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3D IP Survey Commenced at Venus Project ➢ 3D IP/resistivity survey has commenced at Venus ➢ Along strike from Pumpkin Hollow Cu, Au, Ag deposits ➢ Untested copper, gold and silver surface geochemical anomalies

Exploration Programs Sampling & Geoscience Results

3D IP Survey Commenced at Venus Project

➢ 3D IP/resistivity survey has commenced at Venus

➢ Along strike from Pumpkin Hollow Cu, Au, Ag deposits

➢ Untested copper, gold and silver surface geochemical anomalies

VANCOUVER, October 16, 2018 - Altan Nevada Minerals Ltd. (TSX.V ANE) (“Altan Nevada ” or the

“Company”) is pleased to announce that a 3D Induced Polarization (IP)/ resistivity survey has

commenced at the Company’s Venus Project, Yerington District, Nevada, USA.

The Venus Project is within the Yerington copper porphyry district located in the Walker Lane

mineralized belt in Nevada . It is approximately six miles east -south-east of the Yerington Township.

Altan Nevada’s decision to advance exploration at Venus coincides with the dev elopment at the

Pumpkin Hollow Copper Mine owned by Nevada Copper Corporation (TSX:NCU) immediately to the

north and less than one mile from the tenement boundary (Figure 1).

Figure 1 - Aerial view of Altan Nevada’s Venus Project and Nevada Copper’s Pumpkin Hollow Project with deposit locations.

Located on -strike from Pumpkin Hollow, Altan Nevada’s Venus Project consists of 111 unpatented

mining claims covering approximately 2,165 acres (~8.76 km²), all situated on Bureau of Land

Management (Federal) land.

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Altan Nevada commissioned leading geo -scientific exploration consultants, Terra Resources Pty Ltd, to

supervise acquisition and interpretation of the 3D IP/resistivity survey. As the Pumpkin Hollow deposits

are high grade IOCG chalcopyrite -magnetite skarn, magnetics and IP/resistivity will be used to seek to

identify the location of mineralisation under cover.

Figure 2 – The 3DIP survey plan (left) and surface geochemistry (right). The IP transmitter locations shown in red and the

receiver locations shown in blue. Geochemical target areas are shown (right). Also shown are Nevada Copper’s deposit

locations.

The 3D IP/resistivity survey is being acquired in east -west survey configuration with 500m sp aced

transmitter lines and 250m spaced receiver lines. The transmitter and receiver spacing along lines are

100m. Transmitter lines have end-of-line offset for increase depth penetration. The survey has been

designed to “see” up to a depth of 400m.

In summary, Venus is considered to have good potential for the discovery of new deposits of similar size

and grade to Pumpkin Hollow. It also has the potential for discovery of buried porphyry -style copper

mineralization with characteristics similar to the Yerington Mine.

The next stage of the exploration program is to rank and further ground truth the existing targets with

the new 3D IP data with a view to drill test late in 2018 . Altan Nevada looks forward to pro viding

additional information after the results of the 3D IP survey have been assessed.

Contact:

John Jones AM (Chairman)

Perth, Australia

Phone: +61 9322 1788

Email: [email protected]

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Altan Nevada Minerals Ltd

800-1199 West Hastings Street

Vancouver BC Canada V6E-3T5

Competent Person Statement

The information in this report that relates to Exploration Results is based on information compiled by Mr

Barry Bourne, who is employed as a Consultant to the Company through geophysical consultancy Terra

Resources Pty Ltd. Mr Bourne is a fellow of the Australian Institute of Geoscientists and a member of the

Australian Society of Exploration Geophysicists and has sufficient experience of relevance to the styles of

mineralisation and the types of deposits under consideration, and activities unde rtaken, to qualify as a

Competent Person as defined in the 2012 Edition of the Joint Ore reserves Committee (JORC) Australasian

Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mt Bourne consents to

the inclusion in the report of matters based on information in the form and context in which it appears.