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Element 29 Further Confirms past Drill Results Used in Historical Copper Resource Estimate at Flor De Cobre

Drill Results

Element 29 Further Confirms past Drill Results

Used in Historical Copper Resource Estimate

at Flor De Cobre

Vancouver, British Columbia--(Newsfile Corp. - June 1, 2022) - Element 29 Resources Inc.

(TSXV:

ECU) (OTCQB: EMTRF)

("

Element 29

" or the "

Company

") announces results of three additional drill

holes from the recently completed 4,500 metre ("

m

"), twelve-hole drill program at the Flor de Cobre

Copper Project ("

Flor de Cobre

" or "

the Project

") located in southern Peru (

Figure 1

).

Steve Stakiw, Element 29's President and CEO comments, "These latest Flor de Cobre drill results

continue to demonstrate strong correlation with historical holes and adds confidence to our planned

initial mineral resource estimate which we expect to complete following the receipt of the remaining

results. Additionally, we have continued to encounter copper mineralization significantly deeper than in

the historical holes, which supports the potential for primary sulphide resources at depth."

Flor de Cobre Drilling Highlights

These additional holes continue to show excellent correlation with their respective historical holes.

The position and thickness of enrichment intersected by the twinned holes is similar to their

historical counterparts.

Drill hole FDC003 intersected 295.65 m of 0.38% copper ("

Cu

") including 46.95 m of 0.69% Cu

as oxides and 67.30 m of 0.46% Cu in the enriched sulphide zone followed by 145.50 m of 0.30%

Cu in the primary sulphide zone below.

Drill hole FDC004 intersected 164.60 m of 0.43% Cu including 37.45 m of 0.75% Cu in an

enriched sulphide zone followed by 127.15 m of 0.33% Cu in the primary sulphide zone below.

Drill hole FDC005 intersected 143.00 m of 0.34% Cu including 57.40 m of 0.46% Cu in an

enriched sulphide zone followed by 85.60 m of 0.26% Cu in the primary sulphide zone below.

The objectives of the current drill program are to verify the historical resource estimate of 57.4 million

tonnes of 0.67% Cu associated with a supergene enrichment blanket formed on the Candelaria porphyry

("

Candelaria

") and to explore for primary Cu sulphide mineralization underneath the enrichment blanket

to depths of over 500 m.

The source of the historical resource estimate is the report Rio Amarillo Mining Ltd. - Candelaria

Porphyry Copper Deposit, Arequipa, Peru, Mineral Reserve Estimate, 1996. This historical resource is

relevant to Flor de Cobre as it suggests supergene-enriched mineralization of interest may be present at

Candelaria. However, the Company cautions that the parameters, assumptions, and methods used to

calculate the historical estimate are unknown. Additionally, the historical estimate does not use resource

categories described in CIM Definition Standards for Mineral Resources and Mineral Reserves (2014).

It is also unclear what portion of this historical resource estimate is within the current Flor de Cobre

property configuration. A Qualified Person has not done sufficient work to classify the historical estimate

as a current mineral resource and it is unclear if the current work plan will confirm the resource. For these

reasons, the historical resource has not been verified by the Company and the Company is not treating

the historical estimate as a current mineral resource.

Table 1

. Results of drill holes FDC003, FDC004, and FDC005. Grades are length-weighted averages

of samples within the intervals shown.

Hole

From

(m)

To

(m)

Length

2

(m)

Cu

(%)

Mo

(%)

Ag

(ppm)

As

(ppm)

CuEq

1

(%)

FDC003

14.35

310.00

295.65

0.38

0.009

1.1

111

0.42

oxide

14.35

61.30

46.95

0.69

0.005

0.7

16

0.72

enriched

97.20

164.50

67.30

0.46

0.018

0.6

31

0.53

primary

164.50

310.00

145.50

0.30

0.005

1.3

197

0.33

FDC004

74.40

239.00

164.60

0.43

0.006

0.7

12

0.46

enriched

74.40

111.85

37.45

0.75

0.003

0.8

19

0.77

primary

111.85

239.0

127.15

0.33

0.007

0.7

10

0.36

FDC005

65.40

208.40

143.00

0.34

0.004

1.3

59

0.37

enriched

65.40

122.80

57.40

0.46

0.004

0.7

19

0.48

primary

122.80

208.40

85.60

0.26

0.004

1.6

86

0.29

1

Copper equivalent grades (CuEq) are for comparative purposes only. Calculations are uncut and recovery is assumed to be 100% as

metallurgical data is insufficient to allow for estimation of metal recoveries. Copper equivalence (CuEq %) is calculated as: CuEq (%) = Cu (%) +

[3.55 × Mo (%)] + [0.0095 × Ag (g/t)], utilizing metal prices of Cu - US$3.34/lb, Mo - US$11.86/lb and Ag - US$21.87/oz. Metal prices are based on

a 2-year average of monthly LME metal prices.

2

Intervals are downhole drilled core lengths. Drilling data to date is insufficient to determine true width of mineralization. Assay values are uncut.

The Company's drill program consists of approximately 4,500 m of diamond drilling centred on the

Candelaria porphyry complex

(Figure 2)

. A total of 2,180 m was allocated to twin nine historical drill

holes to verify the accuracy of existing historical geochemical assays and drill logs (

Table 3

). These nine

drill holes are interpreted to represent 70% of the Cu contained in the historical copper resource

estimate and potentially verify the assay results and provide the level of confidence needed for

completion of a planned resource estimate that meets CIM best practice guidelines. The first three drill

holes of the 2022 Flor de Cobre drill program included 349 m of 0.77% Cu, including 123 m of 1.42%

Cu (refer to

April 19, 2022

press release). The remaining 2,320 m in three drill holes was allocated to the

drill program will test the primary copper sulphide mineralization potential below the supergene

enrichment blanket to depths of more than 500 m.

Drill hole FDC003 was collared in an early phase of quartz monzodiorite porphyry belonging to the

Candelaria porphyry complex, as shown in Figure 3 and intersected 46.95 m of 0.69% Cu in an oxide

zone above a chalcocite-dominated enrichment zone returning 67.3 m of 0.46% Cu. Primary sulphide

mineralization with a pyrite-chalcopyrite assemblage extended beneath the enrichment zone and

returned 145.5 m of 0.30% Cu. Strong potassic alteration overprinted by sericite-pyrite alteration

continued to the end of the hole at 394 m.

FDC004 intersected the strongly potassic altered, early quartz monzodiorite porphyry through its entire

length. Chalcocite-dominated enrichment was encountered at 74.4 m below surface and returned 37.45

m of 0.75% Cu followed by 127.15 m of 0.33% Cu of primary sulphide. Locally elevated copper grades

are present in the broader primary sulphide interval (see Image 1).

The southern edge of the early quartz monzodiorite porphyry was cored by FDC005, which intersected

an enrichment zone of 57.4 m of 0.46% Cu followed by primary sulphides returning 85.6 m of 0.26% Cu.

Alternating intervals of early quartz monzodiorite porphyry, later quartz monzodiorite porphyry,

hydrothermal breccia, and sedimentary host rocks were intersected.

Comparison with Historical Data

The primary objective of the drilling program is to verify results from historical drilling, which was a

combination of core and reverse circulation drilling completed in the mid-1990's by Rio Amarillo and

Phelps Dodge. Materials from these drilling programs are unavailable and prevented a Qualified Person

from verifying copper geochemical results. Therefore, twinning selected holes is required to verify results

from historical drilling such that it can be used in future resource estimation. Furthermore, analysis of

other elements of interest such as molybdenum and silver were incomplete in the historical database.

Multi-element analysis from twinned holes provides an opportunity to investigate a possible economic

contribution of these constituents.

The third hole of the 2022 program (FDC003) twinned historical reverse circulation drill hole CAR-190,

FDC004 twinned historical reverse circulation hole CAR-189, and FDC005 twinned historical core hole

M-008. Results from the latest batch of holes were very similar to their historical twins both in Cu grades

and the position of the enrichment zone. Graphic representations of the twin and historical drilling results

are plotted in Figures 5 and 6.

Table 2.

Comparison of intervals from the historical drill holes CAR-190, CAR-189, and M-008 with

twinned holes FDC003, FDC004, and FDC005.

FDC003

CAR-190

From

To

Length

Cu%

From

To

Length

Cu%

Zone

14.35

230.00

215.65

0.42

12.00

230.00

218.00

0.47

Total

14.35

61.30

46.95

0.69

12.00

54.00

42.00

0.82

Oxide

97.20

164.50

67.30

0.46

88.00

160.00

72.00

0.52

Enriched

164.50

230.00

65.50

0.36

160.00

230.00

70.00

0.36

Primary

FDC004

CAR-189

From

To

Length

Cu%

From

To

Length

Cu%

Zone

74.40

207.00

132.60

0.44

76.00

208.00

132.00

0.39

Total

74.40

111.85

37.45

0.75

76.00

112.00

36.00

0.79

Enriched

111.85

207.00

95.15

0.31

112.00

208.00

96.00

0.24

Primary

FDC005

M-008

From

To

Length

Cu%

From

To

Length

Cu%

Zone

65.40

208.40

143.00

0.34

73.15

208.65

135.50

0.35

Total

65.40

122.80

57.40

0.46

73.15

127.00

53.85

0.48

Enriched

122.80

208.40

85.60

0.26

127.00

208.65

81.65

0.27

Primary

The Company continues to progress drill permitting on the Atravesado porphyry target ("

Atravesado

") in

preparation for initial drill-testing of a priority porphyry target supported by coincident outcrop geology,

surface geochemistry, and geophysical responses. Atravesado is located approximately 2 kilometres

("

km

") northwest of Candelaria and is a 1.5 km x 1.6 km circular zone characterized by outcropping

copper oxide mineralization in association with quartz vein stockworks and potassic alteration (

Figure

2

). Late-mineral porphyry dikes are also mapped within the target area.

Analytical Quality Control & Quality Assurance

Candelaria Resources S.A.C., a wholly owned subsidiary of Element 29 Resources Inc., supervises

drilling and carries out sampling of HQ and NQ core. Logging and sampling are completed at a secured

Company facility situated on the Flor de Cobre project site. Sample intervals are nominally 2 m long. Drill

core is cut in half using a rotary diamond blade saw and samples are sealed on site before

transportation to the ALS Peru S.A.C. sample preparation facility in Arequipa by Company vehicles and

staff. Prepared samples are sent to Lima by ALS Peru S.A.C. for analysis. ALS Peru S.A.C. is an

independent laboratory. Samples are analyzed for 35 elements using an Aqua Regia digestion and ICP-

AES analysis (ME-ICP41). Samples reporting over limits are analyzed by Aqua Regia digestion with

ICP-AES finish (ME-OG46). ALS meets all requirements of International Standards ISO/IEC

17025:2005 and ISO 9001:2015 for analytical procedures.

Element 29 employs an independent, internal quality assurance/quality control program that includes

insertion of duplicate, blank, and certified reference samples at the field site. The Company is not aware

of any drilling, sampling, recovery, or other factors that could materially affect the accuracy or reliability of

the data reported.

Qualified Person

The scientific and technical content of this press release has been reviewed and approved by Paul J.

Johnston (PhD, P.Geo), Vice President of Exploration for Element 29 and is a "Qualified Person" as

defined in National Instrument 43-101 Standards of Disclosure for Mineral Projects.

Neither the TSX Venture Exchange nor its Regulation Service Provider (as that term is defined

in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or

accuracy of this press release.

Table 3

: List of twelve drill holes forming the 2022 Flor de Cobre drilling program. Nine of the twelve drill

holes are designed to twin historical drill holes. The coordinates, depth, orientation, and hole type of the

historical holes are shown. Drill holes FDC001 through FDC012 are complete, with results pending for

FDC006 through FDC012.

Hole ID

Hole ID

(historical)

East

North

Elev

(m)

Length

(m)

Azimuth

(degrees)

Dip

(degrees)

Historical Hole

Type

FDC001

K-008

245888

8148409

2776

350

0

-90

DDH

FDC002

CAR-188

245812

8148419

2800

256

0

-90

RC

FDC003

CAR-190

246004

8148314

2791

230

0

-90

RC

FDC004

CAR-189

245911

8148317

2793

208

0

-90

RC

FDC005

M-008

245894

8148213

2786

294

0

-90

DDH

FDC006

K-006

245719

8148358

2825

231

0

-90

DDH

FDC007

K-010

246086

8148405

2801

257

0

-90

DDH

FDC008

I-008

245937

8148571

2752

147

0

-90

DDH

FDC009

CAR-186

246212

8148415

2772

211

0

-90

RC

FDC010

NA

245610

8148517

2743

NA

210

-55

NA

FDC011

NA

246104

8148478

2789

NA

44

-55

NA

FDC012

NA

246004

8148314

2791

NA

300

-55

NA

Coordinates are in WGS84 zone 18S UTM

About Flor de Cobre

Flor de Cobre is a porphyry copper exploration project that contains the Candelaria and the recently

outlined Atravesado porphyry copper targets. The property is in the Southern Peru Copper Belt and is 5

km northwest of Nexa Resources' Chapi mine and 26 km southeast of the Cerro Verde mine owned by

Freeport-McMoRan, Sumitomo Metal Mining, and Compañía de Minas Buenaventura. Candelaria is a

classic Andean porphyry system with primary copper sulphide mineralization associated with a multi-

phase quartz monzonite porphyry complex. Weathering redistributed primary mineralization into a sub-

horizontal enrichment blanket containing secondary copper oxide and sulphide minerals at the base of a

hematitic leached cap. Remnants of the upper jarositic component of the leached cap overlying the

hematitic cap are preserved on the higher hill tops around the Candelaria prospect. Atravesado is a

porphyry copper exploration target located about 2 km northwest of Candelaria. An IP/Resistivity

geophysical survey completed in 2020 outlined a core of moderate resistivity measuring 1.5 x 1.6 km

that coincides with widespread copper oxide mineralization, strong copper geochemistry, and late-stage

quartz monzodiorite porphyry dikes. The resistive core is surrounded by a high-chargeability halo

corresponding with weathered quartz-sericite-pyrite alteration.

About Element 29 Resources Inc.

Element 29 Resources Inc. is an emerging copper exploration and development company focused on

advancing its portfolio of Peruvian projects towards development in one of the world's lower-risk mining

jurisdictions. Element 29's growth strategy is led by our strong board and management, who have a

proven track record of discovery and delivering significant value to our shareholders.

The Company's principal objective is to explore and develop its flagship Flor de Cobre porphyry Cu-Mo

project located in southern Peru, 26 km southeast from Freeport-McMoRan's Cerro Verde Cu-Mo mine.

At the same time, the Company intends to build on its potential copper inventory with continued

exploration of its Flor de Cobre project as well as its remaining 22,000 hectares of mining concessions

in Peru, including the recently discovered Elida porphyry copper-molybdenum-silver system located 85

km from the coast in central Peru. Both projects are well located for potential mine development and will

benefit from nearby infrastructure including roads, powerlines, ports, water, and a skilled workforce.

More information is available at

www.e29copper.com

.

For more information:

David Jan

Investor Relations

1-888-246-7881

[email protected]

Forward-Looking Statements

This press release contains certain forward-looking information and forward-looking statements within

the meaning of applicable Canadian securities legislation (collectively, "

Forward-looking

Statements

"). All statements, other than statements of historical fact, constitute Forward-looking

Statements. Words such as "will", "intends", "proposed" and "expects" or similar expressions are

intended to identify Forward-looking Statements. Forward-looking Statements in this press release

include statements related the Company's resource properties, and the Company's plans, focus and

objectives.

Forward-looking Statements involve various risks and uncertainties and are based on certain factors

and assumptions. There can be no assurance that such statements will prove to be accurate, and actual

results and future events could differ materially from those anticipated in such statements. Important

factors that could cause actual results to differ materially from the Company's expectations include

uncertainties related to fluctuations in copper and other commodity prices, uncertainties inherent in the

exploration of mineral properties, the impact and progression of the COVID-19 pandemic and other risk

factors set forth in the Company's prospectus under the heading "Risk Factors". The Company

undertakes no obligation to update or revise any Forward-looking Statements, whether as a result of new

information, future events or otherwise, except as may be required by law. New factors emerge from time

to time, and it is not possible for Element 29 to predict all of them or assess the impact of each such

factor or the extent to which any factor, or combination of factors, may cause results to differ materially

from those contained in any Forward-looking Statement. Any Forward-looking Statements contained in

this press release are expressly qualified in their entirety by this cautionary statement

Figure 1.

Regional setting of the Flor de Cobre Project is in the Southern Peru Copper Belt, between

the Cerro Verde and Chapi mines. The project is at a moderate elevation of less than 2,700 m, is road

accessible, and is close to excellent infrastructure for mine development and operation.

To view an enhanced version of Figure 1, please visit:

https://orders.newsfilecorp.com/files/7414/126041_3979ccc8649ada3e_001full.jpg

1

The source of the historical resource estimate is a press release issued by Rio Amarillo Mining Ltd.

dated November 15, 1996 (Rio Amarillo Mining Ltd., November 15th, 1996: Aija Property Drill Results).

This historical resource is relevant to Flor de Cobre as it suggests supergene-enriched mineralization of

interest may be present at Candelaria. However, the Company cautions that the parameters,

assumptions, and methods used to calculate the historical estimate are unknown. Additionally, the

historical estimate does not use resource categories described in CIM Definition Standards for Mineral

Resources and Mineral Reserves (2014). It is also unclear what portion of this historical resource

estimate is within the current Flor de Cobre property configuration. A Qualified Person has not done

sufficient work to classify the historical estimate as a current mineral resource, and it is unclear what

work might be required to confirm the resource. For these reasons, the historical resource has not been

verified by the Company and the Company is not treating the historical estimate as a current mineral

resource.

Figure 2.

Simplified geology map of the southeastern end of the Flor de Cobre concessions illustrating

the Candelaria porphyry complex. Drill hole locations of the 2022 drill program and historical drill holes

are shown. The positions of sections containing holes FDC003, FDC004, and FDC005 are indicated

with white dashed lines.

To view an enhanced version of Figure 2, please visit:

https://orders.newsfilecorp.com/files/7414/126041_3979ccc8649ada3e_002full.jpg

Figure 3.

Section A-A' showing the position of FDC003, which is twinning historical hole CAR-190. Both

holes were collared vertically. Both holes intersected Cu oxide mineralization within the leached capping

above the enriched sulphide zone.

To view an enhanced version of Figure 3, please visit:

https://orders.newsfilecorp.com/files/7414/126041_figure3.jpg