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Copper Road Resources Intersects 50 Metres of 1.00% Cu Eq at the Richards Breccia and 95 Metres of 0.51% Cu Eq at the Jogran Porphyry, JR Zone,

Drill Results

Copper Road Resources Intersects 50

Metres of 1.00% Cu Eq at the Richards

Breccia and 95 Metres of 0.51% Cu Eq

at the Jogran Porphyry, JR Zone,

Batchewana Bay, Ontario

Your publication dateand timewillappear

here.

| Source: Copper Road Resources

Inc.

Highlights 2023 JR Zone Drill

Program

Richards Breccia

R23-01: 38.63 m @ 1.17%

Cu Eq (76.37 to 115 m)

R23-04: 50.17 m @ 1.00%

Cu Eq (79 to 129.17 m)

Jogran Porphyry

JR-23-01: 342 m @ 0.23%

Cu Eq (8 to 350 m)

JR-23-02: 197 m @ 0.35%

Cu Eq (4 to 201 m)

including 21 m @ 1.04% Cu

Eq (5 to 26 m)

within 95 m @ 0.51% Cu Eq

(4 to 99 m)

TORONTO, Nov. 30, 2023 (GLOBE NEWSWIRE) -- Copper Road Resources

(TSXV: CRD) (“Copper Road” or “the Company”) is pleased toannounce2023

diamond drill results from its 1,250-metredrill program completed in the JR

Zone at the 24,000-hectareCopper Road Project, Batchewana Bay, Ontario.

The JR Zone is located approximately 8 kmfrom the Tribag Zone whichthe

Companydrilled in 2022. The objectivewas toconfirmthe lengthyhistorical

intersections of Copper and Molybdenum mineralization within the Jogran

Porphyry and to demonstrate additional high-grade Copper mineralization

at depth in the Richards Breccia.

Copper Road President and CEO John Timmons comments: “The results

from our initial drill program have established the presence of lengthy near-

surface intersections of porphyry-hosted Copper/Molybdenum

mineralization with shorter intersections of higher-grade Copper/Gold

breccia-hosted mineralization. The Jogran Porphyry and Richards Breccia

targets are approximately 1 km apart and form part of a wider array of alkalic

porphyry and breccia targets in the JR Zone area, similar in areal scale to the

established alkalic porphyry districts or “clusters” in British Columbia and in

Australia.

“The Richards and Jogran targets are two of nineteen targets in the greater

JR Zone area based on the ongoing compilation of historical and current

exploration data. The Company believes the JR Zone has the potential to

deliver multiple larger porphyry and breccia-hosted discoveries.”

Figure 1: JR Zone Long Section

Table 1: Richards Breccia Select Intercepts

Drillhole

Drill Intercept (metres) Grade

From To Length Cu (%) Ag (g/T) Mo (%) Au (g/t) Cu Eq

(%)

R2301 76.37 115.00 38.63 1.06 3.55 0.002 0.07 1.17

Including 98.00 108.00 10.00 2.19 7.96 0.002 0.11 2.35

R2304 80.00 120.00 40.00 0.99 4.58 0.002 0.09 1.11

Including 79.00 129.17 50.17 0.88 4.56 0.002 0.09 1.00

Including 81.00 89.00 8.00 2.09 16.00 0.004 0.21 2.42

Including 117.00 120.00 3.00 2.41 7.20 0.001 0.23 2.66

R2305 72.00 85.00 13.00 0.31 1.72 0.000 0.03 0.35

Including 73.83 75.00 1.17 2.03 11.17 0.001 0.18 2.27

Assumptions used in USD for the copper equivalent calculation are metal prices of

$3.60/lb Copper, $22/oz Silver, $50/kg Molybdenum, $1900/kg Gold and recovery is

assumed to be 100% as no metallurgical test data is available. The following equation

was used to calculate copper equivalence: CuEq = Copper (%) + (Silver (g/t) x 0.01) +

(Molybdenum (%) x 6.30) + (Gold (g/t) x 0.77)

Table 2: Jogran Porphyry Select Intercepts

1

1

Drillhole

Drill Intercept (metres) Grade

From To Length Cu (%) Ag (g/T) Mo (%) Cu Eq

(%)

J2301 8.00 350.00 342.00 0.13 1.18 0.015 0.23

Including 39.00 52.00 13.00 0.16 2.26 0.027 0.35

Including 69.00 98.00 29.00 0.10 1.60 0.040 0.37

Including 188.00 284.00 96.00 0.18 1.23 0.015 0.28

Including 198.00 212.00 14.00 0.20 1.12 0.053 0.55

Including 234.00 245.00 11.00 0.20 1.22 0.004 0.24

Including 256.00 279.00 23.00 0.25 1.55 0.009 0.33

Including 318.78 350.00 31.22 0.17 0.88 0.010 0.24

Including 318.78 335.00 16.22 0.21 1.17 0.016 0.32

J2302 4.00 201.00 197.00 0.17 1.62 0.025 0.35

Including 4.00 99.00 95.00 0.20 1.97 0.048 0.51

Including 5.00 26.00 21.00 0.27 2.15 0.120 1.04

Assumptions used in USD for the copper equivalent calculation are metal

prices of $3.60/lb Copper, $22/oz Silver, $50/kg Molybdenum, $1900/kg Gold

and recovery is assumed to be 100% as no metallurgical test data is available.

The following equation was used to calculate copper equivalence: CuEq =

Copper (%) + (Silver (g/t) x 0.01) + (Molybdenum (%) x 6.30) + (Gold (g/t) x

0.77)

Jogran Porphyry

Two (2) drillholes were completed at Jogran Porphyry to test the extent and

continuity of the mineralization encountered in previous historical

exploration by Jogran Mines and Phelps-Dodge in the early 1960s. The

Jogran Porphyry is a quartz monzonite porphyry intrusion with a distinct

alteration and mineralization style consistent with alkalic porphyry copper-

molybdenum mineralization. Drilling has successfully confirmed the

continuity of the copper and molybdenum mineralization in the porphyry

over long intervals, beyond what was previously known laterally and at

depth, and that the mineralization also extends to the southwest into the

mafic volcanics where it is associated with localized and discrete potassic

alteration (magnetite and biotite) occurring as haloes adjacent to quartz-

carbonate veinlets and as local patches in the mafic volcanics.

Figure 2: Jogran Porphyry: Cross-Sections Showing Drillhole Locations

1

1

J2301: Drilled to test the continuity of the porphyry mineralization beneath

historical hole JDH-16 (165 m @ 0.43% Cu Eq). This hole intersected an

extensive zone of copper mineralization hosted by the porphyry (0.23% Cu

Eq over 342 metres from 8 to 350 metres, including an interval of 0.37% Cu

Eq over 29 metres from 69 to 98 metres). Historical drilling had traced the

mineralized porphyry to a maximum vertical depth of 180-220 metres below

surface. The current drilling has extended the mineralized porphyry to 320

metres below surface and is still open at depth. The broad intersection at

JR-23-01 confirms the presence of near-surface copper mineralization with

strong credit mineralization (Mo, Ag, Au) that increases proportionately with

the higher copper grades. Copper mineralization extends into the mafic

volcanics and appears as consistently mineralized as in the porphyry

intrusion, thereby suggesting the presence of a larger intrusive system

southwest of the Jogran porphyry (i.e. towards the J2 “Roof Zone” Cu-in-MMI

and magnetic high anomaly).

J2302: Drilled to test the continuity of the porphyry mineralization below

historical hole JDH-13 (147 m @ 0.53% Cu Eq). This hole intersected a broad

zone of altered quartz monzonite porphyry containing consistent copper

mineralization with associated strong molybdenum grades throughout the

entire hole (0.35% Cu Eq over 197 metres from 4 to 201 meters including

higher-grade intervals of 0.51% Cu Eq over 95 metres and 1.04% Cu over 21

metres). Copper and molybdenum mineralization also extends into the

altered mafic volcanics, similar to that seen in J2301, again confirming the

potential of higher-grade copper mineralization to the southwest

Richards Breccia

Richards Breccia is an altered polymictic and clast supported breccia. Clasts

consist of altered volcanics, silicified cherty fragments and felsic intrusives.

The presence of felsic intrusive clasts in the breccia indicates an

emplacement related to an intrusive source at depth. Four (4) holes were

drilled to test the continuity of the mineralization originally drill-tested by

Aurogin Resources in 1997 and 1998, with an additional hole testing an area

of high Gradient chargeability located approximately 200 metres to the

west-northwest of Richards. Drilling successfully extended the breccia 50 to

60 metres vertically below the known mineralization, establishing the

vertical extent of mineralization to 130 meters from surface. The breccia is

still open at depth and is technically open to the northeast for at least a

limited strike extent.

Figure 3: Richards Breccia Drillhole Location Map Showing Gradient IP

Anomaly

Figure 4: Richards Breccia: Section along R2301

Figure 5: Richards Breccia: Section along R2304

R2301: Drilled to test the vertical extent of the mineralized breccia

encountered by historical drillholes AR98-07, AR97-24, and AR97-25. This

hole returned grades of 1.17% Cu Eq over 38.63 metres from 76.37 to 115

metres including a higher-grade interval of 2.35% Cu Eq over 10 metres

from 98 to 108 metres. True widths are estimated to be 50% of the drill

widths reported above. This hole extended the mineralization to 50 metres

vertically below AR97-25.

R2302: This hole was designed to test the western strike extent of the

breccia but may have been fault-displaced or dyked out by a mapped

diabase. The hole did not return any significant mineralization.

R2303: This drillhole tested a historical gradient IP anomaly to the southeast

of the breccia. The hole appears to have drilled down a moderately east-

dipping fault that is sub-parallel to the trace of the hole, perhaps explaining

the weak to moderate IP anomaly, but did not intersect any significant

mineralization.

The Company continues to analyse the structural framework of the Richards

Breccia regarding the negative results of R-23-02 and R-23-03, but it is

initially interpreted that the breccia has been fault-displaced to both the

east and the west.

R2304: Drilled to test the northeastern extent of mineralized breccia below

AR98-07. It returned a composite grade of 1.00% Cu Eq over 50.17 metres

from 79 to 129.17 metres. Within this broad zone of mineralization are higher

grade zones of copper enrichment containing 1.11% Cu Eq over 40 metres

and 2.42% Cu Eq over 8 metres. This hole has confirmed extension of

mineralization to 60 metres vertically below AD98-07.

R2305: This hole tested the southeastern edge of a high Gradient IP anomaly

located approximately 100 m to the northwest of the mineralized Richards

Breccia. It intersected dominantly chlorite-carbonate-pyrite altered mafic

volcanics with a few narrow diabase dikes. Notably, there are scattered

patches of sulphide mineralization and associated alteration through out

the length of the hole, with discontinuous anomalous copper values greater

than 0.1% Cu from 52.0 to 148.0 metres (the hole was not continuously

sampled). The zones are characterized by pyrite mineralization in hairline

fractures and as disseminations and, to a lesser extent, quartz-calcite

veinlets containing chalcopyrite+pyrite±bornite±pyrrhotite. Best results from

this hole returned 2.27% Cu Eq over 1.17 metres within a 13-metre-wide

interval of 0.35% Cu Eq from 72 to 85 metres. These results indicate

possible proximity to a mineralized porphyry intrusion or breccia pipe that

may be centred just to the north and/or just below the drill hole.

Exploration Outlook

The Jogran Porphyry and Richards Breccia targets are approximately 1 km

apart and form part of a wider array of alkalic porphyry and breccia targets

in the JR Zone area, similar in areal scale to the established alkalic porphyry

districts or “clusters” in British Columbia and in Australia (see Figure 8

below).

Currently the established porphyry and breccia targets within the JR area

are a combination of MMI soil, stream silt, and lake sediment geochemical

anomalies with local magnetic highs that may indicate intrusive centres

within a larger area of elevated magnetics that is interpreted to indicate a

broad area of propylitic alteration. Within this broad halo, numerous

historical surface showings are reported, and virtually every historical drill

hole has reported at least locally anomalous Copper-Molybdenum

mineralization and related alteration (many not assayed).

The Company is currently planning a large (3 x 4 kilometre), semi-3D, deep-

penetrating IP survey over the main JR area to further advance the targets

as it has only had limited patches of historical IP surveying (mostly

Gradient). This will be followed up with additional drill testing of coincident

geochemical and geophysical anomalies.

Figure 6: Alkalic Porphyry Deposit Clusters Comparison

Sources: the maps above are original and created from publicly available

information and technical reports

Marketing Update

The Company also announces that it has finalized the following sponsorship

arrangements with the Rocks and Stocks News YouTube channel and news

website (“Rocks and Stocks”) and Ahead of the Herd (“AOTH”) newsletter.

Rocks and Stocks is a private entity owned and operated by Allan Laboucan.

Rocks and Stocks is based in Mexico where it operates an online portal for

news related to mining stocks and the precious metals industry. The

Company had paid sponsorship fees to Rocks and Stocks in the amount of

$15,000 on May 4 , 2023, for the period commencing on May 4 , 2023 and

ending on November 4 , 2023. In exchange for such sponsorship fees, Rocks

and Stocks provided coverage of video interviews with the Company’s

management on its various online platforms. No equity compensation was

paid to Rocks and Stocks in connection with the sponsorship. Rocks and

Stocks and the Company are unrelated and unaffiliated entities, and the

Company is not aware of any interest, directly or indirectly, of Rocks and

Stocks or its principal in the Company or its securities.

The Company had paid sponsorship fees to AOTH in the amount of $12,000

over a 6-month period commencing on May 5 , 2023, paid monthly at

$2,000, and ending on November 15th, 2023. AOTH is based in Prince

George, BC, Canada, owned and operated by Rick Mills. AOTH provides

written commentaries of public companies based on public information and

approved by Copper Road management. In exchange for such sponsorship

fees, AOTH provided written interviews with the Company’s management

discussing publicly available information regarding the Company’s project.

No equity compensation was paid to AOTH in connection with the

sponsorship. AOTH and the Company are unrelated and unaffiliated entities,

and the Company is not aware of any interest, directly or indirectly, of AOTH

or its principal in the Company or its securities.

The Company also announces an ongoing contract with Grove Corporate

Services (“Grove”) to assist in developing presentation materials, press

releases, content for social media posts relating to broad market statements

relating to the copper mining industry, and incoming investor relations calls.

Grove, owned by Stephen Coates, is based in Toronto, Canada, providing

incoming investor relations services and social media content creation and

postings among other services. The contract commenced on March 31, 2023

and is ongoing at a monthly rate of $4,000. No equity compensation was

paid to Grove in connection with the sponsorship. Grove and the Company

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