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MANU.V ·

Manhattan Uranium Identifies 3.70% eU₃O₈ Over 5.2 ft in Compilation of 499 Historical Drill Holes at Lisbon Valley, Utah 34% of holes hit mineralization averaging 0.28% eU₃O₈ — matching the district's 0.30% historic production grade across

Drill Results Corporate Updates

Manhattan Uranium Identifies 3.70% eU₃O₈ Over 5.2 ft in Compilation of 499 Historical Drill

Holes at Lisbon Valley, Utah

34% of holes hit mineralization averaging 0.28% eU₃O₈ — matching the district's 0.30% historic production grade across

78 million pounds of U₃O₈1

Vancouver, B.C. – September 10, 2026 – Manhattan Uranium Discovery Corp. (TSXV: MANU, OTC QB: MAUUF, FSE:

J5B0) (“Manhattan” or the “ Company”) is pleased to provide an update on ongoing technical work at its Lisbon Valley

uranium project (“Lisbon Valley”) located in the San Rafael uranium district of Utah.

The North and Central Lisbon Valley Projects comprise 100 claims covering 2,066 acres along the 16-mile-long Lisbon

Valley uranium trend, Utah's largest uranium-producing district, which produced 77.9 million pounds of U₃O₈ at an average

grade of 0.30% U₃O₈ and 10.3 million pounds of V₂O₅ at an average grade of 0.30% V₂O₅ between 1948 and 1988¹. The

properties are located near the historic Mi Vida Mine, one of the district's most prolific past producers, and lie within

trucking distance of Energy Fuels' White Mesa Mill, the only operating conventional uranium mill in the United States.

Highlights

• 3.70% eU₃O₈ over 5.2 ft in hole N -1: The highest-grade historical gamma intercept in the compiled database

and more than ten times the district's reported 0.30% historical production grade.

• 499 historical drill holes compiled into a single modern database: Concentrated on the North Lisbon property

and forming the foundation for the Company's 3D targeting model, with additional legacy records still being

recovered and added.

• More than half the compiled database returned mineralized intercepts: 266 holes (53%) graded above 0.15%

eU₃O₈, which may indicate the mineralized system extends beyond the historically mined areas and across the

Company's North Lisbon block.

• Mineralized intercepts average 0.28% eU ₃O₈: Comparable to the reported 0.30% U ₃O₈ the district mined

between 1948 and 1988, meaning the historical drilling on the Company's ground returned the grades this district

actually produced¹.

• 36 high-priority historical intercepts ranked for follow-up: Filtered to exclude mined-out ground and intervals

within 15 feet of known workings, providing the Company with a drill-ready target list.

“Lisbon Valley alone produced nearly 80 million pounds of U₃O₈ before production ceased in the late 1980s, and much of

that ground has not been evaluated with modern methods. This is not purely greenfield exploration; it is a mill -adjacent

district with a substantial historical production history, and that distinction matters in the context of renewed interest in

domestic uranium supply,” stated William Sheriff, Chairman of Manhattan.

“This is the second major legacy dataset we've compiled and reviewed, and it reflects the broader work underway across

our portfolio. We're developing a much deeper understanding of our U.S. assets, which include 15 past-producing mines.

At Lisbon Valley specifically, a 53% historical gamma -intercept hit rate averaging 0.28% eU ₃O₈ is comparable to the

reported 0.30% in the district . We now have a modern drill -ready foundation across the Lisbon Valley .” st ated Galen

McNamara, CEO and Director of Manhattan.

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Overview

The Company has completed a historical data compilation and digitization effort focused on building a modern digital

drillhole and geological database for the Lisbon Valley.

Figure 1: Lisbon Valley Historical Drill Hole Map

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Selected High-Priority Historical Intercepts

The table below presents 45 high-priority historical intercepts identified to date from the Company's ongoing review of the

database. The table excludes holes flagged as mined out, holes flagged within 5 m of known underground workings,

intervals beginning at 0 m, and exact 1 m or 2 m intervals to avoid including interpreted interval artifacts. These intercepts

are historical in nature, transcribed from legacy project maps and records, and are being used for exploration targeting

and 3D modelling purposes only. They have not yet been independently verified by the Company.

DHID From To Thickness eU₃O₈%

N-1 780.24 785.44 5.2 3.7

FW3-3 815.9 815.9 5 0.94

FW3-2 813.5 813.5 6 0.93

P-3 755.4 755.4 7.5 0.65

81-124 703.65 713.65 10 0.640

P-2 745.4 745.4 2.6 0.54

C-5 798.1 798.1 2.9 0.52

P-1 758.5 758.5 2.9 0.47

FW3-4 810.7 810.7 6 0.44

79-53 765.02 768.52 3.5 0.420

C-10 772 772.0 2.6 0.41

T-5-71 579.70 582.20 1.5 0.410

A-3 721.7 721.7 3.2 0.4

P-4 665.00 665 0.8 0.4

T-5-71 586.7 588.2 1.5 0.4

_07-9 663.10 664.10 1 0.390

_07-7 667.34 668.84 1.5 0.370

106 671.3 671.3 6.5 0.350

0-1 659.35 659.35 3 0.35

FW3-9 809.5 809.5 3.5 0.34

P-5 751.9 751.9 1.3 0.31

C-6 698.2 698.2 3.1 0.3

79-22 722.14 723.14 1 0.280

FW3-8A 788.4 788.4 2.5 0.28

C-2 656.4 656.4 2.8 0.27

U-1 726.5 726.5 4.1 0.27

_07-13 600.39 601.39 1 0.220

T-3-11 730.8 730.8 0.5 0.22

C-7 722.04 722.04 3.8 0.21

T-7-71 749.6 749.6 2 0.21

81-113 710.63 720.13 9.5 0.200

A-8 607.4 607.4 3.2 0.2

N-4 778.6 778.6 4 0.2

C-12 812.2 812.2 4 0.19

79-29 772.28 783.78 11.5 0.110

79-34 816.37 826.37 10 0.110

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79-39 857.97 869.47 11.5 0.100

79-42 742.71 750.71 8 0.100

81-106 716.98 728.48 11.5 0.100

* eU₃O₈ = equivalent U₃O₈ from historical downhole gamma (radiometric) logging, not chemical assays. Values assume

secular equilibrium; disequilibrium, if present, may cause them to overstate or understate true uranium grades. Historical

and unverified; for exploration targeting purposes only.

Geology and Project Context

The Lisbon Valley Project is located in the Lisbon Valley uranium district of Utah, a historically significant uranium -

producing area in the United States. Uranium mineralization at the project is hosted within the Moss Back member of the

Chinle formation and the upper section of the Cutler formation, both of which are fluvial sandstone unit s that served as

the primary hosts for uranium production throughout the Lisbon Valley mining district during the 1950s to 1980s mining

cycle. The district has a well -documented history of uranium production and is underlain by documented infrastructure

including roads, power, and historical mine workings.

The Company's lithology model is being used to constrain uranium -bearing horizons and to support 3D interpretation of

gamma-defined mineralized trends. Using the updated drillhole database, digitized underground workings, and interpreted

lithology model, Manhattan has begun generating preliminary 3D uranium target domains designed to identify areas where

historical gamma intercepts, favorable stratigraphy, and underground development suggest potential for additional

uranium mineralization.

Technical Work Completed to Date

• Consolidated historical drill hole collar, survey, and assay/gamma records into a modern digital database.

• Compiled approximately 499 drill collar locations and matching downhole survey records.

• Recovered additional historical gamma intercepts from legacy project maps not previously captured in the digital

database.

• Added missing survey records where required using vertical -hole assumptions for legacy holes lacking survey

data.

• Reviewed and corrected interval gaps, overlaps, duplicate records, and missing -value codes.

• Built an initial lithology model focused on the Chinle and Cutler formations.

• Generated preliminary 3D uranium target domains to guide follow-up drilling.

Next Steps

• Continued validation and reconciliation of historical gamma data with underground workings and modern

exploration results.

• Refinement of the lithology model and 3D uranium target domains.

• Recovery of additional historical data and expansion of database as the review of legacy records continues.

Technical Disclosure

The historical drill hole and gamma data referenced in this news release were compiled from legacy maps and historical

records believed to be reliable . The Company has not yet completed sufficient work to independently verify these data

and results. In addition, historical gamma values may not be directly comparable to modern chemical assay results and

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are being used by the Company for exploration targeting and modelling purposes only. The Company encourages readers

to exercise appropriate caution when evaluating these data and results.

No current mineral resource or mineral reserve estimate has been established at the Lisbon Valley Project.

The uranium grades in this news release are expressed as equivalent U ₃O₈ (eU₃O₈) and are derived from historical

downhole gamma-probe (radiometric) measurements, not chemical assays. Equivalent grades are calculated from gamma

response and assume secular equilibrium between uranium and its radioactive decay products. Uranium in sandstone -

hosted systems such as those in Lisbon Valley is mobile and may occur in radioactive disequilibrium, in which case eU₃O₈

values may materially overstate or understate true uranium grades. The gamma -probe equipment, calibration standards,

and conversion parameters used by th e historical operators are not fully documented, and the Company has not

independently verified the original measurements or conversions. Reported intervals represent downhole lengths, not true

thicknesses. These historical values are used for exploration targeting and 3D modelling only. The Company encourages

readers to exercise appropriate caution when evaluating these data and/or results.

Mineralization at nearby properties is not necessarily indicative of mineralization at Lisbon Valley, and there can be no

assurance that any processing arrangement will be available.

Qualified Person

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

P.Geo., CEO and a director of Manhattan, who is a Qualified Person as defined by National Instrument 43-101 - Standards

of Disclosure for Mineral Projects (“NI 43-101”). Mr. McNamara is not independent of Manhattan under NI 43-101.

About Manhattan Uranium Discovery Corp.

Manhattan Uranium Discovery Corp. (TSXV: MANU, OTC QB: MAUUF, FSE: J5B0) is a newly consolidated North

American uranium company committed to the discovery, development, and advancement of high -quality uranium assets.

Following the successful acquisitions of Urano Energy and Pegasus Resources, Manhattan now holds a premier portfolio

of 15 past -producing uranium mines across 25 underexplored properties covering 25,099 acres in the United States,

complemented by high -grade exploration potential in Canada’s Atha basca Basin. Backed by an elite technical and

management team with decades of uranium discovery, project advancement, and capital markets experience, Manhattan

is strategically positioned to capitalize on the growing demand for domestic uranium and the Ame rican nuclear

renaissance. For more information about Manhattan, please visit: www.manhattanuranium.com.

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.

Follow Manhattan on social media for the latest updates

• X: https://x.com/manhattanur

• LinkedIn: https://www.linkedin.com/company/manhattanuranium/

On behalf of Manhattan Uranium Discovery Corp

“Galen McNamara”

Chief Executive Officer and Director

604-288-8046

[email protected]

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REFERENCES

¹ Chenoweth, W.L. (1990). Lisbon Valley, Utah's premier uranium area: A summary of exploration and ore production.

Utah Geological and Mineral Survey Open-File Report 188.

FORWARD-LOOKING STATEMENTS

This news release contains “forward -looking statements” and “forward -looking information” within the meaning of

applicable Canadian and United States securities legislation (collectively, “forward-looking statements”). All statements in

this release, other than statements of historical fact, are forward -looking statements. Forward -looking statements are

frequently, but not always, identified by words such as “may”, “will”, “expect”, “intend”, “believe”, “anticipate”, “estimate ”,

“target”, “plan”, “potential”, “c ould” or similar terminology. Forward -looking statements in this release include, without

limitation: the interpretation of historical drill hole, gamma and geological data; the anticipated advancement of the

Company’s mineral properties and project portfo lios, including but not limited to the technical work referenced herein,

including the timing, scope and execution thereof; exploration expenditures, costs and timing of future exploration;

exploration prospects of mineral properties; requirements for addi tional capital; the future price of metals; government

regulation of mining operations; current geopolitical developments, including but not limited to U.S. government policy,

environmental risks; the timing and possible outcome of pending regulatory matte rs; the potential for additional

mineralization; and future plans, projections, objectives, estimates and forecasts and the timing related thereto.

Forward-looking statements are based on management’s current beliefs, expectations and assumptions, including, without

limitation: that historical information is reliable; that future exploration activities will proceed as currently anticipated ; that

permits, equipment, personnel and contractors will be available on commercially reasonable t erms; and that current

commodity prices, labour availability, cost and regulatory frameworks will remain consistent with management’s

expectations. Although management considers these assumptions to be reasonable based on currently available

information, they may prove to be incorrect.

Forward-looking statements are subject to known and unknown risks, uncertainties and other factors that may cause

actual results, performance or achievements to differ materially from those expressed or implied by such forward -looking

statements. Such risks and uncertainties include, without limitation: the risk that historical data may prove to be inaccurate

or unverifiable and that historical radiometric gamma data may not correlate with chemical assay results; that exploration

results may not support further work or drilling; that exploration activities may be delayed, restricted or not carried out as

planned; that permits may be delayed or revoked; the presence of adverse conditions at mineral properties; the price of

uranium and other metals not remaini ng at levels that support continued exploration; the Company’s ability to continue

raising necessary capital to finance operations; and the ability to establish any mineral resource estimate; the Company’s

ability to complete its planned exploration progra ms; environmental regulations or hazards and compliance with complex

regulations associated with mining activities; climate change and climate change regulations; fluctuations in exchange

rates; the business objectives of the Company; whether mineralizatio n can be defined; the uncertainty that any

mineralization encountered on adjacent properties continues on to any of the Company’s properties; the uncertainty that

geological and/or geophysical and/or any trends, interpretations, or conclusions related to a djacent properties have

relevance to any of the Company’s properties; the uncertainty that the exploration season can be extended; changes in

project parameters as plans continue to be refined; the consequences and implications of the historical mining act ivities

on the environment and whether such activities affect potential exploration of the Company’s properties; the implications

of claims from First Nations, Tribes, Tribal Councils or Tribal Governments and land claims settlements on the Company’s

projects; accidents, labour disputes and other risks of the mining industry; future prices of metals; possible variations of

mineral grade or recovery rates; geological, mining and exploration technical problems; failure of plant, equipment or

processes to operate as anticipated; accidents, labour disputes and other risks of the mining industry; title to properties;

operational, technical and geological risks inherent in mineral exploration; changes in capital markets, economic

conditions, regulatory developments and stakeholder relations; the other risks set out in the Company’s public disclosure

record under its profile on SEDAR+ (www.sedarplus.ca) and management’s ability to anticipate and manage the foregoing

risks and uncertainties.

The Company provides no assurance that forward -looking statements will prove to be accurate, as actual results and

future events could differ materially from those anticipated in such statements. Accordingly, readers should not place

undue reliance on forw ard-looking statements. The Company does not undertake to update any forward -looking

statements, other than as required by law.