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Denison Reports Results from Waterbury PEA, Including Base Case Pre-Tax NPV of $177M and IRR of +39.1% Isr Mining Method Estimated to Produce USD$12.23 PER Lb U3O8 Operating Costs J Zone Deposit Renamed Tthe Heldeth Túé (“Tht”) Deposit

Economic Studies

Denison Mines Corp.

1100 – 40 University Ave

Toronto, ON M5J 1T1

www.denisonmines.com

@DenisonMinesCo

PRESS RELEASE

DENISON REPORTS RESULTS FROM WATERBURY PEA,

INCLUDING BASE CASE PRE-TAX NPV OF $177M AND IRR OF +39.1%

ISR MINING METHOD ESTIMATED TO PRODUCE USD$12.23 PER LB U3O8 OPERATING COSTS

J ZONE DEPOSIT RENAMED TTHE HELDETH TÚÉ (“THT”) DEPOSIT

Toronto, ON – Nov. 17, 2020. Denison Mines Corp. (“Denison” or the “Company”) (DML: TSX, DNN:

NYSE American) is pleased to announce the successful completion of an independent Preliminary

Economic Assessment (“PEA”) for the Waterbury Lake Property (“Waterbury”) evaluating the potential use

of the in-situ recovery (“ISR”) mining method at the Tthe Heldeth Túé (see below, formerly named J Zone)

deposit (the “Project”) with associated processing at Denison’s 22.5% owned McClean Lake mill.

The PEA was prepared by Engcomp Engineering & Computing Professionals (“Engcomp”) of Saskatoon

and demonstrates robust economics for a small-scale Athabasca Basin ISR uranium mining project –

including low initial capital costs, low operating costs and globally competitive all-in costs, as follows:

Mine life ~ 6 years (Avg. ~1.6 million lbs U3O8 per year)

Projected mine production (1) 9.7 million lbs U3O8 (177,664 tonnes at 2.49%)

Average cash operating costs USD$12.23 ($16.27) per lb U3O8

Initial capital costs (2) $112 million

Base case pre-tax IRR (3) 39.1%

Base case pre-tax NPV8% (3) $177 million

Base case price assumption UxC spot price(4) (Avg. USD$53.59 per lb U3O8)

Operating profit margin (5) 77% at USD$53.59 per lb U3O8

All-in cost (6) USD$24.93 ($33.16) per lb U3O8

(1) See Deposit, Geology & Projected Mine Plan section below for additional information regarding projected mine production.

Scheduled tonnes and grade do not represent an estimate of mineral reserves.

(2) Initial capital costs exclude $20.1 million of estimated pre-construction Project evaluation and development costs.

(3) NPV and IRR are calculated to the start of pre-production activities for the THT operation.

(4) Spot price forecast is based on “Composite Midpoint” scenario from UxC’s Q3’2020 Uranium Market Outlook

(“UMO”) for the years 2028 to 2033, and is stated in constant (not-inflated) dollars.

(5) Operating profit margin is calculated as uranium revenue less operating costs, divided by uranium revenue.

Operating costs exclude all royalties, surcharges and income taxes.

(6) All-in cost is estimated on a pre-tax basis and includes all project operating costs and capital costs, excluding

project evaluation and development costs, divided by the estimated number of finished pounds U3O8 produced.

Denison is also pleased to announce the re-naming of the J Zone deposit to the “Tthe Heldeth Túé” (“THT”)

deposit – pronounced “Tey Hel-deth Tway”. The Ya’thi Néné Land and Resource Office (“YNLR”), working

together with Denison, reviewed the Conceptual Mining Study (“Concept Study”) prepared by Denison for

the J Zone deposit prior to initiation of the PEA (see news release dated July 28, 2020). The YNLR provided

valuable early feedback related to the Project’s next steps, and recommended the use of a Dené name for

the deposit that would recognize and respect the connection of the Athabasca Denesųłiné to the land where

the deposit is located.

This press release constitutes a “designated news release” for the purposes of the Company’s prospectus

supplement dated November 13, 2020 to its short form base shelf prospectus dated April 2, 2020.

David Cates, President and CEO of Denison, commented:

“The Waterbury PEA further demonstrates the potential for the ISR mining method to change Canada’s

global competitiveness in the uranium mining sector – without requiring the discovery and development of

massive-scale uranium mines. The selection of the ISR mining method for the Tthe Heldeth Túé deposit

has transformed our expectations for the Project – generating robust preliminary financial results with

comparatively modest upfront capital costs and positioning the Project as Denison’s second ISR amenable

development asset with a cost profile that is highly competitive amongst undeveloped uranium mining

assets globally.”

David Bronkhorst, VP Operations of Denison further added:

“Denison’s technical team successfully modelled the application of the ISR mining method to the Tthe

Heldeth Túé deposit in the internal concept study and the preliminary results have now been validated with

the completion of an independent NI 43-101 compliant PEA. Denison’s plan for the Project includes a

‘freeze wall’ design adapted from the ‘freeze dome’ outlined for the Phoenix deposit in the Wheeler River

Pre-Feasibility Study (‘Wheeler PFS’). The freeze wall design allows for the containment of a smaller area

and a significant reduction in up front capital costs, as compared to the ‘freeze dome’. Additionally, the

freeze wall is expected to offer environmental advantages by providing containment of the ISR mining

operation from the depth of the uranium deposit all the way to surface. With the positive results of the freeze

wall design demonstrated in the Waterbury PEA, Denison is also evaluating the potential benefits of a

freeze wall (rather than freeze dome) for use at Wheeler River’s Phoenix deposit.”

Waterbury is owned by the Waterbury Lake Uranium Limited Partnership (“WLULP”), of which Denison

Waterbury Corp. (a wholly-owned subsidiary of Denison) owns 66.90% and Korea Waterbury Lake Uranium

Limited Partnership (“KWULP”) owns 33.10%. KWULP is comprised of a consortium of investors, in which

Korea Hydro & Nuclear Power (“KHNP”) holds a majority position. KHNP is headquartered in Gyeongju,

South Korea and is the country’s largest electrical power generation company, operating 24 nuclear power

reactors and supplying approximately one-quarter of the country’s electricity. KHNP is also a significant

shareholder in Denison.

The PEA is prepared on a Project (100% ownership) and pre-tax basis, as each of the partners to the

WLULP are subject to different tax and other obligations. After-tax results attributable to Denison’s

ownership interest are provided below under the heading “Indicative Denison Post-Tax Results”. All

amounts are in Canadian dollars unless otherwise noted.

The PEA is a preliminary analysis of the potential viability of the Project ’s mineral resources, and should

not be considered the same as a Pre-Feasibility or Feasibility Study, as various factors are preliminary in

nature. There is no certainty that the results from the PEA will be realized. Mineral resources are not mineral

reserves and do not have demonstrated economic viability.

Preliminary Economic Assessment Highlights

• Selection of ISR mining method potentially unlocks the value of the THT deposit: Following the

release of the Wheeler PFS in 2018 and subsequent studies aimed at increasing confidence in the

ISR mining method for the Phoenix deposit, including the achievement of “proof of concept” (see

Denison’s news release dated June 4, 2020), Denison evaluated the application of the ISR mining

method on the THT deposit. Similar to Phoenix, the THT deposit is an unconformity-related uranium

deposit, where the mineralization is interpreted to be situated in permeable ground – expected to allow

a mining solution to travel within the mineralized zone. Additionally, the basement rock located below

the mineralized zone is interpreted to be highly impermeable and is expected to allow for containment

of the mining solution beneath the deposit.

• Freeze Wall design expected to reduce technical risk and upfront capital costs : Full hydraulic

containment of the orebody during mining activities has been planned for the Project with the

installation of a freeze wall from surface to the basement rocks underlying the THT deposit– effectively

creating containment 360 degrees around the deposit. This design makes use of established ground-

freezing technology and conventional diamond drilling to create a physical perimeter around the

deposit – containing the mining solution used in the ISR mining process and protecting the surrounding

environment to minimize environmental impact s of the P roject. Several additional containment

methodologies were evaluated as part of the Concept Study – including the f reeze dome design

outlined in the Wheeler PFS. Results of the Concept Study showed that the freeze wall design offered

considerably lower technical risk, equal or greater environmental protection, a smaller environmental

footprint, sustainability benefits associated with the utilization of drilling techniques conducive to local

employment, and improved economic results with significantly lower initial capital costs.

• Existing regional infrastructure offers significant benefit: The Waterbury Lake property is located

approximately 15 kilometres from Denison’s 22.5% owned McClean Lake uranium mill, in the

infrastructure rich eastern portion of the Athabasca Basin region. The PEA assumes the McClean

Lake uranium mill will be used to process the Uranium Bearing Solution (“UBS”) to be recovered from

the ISR wellfield and the nearby Points North Landing (“Points North”) facilities will be used for

accommodations and other support services. Taken together, this existing regional infrastructure

results in a significant reduction in the initial capital costs and operating costs estimated in the PEA.

• Potential to be one of the most environmentally responsible mining operations in the world:

The combination of the ISR mining method with a high-grade uranium deposit in the Athabasca Basin

region has the potential to result in one of the most environmentally protective mining operations in

the world – owing to the small foot print of the operation and its minimal surface disturbances, as well

as the fact that there are no tailings expected to be generated and no site water discharge planned.

The modelled operation also has access to the Provincial power grid and is not expected to rely on

diesel generators for primary power on site. Additionally, t he freeze wall design provides for the

physical isolation of the ISR mining operation from the surrounding environment, which alleviates the

primary environmental concern of conventional ISR mining operations and facilitates a controlled

restoration process once mining has been completed.

THT ISR Operation – Summary

The THT ISR operation is estimated to produce total mine production of 9.7 million pounds U3O8 (177,664

tonnes at 2.49% U3O8) over an approximate six year mine-life with final processing occurring at Denison’s

22.5% owned McClean Lake mill. The PEA includes an indicative timeline with p re-production activities

beginning in 2025, and with first production estimated in 2028.

Table 1 – Waterbury PEA Financial Results (100% Basis)

Base case pre-tax NPV8% (1) $177 million

Base case pre-tax IRR (1) 39.1%

Base case pre-tax payback period (2) ~22 months

Initial capital costs (3) $112 million

Average annual mine production(4) ~1.6 million lbs U3O8

Mine life ~6 years

Exchange rate (5) (US$:CAD$) 1:1.33

Discount rate 8.00%

(1) NPV and IRR are calculated to the start of pre-production activities for the Project.

(2) Payback period is stated as number of months to pay-back from the start of uranium production.

(3) Initial capital costs exclude $20.1 million of estimated pre-construction Project evaluation and development costs.

(4) Scheduled tonnes and grade do not represent an estimate of mineral reserves. See Deposit, Geology & Mine plan

section below for additional information regarding projected mine production.

(5) Exchange rate applied on uranium sales.

Table 2 – THT Operating Cost per Pound U3O8

CAD$ USD$

Mining / Wellfield 5.73 4.31

Milling / Processing 8.07 6.07

Transport to converter 0.53 0.40

Site support and administration 1.94 1.46

Total Operating Costs per pound U3O8 $16.27 $12.23

Table 3 – THT Capital Costs ($ million) (1)

Initial Sustaining Total

Wellfield 49.6 24.4 74.0

Milling (McClean Lake modifications) 1.1 - 1.1

Surface facilities 2.1 - 2.1

Utilities 0.7 - 0.7

Electrical 5.0 - 5.0

Civil & earthworks 5.8 0.4 6.2

Offsite infrastructure 7.5 - 7.5

Decommissioning - 19.4 19.4

Construction Indirect 14.0 - 14.0

Subtotal 85.8 44.2 130.0

Contingency 25.8 5.8 31.6

Total Capital Costs (100%) 111.6 50.0 161.6

(1) Initial capital costs exclude $20.1 million of estimated pre-construction Project evaluation and development costs.

The PEA has been completed in accordance with NI 43- 101, Canadian Institute of Mining, Milling and

Petroleum (CIM) standards and best practices , as well as other standards such as the AACE Cost

Estimation Standards. The PEA is a preliminary analysis of the potential viability of the Project’s mineral

resources, and should not be considered the same as a Pre-Feasibility or Feasibility Study, as various

factors are preliminary in nature. There is no certainty that the results from the PEA will be realized. Mineral

resources are not mineral reserves and do not have demonstrated economic viability.

The technical report supporting the PEA results included in this news release will be filed on SEDAR within

45 days of this release. Estimated capital and operating costs are summarized above, with details provided

throughout the balance of this news release. Initial capital costs reflect the estimated cost of building the

proposed ISR mining operation and exclude future project evaluation and development costs that must be

incurred prior to construction. These costs should be considered when assessing the merit of advancing

the project to a development decision in the future.

Price Assumptions & Sensitivities

The base -case economic analysis assumes uranium sales will be made from time to time throughout

production at UxC’s forecasted annual “Composite Midpoint” spot price from the Q3’2020 Uranium Market

Outlook (“UMO”), which is stated annually in constant (non-inflated) 2020 dollars and ranges from ~USD$49

per lb U3O8 to USD$57 per lb U3O8 during the approximate six year estimated life of the THT operation

(assumed for pricing purposes to be from 2028 to 2033). The average base case selling price is USD$53.59

per lb U3O8.

Given the estimated all-in costs of USD$24.93 per lb U3O8, the Project is projected to be able to generate

positive economic results at uranium selling prices in the range of recent market conditions, while also

offering excellent leverage to a rising uranium price, as outlined below:

Table 4 – Sensitivity of Waterbury to Uranium Pricing Scenarios (100% Basis)

Low Case Base case High Case

Uranium price USD$35 per lb U3O8 UxC spot price (3) USD$65 per lb U3O8

Pre-tax NPV8% (1) $38 million $ 177 million $ 265 million

Pre-tax IRR (1) 17.4% 39.1% 50.0%

Pre-tax payback period (2) ~33 months ~22 months ~18 months

(1) NPV and IRR are calculated to the start of pre-production activities for the Project.

(2) Payback period is stated as number of months to pay-back from the start of uranium production.

(3) Spot price forecast is based on “Composite Midpoint” scenario from UxC’s Q3’2020 Uranium Market Outlook (“UMO”) for the years

2028 to 2033 and is stated in constant (not-inflated) dollars.

ISR Mining Method Transforms Potential for Smaller Scale Unconformity Hosted Deposits

The ISR mining method currently accounts for over 50% of the world’s uranium production – with most of

the production coming from the low -cost mining operations in Kazakhstan. The mining method involves

pumping a mining solution (lixiviant) through a suitable orebody via a series of injection wells drilled from

surface. As the lixiviant travels through the hos t rock, it dissolves or leaches the uranium into the mining

solution, producing a UBS, which is then pumped back to surface via recovery wells. Once on surface, the

UBS is transported (either by pipeline or trucks) to a surface processing plant for the chemical separation /

removal of the uranium, and reconditioning of the lixiviant for reinjection into the orebody and further mining

cycles.

Notably, the ISR mining method does not involve the mechanical excavation or milling (e.g. crushing and

grinding) of the uranium bearing host rock. Additionally, as the leaching process occurs underground, as

the lix iviant travels through the host rock, there is little waste produced by the ISR mining process –

including no generation of conventional tailings requiring long term storage. Taken together, the capital cost

profile of ISR mining is typically a fraction of a conventional uranium mine – which would require a shaft,

decline, or open pit to access the orebody, as well as a processing plant capable of accepting the host rock,

leaching in vessels on surface, and neutralizing any associated waste for long-term storage.

Similarly, the ISR mining process relies primarily on the flow of the mining solution through the network of

injection and recovery wells, which involves a support system of pumps and piping, but does not require

heavy equipment, is generally not energy intensive, and does not require miners to work underground or in

close proximity to the uranium orebody, which is advantageous from a safety and radiation protection

standpoint. These factors, amongst others, contribute to ISR mining operations typically having lower

operating cost profiles in comparison to conventional uranium mines.

While the ISR mining method is not currently being used in Canada for uranium mining, unconformity -

related uranium deposits in the Athabasca Basin, including the THT deposit and the Phoenix deposit, have

all the attributes necessary to be a successful ISR operation, as outlined below:

1. Mineralization that is situated in permeable ground, allowing the mining solution to travel from the

injection well through the orebody and ultimately back to surface via a recovery well;

2. Mineralization that is readily dissolvable by the mining solution; and

3. Mineralization that is within a setting which allows for containment of the mining solution – such

that the mining solution can be recovered without contaminating the environment or being diluted

by natural ground water.

The geological features found in the THT deposit are similar to those of Wheeler River’s Phoenix deposit,

offering amenability to ISR mining – including the position of the deposit at the unconformity, anticipated

permeability of the mineralized zone, and the impermeability of the underlying basement rock.

The results of the PEA for the THT deposit demonstrate that even smaller-scale uranium deposits in the

Athabasca Basin region, with access to an existing processing plant, have the potential to become globally

competitive as a result of the unique cost advantages associated with the ISR mining method.

As ISR mining is a novel mining method for the Athabasca Basin, there is risk that the Company may not

be able to complete ISR operations as outlined in the PEA and/or that the costs could be materially different

than estimated.

Deposit, Geology & Projected Mine Plan

Waterbury is host to two uranium deposits, THT and Huskie, with estimated mineral resources listed in the

table below.

Table 5 – Waterbury Mineral resource Statement (1), (2) (100% Basis, 0.1% grade cut-off)

Deposit Deposit Zone Category Tonnage

(kt)

Grade

(%U3O8)

Contained Metal

(x1,000 lbs. U3O8)

Tthe Heldeth Túé

East pod (3) Indicated 164 3.2 11,580

West pod (3) Indicated 128 0.4 1,230

Total Indicated 291 2.0 12,810

Huskie Total Inferred 268 0.96 5,687

(1) Numbers may not add due to rounding.

(2) For further details, see the Company’s report entitled "Technical Report with an Updated Mineral Resource Estimate for the Waterbury Lake

Property, Northern Saskatchewan, Canada – Mineral Resource Estimate”, as filed on SEDAR and available on the Company’s

website. Mineral resources that are not mineral reserves do not have demonstrated economic viability.

(3) For presentation purposes for this press release, the THT mineral resource estimate presented in this table has been divided into the East

and West pods, to illustrate each zone’s estimated size and the potential applicability of mining methods, and is not intended to replace or

amend the mineral resource estimate in the technical report referred to in note (2) above.

The PEA has been prepared to eval uate the technical and economic viability of extracting the Indicated

mineral resources estimated for the THT deposit, and excludes the Inferred mineral resources estimated

for the Huskie deposit. The geologic setting of the Huskie deposit differs from the THT deposit – in that it is

hosted entirely in the basement rocks underlying the Athabasca sandstone, and accordingly is not expected

to be sufficiently permeable to be amenable to development with the ISR mining method.

As discussed above, the THT deposit is expected to be amenable to ISR mining owing to its position at the

contact of the basement rock s and the overlying Athabasca Sandstone, where permeability is increased.

The THT deposit is hosted in an east-west fault with the underlying basement consisting of metasediments

bounded by orthogneiss to the north and south. The metasediments are 90 to 120 metres thick and include

a 20 metre thick graphitic pelitic gneiss.

There are two defined mineralized pods that make up the THT deposit – the West pod and the East pod.

The East pod contains over 90% of the Indicated mineral resources and angled drilling from land is expected

to allow for ISR wells and the associated freeze wall to reach the THT deposit East pod without constructing

a berm or peninsula into the surrounding lakes (see Figure 1). Accordingly, the PEA considers the recovery

of the East pod only. A portion of the East pod is expected to be sterilized as a result of the installation of

the freeze wall, rendering approximately 206,000 lbs U3O8 unrecoverable. The balance of the East pod is

assumed to be recoverable based on an 85% mining recovery rate, resulting in total projected mine

production of 9.7 million lbs of U3O8, as shown in Table 6 below. Projections of scheduled tonnes and grade

do not represent an estimate of mineral reserves.

Table 6 - Tthe Heldeth Túé Projected Mine Production (100% Basis, 0.0% grade cut-off)

Tthe Heldeth Túé

Deposit Area

Tonnage(1)

(kt)

Grade(1)

(%U3O8)

Contained

Metal(1)

(x1,000 lbs. U3O8)

Sterilized

Metal(1)

(x1,000 lbs. U3O8)

Projected Mine

Production(2)

(x1,000 lbs. U3O8)

West Pod 226 0.27 1,347 n/a 0

East Pod 212 2.49 11,634 206 9,713

(1) Tonnage, Grade, Contained Metal and Sterilized Metal presented at a 0% grade cut off to reflect ISR mining method.

(2) ISR Mine Projected Production uses the application of an 85% ISR mining recovery factor with a 0% mineral resource grade cut-off.

The THT deposit is extremely well defined by 268 drill holes intersecting uranium mineralization over a

combined east-west strike length of up to 700 metres and a maximum north-south lateral width of 70 metres.

The mineralization thickness varies from 0.50 to 19.5 metres and the mineralization is found within several

metres of the unconformity at depths of 195 to 230 metres. The THT deposit has been drilled, on average,

at 10 metre by 25 metre spacings across the deposit and in some cases a more dense drill spacing has

been applied. The genesis and structural complexity of the deposit are well understood. There are no

outlying elements of the deposit requiring further drill testing.

Importantly, during the PEA process, additional work was undertaken to obtain permeability data for the

THT deposit. Permeability values collected from core samples from within the mineralized zone were

reviewed by a team of independent experts who concluded that adequate hydraulic conductivity values ,

necessary to support economical ISR production rates , could be achieved through a combination of

engineering controls (e.g. well spacing) and utilization of permeability enhancement techniques. Additional

hydrogeologic testing and characterization of the THT deposit will be required to validate these assumptions

in future studies.

THT Freeze Wall Design

In conventional ISR operations, containment of the mining solution is typically achieved by natural

impermeable bounding layers in the geological strata and/or by creating a natural drawdown (via pumping)

of the water table towards the ore zone. At the THT deposit, there is a natural impermeable layer below the

deposit, in the form of a competent package of basement rocks, but the deposit is otherwise hydraulically

connected to the vast regional groundwater system in the overlying sandstone formation that defines the

Athabasca Basin. An artificial freeze wall is planned to isolate the ISR wellfield from the surrounding

environment and contain the mining solution within the mineralized zone.

The freeze wall is expected to be established by drilling a series of vertical or angled drill holes from surface.

Once the hole has been completed, it will be cased with a dual-layered pipe that will allow for the circulation

of a low -temperature brine solution in the holes , which is designed to remove heat from the ground and

result in the freezing of the natural groundwater in the vicinity of the freeze hole. The frozen ground will

expand out from each freeze hole and merge together with the frozen ground associated with an adjacent

freeze hole, establishing an impermeable frozen wall that will surround the perimeter of the deposit from

surface to depth. The freeze holes will also be keyed into the basement rock below the deposit to effectively

create an in-ground leach vessel for the ISR mining to take place within.

The freeze wall design is comprised of 92 holes planned at 7 metre spacing to a target depth of 200 metres,

which will extend below the unconformity elevation into the basement rock. This represents a total of 28,766

metres of drilling, which is anticipated to be completed using commonly used diamond drilling methods

conducive to local employment. This drilling method and design has a much lower technical risk profile than

the horizontal drilling required as part of the f reeze dome design included in the Wheeler PFS, as both

diamond drilling and the associated ground freezing in vertical or angled drill holes, are well established

throughout the world and are already in use in the existing mining operations in the Athabasca Basin region.

The PEA assumes that it will take 12 months, after installing the necessary freeze holes, for the ground

freezing process to advance to a sufficient point to achieve the desired level of containment.

Several other containment options were investigated as part of the Concept Study, including t he freeze

dome design outlined in the Wheeler PFS. The installation of a freeze wall showed significant advantages

in comparison to a freeze dome, with a much lower technical risk profile and equal or greater environmental

protection, as well as a smaller environmental footprint, and greater potential for community benefits.

Denison is evaluating a potential adaptation to the ground freezing containment design at Wheeler River to

take advantage of the potential benefits of a freeze wall design similar to the proposed design for the THT

deposit.

See Figure 1 for proposed THT Wellfield and Freeze Wall Containment Configuration

ISR Wellfield Design

Conventional ISR roll -front uranium deposits are typically spread out over several square kilometres of

area, owing to the low-grade nature of the deposits. An ISR uranium mining operation in the United States

or Kazakhstan will typically have uranium grades in the range of 0.03 - 0.30% U3O8. Accordingly, the low-

grade nature of these deposits , combined with well spacing, reagent consumption, surface piping and

pumping distribution systems , all contribute to create economic thresholds which impact the viability of

some deposits.

In the case of the THT east pod, the ore is confined to a relatively small area (300 metres x 70 metres) and

has demonstrated itself to be readily leachable in laboratory testing. The average grade of mineralization

in the east pod (approximately 2.49 % U 3O8) is also several times higher than a typical low -grade ISR

operation.

The wellfield design included in the P EA uses 184 wells at 7 m etre spacing arranged in a 5- spot pattern,

with four injection wells around one recovery well . The wells will be drilled from surface within the freeze

wall and angled out to penetrate the mineralized zone at depth with a roughly 7 m etre spacing. The

maximum drilling angle is limited to 45 degrees to reduce the technical risk of drilling and well installation.

Eight monitoring wells will be installed outside of the freeze wall to detect and remediate any excursion of

lixiviant from the mining zone, which is considered unlikely due to the containment of the freeze wall.

Table 7 – Summary THT ISR Wellfield Wells

Number of Wells Drill Metres

Recovery Wells 66 20,637

Injection Wells 118 36,896

Monitoring Wells 8 1,750

Total 192 59,283

See Figure 1 for proposed THT Wellfield and Freeze Wall Containment Configuration

Metallurgy, Lixiviant Supply & Processing of UBS

Production of the lixiviant mix and final mineral processing of the UBS expected to be recovered from the

THT deposit is assumed to occur at the nearby McClean Lake mill. The mill is owned by the McClean Lake

Joint Venture (“MLJV”) of which Orano Canada Inc. holds a 70% interest, Denison Mines Inc . (a wholly-

owned subsidiary of Denison) holds a 22.5% interest, and OURD (Canada) Co., Ltd. holds a 7.5% interest.

The mill is currently processing material from the Cigar Lake mine under a toll milling agreement (up to 18

million lbs U3O8 per year); however, it has approximately 6 million lbs U3O8 per year in additional licenced