is hosted within a Cambrian age

Badshot

Limestone which also hosts Zn-Pb-Ag

mineralization

at

Teck's

recently producing Pend

Oreille

Mine as well as past producers including the Blue Bell Mine, Reeves

MacDonald

Mine,

JerseyEmerald

and

HB

mines.

Mineralization

at Duncan Lake forms in the crest and limbs of the

regional scale Duncan Lake anticline, where strong zinc-lead +/- silver

mineralization

has been

traced by surface and underground drilling for approximately 2,500

m

. At Duncan Lake,

Rokmaster

will be targeting > 30

Mt

of >10% Zn+Pb+Ag. Historical background and a

geological synthesis of the Duncan Lake deposit is provided in a NI 43-101 report by

Lane, B.,

2018: Technical Report on the Duncan Lake Project.

Footnote (1).

The qualified person has been unable to verify this inferred resource.

CAUTIONARY NOTE REGARDING FORWARD LOOKING STATEMENTS: This news release may

contain forward-looking information within the meaning of applicable securities laws ("forward-

looking statements"). Forward-looking statements are statements that are not historical facts and

are generally, but not always, identified by the words "expects," "plans," "anticipates," "believes,"

"intends," "estimates," 'projects," "potential" and similar expressions, or that events or conditions

"will," "would," "may," "could" or "should" occur. These forward-looking statements are subject to a

variety of risks and uncertainties which could cause actual events or results to differ materially from

those reflected in the forward-looking statements, including, without limitation: risks related to

fluctuations in metal prices; uncertainties related to raising sufficient financing to fund the planned

work in a timely manner and on acceptable terms; changes in planned work resulting from weather,

logistical, technical or other factors; the possibility that results of work will not fulfill expectations and

realize the perceived potential of the Company's properties; risk of accidents, equipment

breakdowns and labour disputes or other unanticipated difficulties or interruptions; the possibility of

cost overruns or unanticipated expenses in the work program; the risk of environmental

contamination or damage resulting from Rokmaster's operations and other risks and uncertainties.

Any forward-looking statement speaks only as of the date it is made and, except as may be

required by applicable securities laws, the Company disclaims any intent or obligation to update any

forward-looking statement, whether as a result of new information, future vents or results or

otherwise.

SOURCE

Rokmaster Resources Corp.

View original content to download multimedia:

http://www.newswire.ca/en/releases/archive/August2022/29/c6694.html

%SEDAR: 00031923E

For further information:

Please contact Mr. John Mirko, CEO of Rokmaster Resources,

[email protected], Ph. 1-604-290-4647; For shareholder information, please contact: Mike

Kordysz, [email protected], Ph. +1 (604) 319-3171

CO: Rokmaster Resources Corp.

CNW 05:00e 29-AUG-22