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Manning Ventures hires driller for upcoming drill program at the Copper Hill Project, Nevada, USA.

Exploration Programs

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Manning Ventures Inc.

Suite 303, 750 West Pender Street

Vancouver, BC V6C 2T7

MANNING VENTURES HIRES DRILLER FOR UPCOMING DRILL

PROGRAM AT THE COPPER HILL PROJECT, NEVADA, USA

Vancouver, British Columbia, November 14, 2024 – Manning Ventures Inc. (the “Company”

or “Manning”) (CSE: MANN; Frankfurt: 1H5; US:MANVF) is pleased to announce that it has

contracted the driller for the upcoming exploration program at the Copper Hill Project, Nevada,

USA.

Boart Longyear of Salt Lake City, Utah, will provide the drill rig, all relevant equipment and crew

for up to nine Reverse Circulation (“RC”) drill holes totalling approximately 2,500 meters

anticipated for the initial phase one drill program.

Drilling will test for skarn mineralization on the contact between the limestone and the intrusive

for the Northern and the Southern Zones. The two zones outline target areas that returned

significant copper values (0.5 to > 1.0% copper) in intense skarn alteration. The Copper Hill

Project is comprised of 108 unpatented lode mining claims that cover 2,215 acres (896.3 Ha).

The Company is advancing road building activities to the established drill pad locations and will

announce mobilization dates shortly.

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Image 1: Phase one planned drill sites, Copper Hill Project, Nevada, USA

Recent geological mapping has identified four primary rock units within Triassic Luning limestone

which was intruded by a Jurassic igneous complex which was then overlain by Neogene age

Volcanic rocks and Quarternary aged unconsolidated gravels. Comparison of the geophysical

interpretations and surface geochemical sampling results announced previously with the current

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geological mapping indicates a series of west-northwest and northwest trending structural fabrics

providing the primary controls to copper mineralization at Copper Hill. The northwest faults and

associated magnetic and gravity linears represent structural breaks and pathways for mineralizing

fluids as witnessed by the elevated copper values returned within these zones.

Skarn-type alteration and mineralization is found throughout the Mesozoic limestone and igneous

rocks. It occurs in two prominent geologic settings on the copper hill property see figure 1.

• Limestone-granodiorite contact

• Along northwest and west-northwest trending faults and fault zones; dominantly in the

Jurassic igneous rocks with less intense, more distal-type skarn-type alteration in the

Triassic Luning Limestone.

Mineralization Controls

The mapping and compilation of all exploration data at Copper Hill outlines an untested, highly

prospective, copper/gold bearing skarn target. Potential may exist for a porphyry type copper

deposit to be found deep beneath Copper Mountain or beneath the covered southeast intrusive.

Additionally, porphyry-related veins and local chloritic and sericitic alteration is found along these

northwest trends.

Two exploration corridors termed the Northern Zone and the Southern Zone outline areas with

over 1500 meters (>5,000 feet) of strike length which host significant, intense skarn alteration and

elevated copper values (0.5 to >1.0% copper).

The most significant features on the west-northwest trends are:

• Northern Zone

1. Correlates with northern copper in soils anomaly

2. Aligns with garnetite, copper-bearing zones

3. Aligns with larger dikes of diorite

• Southern Zone

1. Adjacent to deepest historic mineralization and proximal to historic shallow, near surface

mines (limestone host in historic mine area is likely very thin and gets wider and thicker

moving to southeast).

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2. Aligns with gravity trend indicating Limestone/intrusive contact connecting southeast

to “SE” buried intrusive.

3. Northern end of southern zone associated with high-grade surface sampling and historic

mining of garnetite and massive magnetite skarn zones.

4. Correlates with southern high copper in soils anomaly.

Image 2: Location of Copper Hill, Walker Lane Trend, Nevada, USA

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About the Copper Hill Project

Located within the prolific Walker Lane trend in southern Nevada, Copper Hill is situated one of

the premier jurisdictions for precious metals mining in the world. Historic endowment within

Walker Lane includes 50Moz Au, 700Moz Ag, and 4Mt Cu. Copper Hill hosts copper-gold-

molybdenum mineralization in both porphyry and skarn styled deposits in Mineral County,

Nevada.

The Project is centered on a Jurassic Age quartz monzonite porphyry intruding Triassic age Luning

Limestone. The claims are located 33 miles east of the Yerington Copper District which hosts the

Yerington Copper Mine (Anaconda 1952-1978), Ann Mason Deposit, Bear Deposit, MacArthur

Deposit, and the Pumpkin Hollow Mine.

Historically at Copper Hill, reported high-grade copper was mined from underground shafts from

skarn and porphyry-copper styled mineralization at the Copper Mountain Mine. Between 1914

to 1926 mining from the “Copper Mountain Mine” produced an estimated 1,000,000 pounds of

copper from shallow underground workings. Historic reporting from the period of production

describes ore zones of contact skarn- type and porphyry-type mineralization with shipping grades

ranging from 3.5 to 11.0% copper*.

The Copper Hill mineralizing system forms a topographic high surrounded and partially covered

by younger volcanic rocks. Mineralization identified at Copper Hill are bornite, chalcocite,

chalcopyrite, chrysocolla, copper-native, covellite, cuprite, gold, malachite, molybdenite, silver,

sphalerite (rare), and tetrahedrite.

The Copper Mountain area was explored between 1959 to 1979 by Idaho Minning Corp. and

Walker-Martel who conducted ground geophysics, underground mapping, prospecting and

reported 6000 feet of Rotary drilling. Since that time ground magnetics were conducted in 2007.

Rock sampling collected at this time returned values from select samples of 7.2% and 12.7%

copper and 1.06 g/t gold and 1.19 g/t gold respectively.

*Historic Mining information was summarized from an “Unpublished Report on the Carson Sink

Area, Nevada by F.C. Schrader, U.S. Geological Survey (Field work 1911-1920) 1947”. Manning

Ventures cautions investors that the historic exploration and production information is believed

to be accurate but has not been verified by a qualified person.

Warren Robb P.Geo., is the designated Qualified Person as defined by National Instrument 43-101

and is responsible for the technical information contained in this release.

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About Manning

Manning Ventures is a mineral exploration and development company focused metals and

materials critical to the growing Energy Metals space. Manning’s project portfolio is focused on

Copper in Nevada, Lithium/Copper in Ontario and Quebec, and multiple Iron Ore projects in

Quebec.

For further information contact:

Manning Ventures Inc.

Alex Klenman - CEO

Email: [email protected]

Telephone: (604) 681-0084

www.manning-ventures.com

FORWARD LOOKING STATEMENTS:

The Canadian Securities Exchange does not accept responsibility for the adequacy or accuracy of

this news release.

Certain statements in this press release may contain forward-looking information (within the

meaning of Canadian securities legislation), including, without limitation, the Company’s

payment of the Exercise Price during the Option Term, the granting of the net smelter return

royalty to the Optionor, and the Company’s payment of the annual minimum payments to the

Optionor. These statements address future events and conditions and, as such, involve known and

unknown risks, uncertainties, and other factors, which may cause the actual results, performance,

or achievements to be materially different from any future results, performance, or achievements

expressed or implied by the statements. Forward-looking statements speak only as of the date those

statements are made. Although the Company believes the expectations expressed in such forward-

looking statements are based on reasonable assumptions, such statements are not guarantees of

future performance and actual results may differ materially from those in the forward-looking

statements. Factors that could cause the actual results to differ materially from those in forward-

looking statements include regulatory actions, market prices, and continued availability of capital

and financing, and general economic, market or business conditions. Investors are cautioned that

any such statements are not guarantees of future performance and actual results or developments

may differ materially from those projected in the forward-looking statements. Forward-looking

statements are based on the beliefs, estimates and opinions of the Company's management on the

date the statements are made. Except as required by applicable law, the Company assumes no

obligation to update or to publicly announce the results of any change to any forward-looking

statement contained or incorporated by reference herein to reflect actual results, future events or

developments, changes in assumptions, or changes in other factors affecting the forward-looking

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statements. If the Company updates any forward-looking statement(s), no inference should be

drawn that it will make additional updates with respect to those or other forward-looking

statements.