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CHALICE MINING LIMITED Capital/Financing Update 2021

Jan 26, 2021

64649_rns_2021-01-26_a1d1fc69-3ce0-4d17-8540-7b5daa888a05.pdf

Capital/Financing Update

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27 January 2021

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Four new high-grade zones defined as Julimar continues to grow

More wide, high-grade intersections extend the G1, G2 and G4 Zones and define four new shallow high-grade zones

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Highlights

  • Ongoing step-out and resource definition drilling at the ~1.6km x >0.8km Gonneville Intrusion continues to expand the major Julimar PGE-Ni-Cu-Co-Au discovery.

  • High-grade G1-G4 Zones extended and four new internal high-grade PGE +/- Ni-Cu-Co-Au zones defined (G8-G11) :

  • G1-G2 (zones merge at depth): >690m of strike length x up to 490m of dip extent, open north along strike and down-dip;

  • G3: >465m of strike length x up to 280m of dip extent, open north along strike and down-dip;

  • G4: >1,000m of strike length x up to 430m of dip extent, open north along strike and down-dip;

  • G8: >350m of strike length x up to 250m of dip extent, wide open ;

  • G9: >350m of strike length x up to 200m of dip extent, wide open;

  • G10: >400m of strike length x up to 300m of dip extent, open north along strike and down-dip;

  • G11: >1,000m of strike length x up to 300m of dip extent, open north along strike and down-dip.

  • Significant new high-grade drill intersections (>1g/t Pd cut-off grade) include:

  • 39m @ 3.8g/t Pd , 0.6g/t Pt, 0.3% Ni , 0.2% Cu, 0.02% Co from 290m (JD023, G1 & G2 ), incl:

    • 2.0m @ 14.9g/t Pd, 0.02g/t Pt, 0.04% Ni, 0.2% Cu, 0.04% Co, and :

    • 4.5m @ 7.1g/t Pd, 1.4g/t Pt, 0.9% Ni, 0.5% Cu, 0.06% Co .

  • 34.5m @ 2.8g/t Pd, 0.7g/t Pt, 0.4g/t Au, 0.2% Ni , 1.9% Cu, 0.02% Co from 139.8m (JD019, G4 );

  • 11m @ 13.0g/t Pd, 1.3g/t Pt , 0.3g/t Au, 0.1% Ni, 0.1% Cu, 0.01% Co from 78m (JRC121, G11 ), incl: ▪ 1m @ 118g/t Pd, 8.0g/t Pt, 2.7g/t Au, 0.2% Ni, 0.1% Cu .

  • 20m @ 2.9g/t Pd, 1.5g/t Pt, 0.8g/t Au , 0.1% Ni, 0.8% Cu , 0.01% Co from 97m (JRC121; G11 ), incl:

    • 11m @ 4.0g/t Pd, 2.7g/t Pt, 1.3g/t Au, 0.2% Ni, 1.4% Cu.
  • 18m @ 4.6g/t Pd, 0.5g/t Pt, 0.4% Ni, 0.1% Cu, 0.03% Co from 121m (JRC112; G10 );

  • 17m @ 4.1g/t Pd, 0.8g/t Pt, 0.4g/t Au, 0.5% Ni, 0.3% Cu, 0.03% Co from 91m (JRC123; G11 );

  • 18m @ 3.4g/t Pd, 1.1g/t Pt , 0.1g/t Au, 0.3% Ni, 0.4% Cu, 0.15% Co from 5m (JRC087, Oxide );

  • 10.7m @ 5.0g/t Pd, 0.7g/t Pt, 0.9% Ni, 0.5% Cu , 0.04% Co from 50m (JD026, G1 );

  • 24m @ 2.1g/t Pd , 0.5g/t Pt, 0.3g/t Au, 0.2% Ni, 0.1% Cu, 0.01% Co from 134m (JRC119; G4 );

  • Assay results pending for a further 45 completed drill holes .

  • Chalice is fully funded to continue its 6-rig resource drill-out and comprehensive metallurgical testwork program at Julimar with >$130 million in cash.

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Chalice Mining

ABN 47 116 648 956 Level 2, 1292 Hay Street West Perth, Western Australia T: +61 8 9322 3960 GPO Box 2890, Perth WA 6001 F: +61 8 9322 5800

[email protected] @chalicemining www.chalicemining.com chalice-mining

Chalice Mining Limited (“Chalice” or “the Company”, ASX: CHN | OTCQB: CGMLF) is pleased to report significant new results from ongoing exploration activities at its 100%-owned Julimar Nickel-CopperPlatinum Group Element (PGE) Project , located ~70km north-east of Perth in Western Australia.

Six rigs (three Reverse Circulation (“RC”) and three diamond) are continuing the ~160,000m step-out and resource definition drill program at the ~1.6km x >0.8km Gonneville Intrusion. Reconnaissance soil sampling and Moving Loop EM programs have commenced concurrently in the Julimar State Forest to the north.

Drilling is continuing to test a range of targets across the Gonneville Intrusion, including:

  • Down-dip (western) extension of the high-grade G1, G2, G4, G5 and G6 zones (diamond and shallow RC drilling);

  • Shallow strike (southern) extensions of the high-grade G1 and G2 zones (diamond drilling);

  • Extensions of the newly defined high-grade G8-G11 zones (RC, diamond drilling); and

  • Infill resource definition drilling on an 80m x 40m grid across the Gonneville intrusion (RC, diamond drilling) – ultimately infill is expected to be on a 40m x 40m grid in order to define resources in the Indicated category.

A total of 40 diamond drill holes (including RC pre-collars with diamond tails) and 167 RC drill holes have been completed to date at the project, of which assay results have now been reported for 28 diamond and 134 RC holes (assay results are pending for a further 45 completed drill holes).

Within the 64 new drill holes reported in this announcement, there were 260 mineralised intervals (>4m width and >0.3g/t Pd cut-off grade) and 188 high-grade mineralised intervals (>2m width with >1g/t Pd cut-off grade).

Chalice Managing Director, Alex Dorsch, said: “We’ve started the New Year with strong momentum on several fronts, with drilling at our major Julimar discovery continuing to expand the high-grade footprint of the deposit and initial on-ground activities underway to test the exciting new EM targets along strike to the north.

“Drilling within the Gonneville deposit continues to deliver outstanding results and once again, we are seeing a diverse range of mineralisation styles, reflecting the sulphide-rich nature of the Gonneville Intrusion.

“We have now defined four new high-grade zones (G8-G11), each returning significant wide and highgrade intersections, which is very promising. Given the shallow nature of these zones, we expect that they may benefit future project economics.

“Meanwhile, drilling into the eastern contact of the intrusion, targeting the G4 and G11 zones, has produced some interesting results, encountering discrete pods of high-grade mineralisation interpreted as being associated with potential lows in the basal contact of the intrusion, where sulphides have deposited within the magma flow.

“Initial activities in the Julimar State Forest have commenced, and we are eagerly anticipating first results from that work over the coming weeks. The initial activities will determine the potential for Julimar to be a multi-deposit, world-class mineral province if our previously identified airborne EM anomalies develop into additional discoveries beyond Gonneville.

“With six rigs drilling and more rigs joining shortly, we are on track to meet our mid-2021 guidance for a maiden Mineral Resource for Gonneville and continue to prioritise the growth of the high-grade mineralised zones with step-out drilling. We have also commenced initial resource and pit-shell modelling, which is guiding our drill pattern.”

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Chalice Mining Limited ABN 47 116 648 956

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Figure 1. Gonneville Intrusion Plan View – new key drill results and high-grade G1-G11 zone outlines over TMI-RTP magnetics.

Figure 2 (next page). Gonneville high-grade G1-G11 zones 3D View looking North-West (approx. downdip of the high-grade zones).

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Table 1. Maximum dimensions and status of high-grade zones at Gonneville.

Zone Previous
strike extent
Previous
dip-extent
Current
strike extent
Current
dip-extent
Status
G1 450m 390m Merges with G2 at depth
G2 600m 400m 690m 490m Open down-dip and to the north
G3 465m 210m 465m 280m Open down-dip and to the north
G4 800m 430m 1000m 430m Open down-dip and to the north
G5 450m 200m 450m 270m Open down-dip
G6 300m 450m 300m 450m Open down-dip
G7 350m 500m 350m 500m Open down-dip
G8 350m 250m Open down-dip and along strike
G9 350m 200m Open down-dip and along strike
G10 400m 300m Open down-dip and to the north
G11 1000m 300m Opendown-dip andtothenorth

G1-G2 Zones

Diamond drill holes JD022 and JD023 targeted down-dip extensions of the G1 and G2 Zones. JD022 intersected several granite dykes in the interpreted G1 and G2 positions, however the G4 and G6 Zones were intersected at the anticipated target positions.

JD023 intersected several zones of mineralisation at the predicted G1-G2 target positions, where previously reported hole JD013 intersected 45.1m @ 2.9g/t Pd, 0.8g/t Pt, 0.4% Ni, 0.3% Cu, 0.03% Co ( Figure 3 ) extending the zones ~55m down-dip. The hole also intersected the G4 Zone at depth.

Significant new intersections include:

  • 8.1m @ 2.2g/t Pd, 0.2g/t Pt, 0.02g/t Au, 0.2% Ni, 0.1% Cu, 0.02% Co from 249m (JD023 - G5);

  • 39m @ 3.8g/t Pd, 0.6g/t Pt, 0.03g/t Au, 0.3% Ni, 0.2% Cu, 0.02% Co from 290m (JD023 – G1 & G2);

  • 23m @ 1.4g/t Pd, 0.2g/t Pt, 0.26g/t Au, 0.2% Ni, 0.3% Cu, 0.02% Co from 486m (JD023 - G4);

  • 11m @ 1.3g/t Pd, 0.3g/t Pt, 0.06g/t Au, 0.2% Ni, 0.3% Cu, 0.02% Co from 364m (JD022 – G6); and,

  • 22m @ 1.4g/t Pd, 0.3g/t Pt, 0.27g/t Au, 0.2% Ni, 0.5% Cu, 0.01% Co from 380m (JD022 – G4).

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Figure 3. Gonneville Cross Section ‘A’ – oblique view looking north-east +/- 25m.

JD032 was subsequently drilled ~70m down-dip of the G1-G2 intersection in JD023 and intersected an 11.6m wide zone of semi-massive to matrix sulphides from 407m ( Figure 4 ) which correlates with the downdip extension of the high-grade G1/G2 intersection reported in JD023. This demonstrates that the G2 Zone (and the Gonneville Intrusion itself) remain open down-dip. All assays for JD032 are pending.

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Figure 4. Semi-massive and matrix pyrrhotite-pentlandite-chalcopyrite sulphides over 408.9-418.6m JD032.

Diamond drill hole JD026 targeted the southern extension of the G1 and G2 zones and intersected two significant zones of shallow mineralisation including:

  • 10.7m @ 5.0g/t Pd, 0.7g/t Pt, 0.07g/t Au, 0.9% Ni, 0.5% Cu, 0.04% Co from 50m (JD026 - G1); and,

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  • 9.7m @ 1.1g/t Pd, 0.2g/t Pt, 0.01g/t Au, 0.2% Ni, 0.1% Cu, 0.02% Co from 137m (JD026 – G2).

JD026 extended the G1 and G2 zones ~100m and ~50m south respectively, and the zones remain open along strike to the south.

New G8-G11 Zones

Extensional and infill drilling has identified two additional high-grade zones (G8 and G9) in the hanging wall of the G1-G5 zones. These zones are relatively narrow and generally lower grade than the G1-G3 zones; however, they remain open both along strike and down dip.

Previous drilling between the G2 and G4 zones intersected isolated, higher grade intercepts within broad zones of disseminated mineralisation. Infill drilling has defined a generally narrow zone of high-grade mineralisation (G10) over ~400m strike and up to 300m of dip extent, subparallel to the G2 and G4 zones. Significant intersections include:

  • 18m @ 4.6g/t Pd, 0.5g/t Pt, 0.02g/t Au, 0.4% Ni, 0.1% Cu, 0.03% Co from 121m (JRC112);

  • 11m @ 1.3g/t Pd, 0.2g/t Pt, 0.01g/t Au, 0.3% Ni, 0.2% Cu, 0.03% Co from 209m (JRC129); and,

  • 7m @ 1.5g/t Pd, 0.3g/t Pt, 0.02g/t Au, 0.3% Ni, 0.1% Cu, 0.02% Co from 248m (JRC094).

A new high-grade zone (G11) has been intersected in the hanging wall of the G4 zone near the eastern footwall contact ( Figure 5 ). This zone appears to be the southern extension of a previously identified, but poorly constrained zone over a ~1km strike length. G11 is open along strike to the north and down-dip.

Significant new intersections in the new G11 Zone include:

  • 11m @ 13.0g/t Pd, 1.3g/t Pt, 0.3g/t Au, 0.1% Ni, 0.1% Cu, 0.01% Co from 78m (JRC121);

  • 20m @ 2.9g/t Pd, 1.5g/t Pt, 0.8g/t Au, 0.1% Ni, 0.8% Cu, 0.01% Co from 97m (JRC121);

  • 17m @ 4.1g/t Pd, 0.8g/t Pt, 0.4g/t Au, 0.5% Ni, 0.3% Cu, 0.03% Co from 91m (JRC123); and,

  • 27m @ 1.6g/t Pd, 1.7g/t Pt, 0.1g/t Au, 0.1% Ni, 0.04% Cu, 0.01% Co from 91m (JRC119).

Cross-cutting dolerite dykes appear more prevalent in the eastern portion of the Gonneville Intrusion. These show appreciable changes in thickness and orientation in areas of recent drilling, and therefore the interpreted continuity of mineralised zones around these dykes is poorly constrained.

Faults have also been intersected near the footwall contact and the impact of these on continuity is unknown. Additional infill drilling should help better define the impacts of dykes and faults, and improve Chalice’s understanding of the continuity of the mineralised zones in these areas.

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Figure 5. Gonneville Cross Section ‘B’ – 6,512,780mN +/- 25m.

G4 Zone

Infill drilling on a nominal 80m x 40m grid targeting mostly the shallow (eastern) section of the Gonneville intrusion has intersected mineralisation supporting the interpretation of moderately westerly dipping zones of higher-grade mineralisation within broad zones of lower grade mineralisation associated with disseminated sulphides.

Significant new intersections include:

  • 34.5m @ 2.8g/t Pd, 0.7g/t Pt, 0.37g/t Au, 0.2% Ni, 1.9% Cu, 0.02% Co from 139.8m (JD019);

  • 24m @ 2.1g/t Pd, 0.5g/t Pt, 0.3g/t Au, 0.2% Ni, 0.1% Cu, 0.01% Co from 134m (JRC119);

  • 12m @ 2.7g/t Pd, 0.8g/t Pt, 0.39g/t Au, 0.2% Ni, 0.7% Cu, 0.02% Co from 198m (JRC117);

  • 5m @ 4.2g/t Pd, 0.5g/t Pt, 0.12g/t Au, 0.7% Ni, 0.6% Cu, 0.06% Co from 100m (JRC097); and,

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• 16m @ 2.0g/t Pd, 0.4g/t Pt, 0.08g/t Au, 0.3% Ni, 0.4% Cu, 0.02% Co from 73m (JRC095).

Diamond drill hole JD019 was drilled ~30m down-dip of previously reported RC drill hole JRC089 (50m @ 1.8g/t Pd, 0.5 g/t Pt, 0.9g/t Au, 0.2% Ni, 1.1% Cu, 0.02% Cu from 112m) and intersected a similar style of disseminated, chalcopyrite-dominant, mineralisation at the interpreted G4 position near the eastern (footwall) contact of the Gonneville intrusion ( Figure 6 ).

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Figure 6. Gonneville Cross Section ‘C’ – 6,512,360mN +/- 25m.

Further drilling on section indicates that the G4 Zone narrows at depth (JRC117, 124) and up-dip (JRC088), with the shallow G4 limit apparently cut-off by post-mineralisation dolerite dykes intersected in JRC084 and JRC086.

Oxide Zones

Wide zones of shallow, high-grade PGE+/-Au mineralisation continue to be intersected in saprolitic clays developed over Gonneville ultramafic geology ( Figure 1 ). The PGE enriched oxide zone now extends over two distinct areas of ~1km x ~0.5km (south) and ~1km x ~0.15km (north).

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Significant new intersections include:

  • 18m @ 3.4g/t Pd, 1.1g/t Pt from 5m (JRC087);

  • 22m @ 1.9g/t Pd, 0.4g/t Pt from 8m (JRC092);

  • 21m @ 1.5g/t Pd, 0.4g/t Pt from 9m (JRC094);

  • 18m @ 2.2g/t Pd, 0.5g/t Pt from 7m (JRC103);

  • 23m @ 2.4g/t Pd, 0.3g/t Pt from 5m (JRC105);

  • 21m @ 2.0g/t Pd, 0.5g/t Pt from 5m (JRC112);

  • 15m @ 1.7g/t Pd, 0.3g/t Pt from 9m (JRC121); and,

  • 17m @ 2.6g/t Pd, 0.8g/t Pt from 10m (JRC122).

Initial metallurgical testwork on oxide samples to date indicates that the palladium and gold can be recovered under atmospheric oxidative leach conditions; as such, the oxide zones are considered to have significant economic potential for the Project.

Forward plan

Chalice is continuing its approach of simultaneously exploring and evaluating the zones of high-grade PGE-Ni-Cu-Co+/-Au mineralisation and the extensive PGE-Ni-Cu-Co+/-Au zones associated with disseminated sulphides within the ~1.6km x >0.8km Gonneville Intrusion.

Ongoing and planned activities at Julimar include:

  • Resource definition drilling – a ~160,000m RC/diamond drill program is underway with 3 RC and 3 diamond rigs. Drilling is initially being undertaken on an 40m x 40m spaced grid over the high-grade areas. This 40m spacing is expected to be sufficient to define Mineral Resources in the indicated category.

  • Down-hole EM Geophysics – DHEM continues to play a key role in identifying potential high-grade targets for follow-up drilling and will be completed on selected holes and in areas of wide-spaced drilling. It is important to note that the lack of an EM target does not necessarily preclude the presence of high-grade mineralisation, based on drill results received to date.

  • Metallurgical testwork – Further sulphide flotation and oxide leach testwork is underway on 200kg of composite metallurgical samples, compiled from drill samples collected from various mineralisation styles within the intrusion.

  • Geochemistry and Geochronology – the Company has engaged the Geological Survey of WA (GSWA) and a specialist consultant to conduct initial geochemical analysis and metallogenesis studies. This work aims to improve our geological and mineralogical understanding of the discovery and enhance our targeting capability as we search for similar discoveries across our large land holding in the West Yilgarn Ni-Cu-PGE Province.

  • Reconnaissance activities within the Julimar State Forest – initial wide-spaced soil sampling and Moving Loop EM programs have commenced at the Hartog EM Anomaly. Reconnaissance activities will continue over the next 1-2 months. The results of this work will assist in determining whether Julimar has the potential to host multiple Ni-Cu-PGE mineralised systems.

Authorised for release on behalf of the Company by:

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Chalice Mining Limited ABN 47 116 648 956

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Alex Dorsch Managing Director

For further information, please visit www.chalicemining.com to view our latest corporate presentation, or contact:

Corporate Enquiries Media Enquiries Alex Dorsch Nicholas Read Managing Director Principal and Managing Director Chalice Mining Limited Read Corporate Investor Relations +61 8 9322 3960 +61 8 9388 1474 [email protected] [email protected]

Follow our communications: LinkedIn: chalice-mining Twitter: @chalicemining

About the Julimar Nickel-Copper-PGE Project, Western Australia

The 100%-owned Julimar Nickel-Copper-PGE Project is located ~70km north-east of Perth on private farmland and State Forest. The Project has direct access to major highway, rail, power and port infrastructure in one of the world’s most attractive mining jurisdictions – Western Australia.

The Project was staked in 2018 as part of Chalice’s global search for high-potential nickel sulphide exploration opportunities.

Chalice interpreted the possible presence of a mafic-ultramafic layered intrusive complex (the ‘Julimar Complex’) based on high-resolution airborne magnetics. The Julimar Complex is interpreted to extend over ~26km of strike and is confirmed to be highly prospective for nickel, copper and platinum group elements ( Figure 7 ).

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Figure 7. Julimar Project tenure over regional magnetics.

Prior to Chalice’s major discovery, the Julimar Complex had never been explored for Ni-Cu-PGE mineralisation, and the lack of any bedrock geology exposures and widespread development of laterite and transported cover in the region hindered the confirmation of the conceptual geological model.

Exploration activities to date have been confined to the ~1.6km x >0.8km Gonneville Intrusion on largely Chalice owned private land only, while the access approval to the remainder of the Complex within the Julimar State Forest was pending.

Chalice commenced a systematic greenfield exploration program over the Gonneville Intrusion in mid2019. The initial drill program commenced in Q1 2020 and resulted in the discovery of shallow high-grade PGE-nickel-copper-cobalt mineralisation. The first drill hole (JRC001) intersected 19m @ 8.4g/t Pd, 1.1g/t Pt, 2.6% Ni, 1.0% Cu and 0.14% Co from 48m. The major greenfield Gonneville discovery defined the new West Yilgarn Ni-Cu-PGE Province.

The Intrusion is interpreted to be a layered mafic-ultramafic ‘sill’, with a moderate westerly dip and gentle northerly plunge. The potential ‘feeder’ for the system, a highly prospective area for high-grade mineralisation, is yet to be discovered. PGE-Ni-Cu-Co +/- Au sulphide mineralisation is widespread

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throughout the Intrusion and has been intersected down to ~850m below surface to date. The intrusion is open to the north into the Julimar State Forest and its depth extent is still unknown.

Eleven high-grade massive / matrix / heavily disseminated sulphide zones (G1-11) have been defined to date over the Intrusion. The discrete high-grade PGE-Ni-Cu-Co +/- Au zones comprise sulphide-rich accumulations (10-100% sulphide, defined by >1g/t Pd cut-off) and typically have a grade range of 1- 15g/t PGE+Au, 0.5-3.3% Ni, 0.4-4.5% Cu and 0.03-0.27% Co.

The Intrusion also hosts widespread disseminated PGE-Ni-Cu-Co mineralisation (trace to 3% on average) surrounding the high-grade zones, which typically has a grade range of 0.5-2.0g/t PGE, 0.1-0.2% Ni, 0.050.15% Cu and 0.01-0.03% Co.

Weathering at Gonneville extends down to ~30-40m below surface and a well-developed saprolite (oxide) profile after serpentinite contains elevated PGE-Au grades (typically ranging from 1.2-4.5g/t PGE+Au) from near surface to a depth of ~25m.

Early stage metallurgical testwork completed to date on selected high-grade and disseminated sulphide mineralisation samples from Gonneville has returned promising flotation results, giving initial encouragement that the sulphide-hosted mineralisation at Gonneville will be amenable to conventional flotation under standard conditions.

Tests completed on a composite of oxide mineralisation samples has also returned promising results, with the extraction of palladium and gold achieved through oxidative leaching under standard conditions.

An airborne electromagnetic (EM) survey was completed in September 2020 over the entire Julimar Complex. Three new large EM anomalies were identified – Hartog, Baudin and Jansz. The Hartog EM Anomaly extends ~6.5km directly north of the Gonneville Intrusion into the Julimar State Forest.

About Platinum Group Elements

The Platinum Group Elements (PGEs) are a group of six precious metals clustered together on the periodic table: platinum (Pt), palladium (Pd), iridium (Ir), osmium (Os), rhodium (Rh) and ruthenium (Ru).

PGEs have many desirable properties and as such have a wide variety of applications. Most notably, they are used as auto-catalysts (pollution control devices for vehicles), but are also used in jewellery, electronics, hydrogen production / purification and in hydrogen fuel cells.

Palladium is very rare and is currently one of the most valuable precious metals, with an acute supply shortage driving prices to a recent record high of US$2,856/oz in February 2020. The current spot price is approximately US$2,400/oz.

Strong demand growth (~11.5Moz in 2019[1] ) is being driven by regulations requiring increased use of the metal, particularly as an auto-catalyst in gasoline and gasoline-hybrid vehicles. The total palladium market supply from all sources in 2019 was ~10.8Moz, and >75% is sourced from mines in Russia and South Africa[1] .

1 Source: S&P Global Market Intelligence

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Competent Persons and Qualifying Persons Statement

The information in this announcement that relates to Exploration Results in relation to the Julimar Nickel-Copper-PGE Project is based on and fairly represents information and supporting documentation compiled by Dr. Kevin Frost BSc (Hons), PhD, a Competent Person, who is a Member of the Australian Institute of Geoscientists. Dr. Frost is a full-time employee of the Company and has sufficient experience that is relevant to the activity being undertaken to qualify as a Competent Person as defined in the 2012 edition of the Australasian Code for Reporting of Exploration Results, Minerals Resources and Ore Reserves, and is a Qualified Person under National Instrument 43-101 – ‘Standards of Disclosure for Mineral Projects’. The Qualified Person has verified the data disclosed in this release, including sampling, analytical and test data underlying the information contained in this release. Dr. Frost consents to the inclusion in the announcement of the matters based on his information in the form and context in which it appears.

The Information in this announcement that relates to prior exploration results for the Julimar Project is extracted from the following ASX announcements:

  • “Chalice discovers new high-grade PGE-Cu-Au zone at Julimar”, 9 July 2020

  • “Significant extension of high-grade PGE-Ni-Cu-Co zones at Julimar”, 17 August 2020

  • “Positive preliminary metallurgical results at Julimar”, 1 September 2020

  • "Major new 6.5km-long EM anomaly identified at Julimar", 22 September 2020

  • “Significant new PGE-copper-gold horizon defined at Julimar”, 6 October 2020

  • “Significant high-grade PGE-Cu-Au extensions at Julimar”, 18 November 2020

The above announcements are available to view on the Company’s website at www.chalicemining.com. The Company confirms that it is not aware of any new information or data that materially affects the exploration results included in the relevant original market announcements. The Company confirms that the form and context in which the Competent Person and Qualified Person’s findings are presented have not been materially modified from the relevant original market announcements.

Forward Looking Statements

This report may contain forward-looking information within the meaning of Canadian securities legislation and forwardlooking statements within the meaning of the United States Private Securities Litigation Reform Act of 1995 (collectively, forward-looking statements). These forward-looking statements are made as of the date of this report and Chalice Mining Limited (the Company) does not intend, and does not assume any obligation, to update these forward-looking statements.

Forward-looking statements relate to future events or future performance and reflect Company management’s expectations or beliefs regarding future events and include, but are not limited to, the Company’s strategy, the fair value of investments, the estimation of mineral reserve and mineral resources, the realisation of mineral resource estimates, the likelihood of exploration success at the Company’s projects, the prospectivity of the Company’s exploration projects, the existence of additional EM anomalies within the project, the timing of future exploration activities on the Company’s exploration projects, planned expenditures and budgets and the execution thereof, the timing and availability of drill results, potential sites for additional drilling, the timing and amount of estimated future production, costs of production, capital expenditures, success of mining operations, environmental risks, unanticipated reclamation expenses, title disputes or claims and limitations on insurance coverage.

In certain cases, forward-looking statements can be identified by the use of words such as “anticipating”, “appear”, “impact”, “plan”, “planned”, “expect”, “expected”, “extend” “indicates”, “will”, “may”, “would”, “on track”, “potential”, “pending”, “prospective”, “promising”, “occur”, or variations of such words and phrases or statements that certain actions, events or results may, could, would, might or will be taken, occur or be achieved or the negative of these terms or comparable terminology. By their very nature forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements of the Company to be materially different from any future results, performance or achievements expressed or implied by the forward-looking statements.

Such factors may include, among others, risks related to actual results of current or planned exploration activities; assay results of visually interpreted mineralised intersections; obtaining appropriate access to relevant freehold properties and the Julimar State Forest; whether geophysical anomalies are related to economic mineralisation or some other feature; obtaining access to undertake additional ground disturbing exploration work on EM anomalies located in the Julimar State Forrest; the results from testing EM anomalies; results of planned metallurgical test work; changes in project parameters as plans continue to be refined; changes in exploration programs based upon the results of exploration, future prices of mineral resources; grade or recovery rates; accidents, labour disputes and other risks of the mining

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 15

industry; delays in obtaining governmental approvals or financing or in the completion of development or construction activities; movements in the share price of investments and the timing and proceeds realised on future disposals of investments, the impact of the COVID 19 epidemic as well as those factors detailed from time to time in the Company’s interim and annual financial statements, all of which are filed and available for review on SEDAR at sedar.com, ASX at asx.com.au and OTC Markets at otcmarkets.com.

Although the Company has attempted to identify important factors that could cause actual actions, events or results to differ materially from those described in forward-looking statements, there may be other factors that cause actions, events or results not to be as anticipated, estimated or intended. There can be 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 forward-looking statements.

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 16

Appendix 1: Significant new drill intersections (>0.3g/t Pd cut-off) – Julimar Ni-Cu-PGE Project.

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
JD009 258.0 377.0 119.0 0.45 0.10 0.01 0.16 0.04 0.01 Sulphide
JD009 420.0 470.0 50.0 0.42 0.16 0.02 0.12 0.05 0.01 Sulphide
JD017 10.0 29.0 19.0 0.60 0.15 0.00 0.13 0.06 0.02 Oxide
JD017 31.0 78.0 47.0 0.63 0.12 0.03 0.14 0.12 0.02 Sulphide
Incl 63.0 66.0 3.0 1.14 0.20 0.03 0.17 0.09 0.02 Sulphide
JD017 102.0 108.0 6.0 0.33 0.08 0.01 0.09 0.05 0.01 Sulphide
JD017 120.0 228.0 108.0 0.54 0.11 0.01 0.15 0.12 0.02 Sulphide
Incl 170.0 172.0 2.0 1.53 0.12 0.07 0.47 3.18 0.07 Sulphide
JD017 232.6 252.2 19.6 0.48 0.10 0.02 0.14 0.07 0.02 Sulphide
JD017 256.5 334.7 78.2 0.57 0.12 0.01 0.14 0.07 0.02 Sulphide
Incl 300.0 302.0 2.0 1.53 0.25 0.01 0.15 0.06 0.02 Sulphide
JD017 379.1 403.4 24.4 0.58 0.14 0.02 0.15 0.07 0.01 Sulphide
Incl 389.0 393.4 4.4 1.18 0.30 0.02 0.21 0.07 0.02 Sulphide
JD017 407.6 425.9 18.3 0.74 0.22 0.02 0.20 0.09 0.02 Sulphide
Incl 412.0 418.0 6.0 1.04 0.41 0.02 0.27 0.10 0.02 Sulphide
JD017 432.9 553.8 120.9 0.50 0.11 0.02 0.16 0.08 0.02 Sulphide
JD017 559.6 564.9 5.4 0.75 0.22 0.04 0.10 0.02 0.01 Sulphide
JD019 7.3 32.1 24.8 0.76 0.23 0.02 0.17 0.11 0.04 Oxide
Incl 8.7 19.3 10.6 1.40 0.46 0.04 0.23 0.24 0.08 Oxide
JD019 32.1 108.0 75.9 0.41 0.09 0.01 0.16 0.04 0.01 Sulphide
JD019 113.0 122.0 9.0 0.34 0.09 0.01 0.17 0.02 0.01 Sulphide
JD019 127.0 131.0 4.0 0.30 0.07 0.01 0.16 0.00 0.02 Sulphide
JD019 139.8 174.3 34.5 2.81 0.73 0.37 0.18 1.88 0.02 Sulphide
JD020 5.0 26.0 21.0 0.68 0.04 0.00 0.04 0.07 0.01 Oxide
JD020 67.2 125.0 57.8 0.89 0.22 0.05 0.15 0.12 0.01 Sulphide
Incl 73.1 86.3 13.2 2.10 0.55 0.16 0.23 0.26 0.02 Sulphide
JD020 131.0 193.0 62.0 0.85 0.15 0.03 0.17 0.14 0.01 Sulphide
Incl 145.0 147.0 2.0 2.80 0.11 0.09 0.31 1.26 0.03 Sulphide
and 172.0 174.0 2.0 1.62 0.19 0.13 0.24 0.16 0.02 Sulphide
and 178.0 185.0 7.0 2.22 0.24 0.03 0.21 0.31 0.02 Sulphide
JD021 9.8 37.0 27.2 0.96 0.24 0.01 0.12 0.09 0.02 Oxide
Incl 12.8 22.8 10.0 1.68 0.40 0.01 0.18 0.16 0.05 Oxide
JD021 37.0 125.0 88.0 0.68 0.13 0.01 0.18 0.09 0.02 Sulphide
Incl 45.0 48.0 3.0 1.08 0.24 0.00 0.23 0.16 0.02 Sulphide
and 71.6 73.8 2.2 4.17 0.44 0.05 1.11 1.02 0.08 Sulphide
JD021 132.0 147.0 15.0 0.40 0.08 0.01 0.18 0.07 0.02 Sulphide
JD021 203.0 215.0 12.0 0.68 0.19 0.02 0.11 0.03 0.01 Sulphide
Incl 209.0 213.0 4.0 1.23 0.34 0.04 0.13 0.04 0.01 Sulphide
JD022 124.0 145.0 21.0 0.70 0.16 0.01 0.19 0.13 0.02 Sulphide
Incl 125.0 127.0 2.0 2.36 0.51 0.02 0.40 0.68 0.03 Sulphide
JD022 173.0 179.4 6.4 0.89 0.08 0.02 0.19 0.57 0.02 Sulphide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 17

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
JD022 203.0 213.0 10.0 0.45 0.13 0.00 0.13 0.02 0.01 Sulphide
JD022 218.0 230.0 12.0 0.34 0.12 0.01 0.13 0.02 0.01 Sulphide
JD022 235.0 246.8 11.8 0.51 0.16 0.01 0.13 0.03 0.01 Sulphide
JD022 258.4 287.0 28.6 0.49 0.14 0.01 0.16 0.03 0.02 Sulphide
JD022 305.6 438.1 132.5 0.70 0.18 0.06 0.15 0.16 0.01 Sulphide
Incl 364.0 375.0 11.0 1.25 0.27 0.06 0.17 0.28 0.02 Sulphide
and 380.0 402.0 22.0 1.41 0.33 0.27 0.15 0.53 0.01 Sulphide
and 436.0 438.1 2.1 1.33 0.72 0.19 0.11 0.04 0.01 Sulphide
JD023 10.0 34.8 24.8 0.67 0.14 0.01 0.12 0.12 0.02 Oxide
Incl 15.0 18.8 3.8 1.16 0.27 0.01 0.10 0.13 0.03 Oxide
JD023 34.8 96.0 61.2 0.69 0.15 0.06 0.15 0.16 0.02 Sulphide
Incl 48.0 50.0 2.0 1.22 0.22 0.04 0.18 0.12 0.02 Sulphide
and 60.9 63.0 2.1 1.13 0.20 0.04 0.20 0.19 0.02 Sulphide
and 71.0 74.0 3.0 1.15 0.20 0.05 0.22 0.12 0.02 Sulphide
JD023 148.5 284.5 136.0 0.73 0.13 0.01 0.16 0.07 0.02 Sulphide
Incl 208.0 211.0 3.0 1.24 0.16 0.01 0.22 0.31 0.03 Sulphide
and 218.0 222.0 4.0 1.03 0.25 0.02 0.16 0.08 0.02 Sulphide
and 249.0 257.1 8.1 2.23 0.22 0.02 0.18 0.09 0.02 Sulphide
JD023 288.9 333.0 44.2 3.38 0.56 0.02 0.30 0.24 0.02 Sulphide
Incl 290.0 329.0 39.0 3.76 0.63 0.03 0.33 0.23 0.02 Sulphide
JD023 344.0 355.9 11.9 0.63 0.25 0.03 0.14 0.64 0.01 Sulphide
Incl 344.0 347.0 3.0 1.31 0.74 0.04 0.15 0.60 0.01 Sulphide
JD023 382.8 451.0 68.2 0.50 0.12 0.01 0.18 0.06 0.01 Sulphide
JD023 474.0 509.3 35.4 1.07 0.20 0.18 0.16 0.22 0.02 Sulphide
Incl 486.0 509.0 23.0 1.37 0.24 0.26 0.17 0.33 0.02 Sulphide
JD026 47.0 61.0 14.0 3.85 0.56 0.06 0.67 0.41 0.04 Sulphide
Incl 50.0 60.7 10.7 4.95 0.73 0.07 0.86 0.52 0.04 Sulphide
JD026 69.3 88.0 18.7 0.92 0.41 0.05 0.24 0.29 0.02 Sulphide
Incl 72.0 76.3 4.3 3.04 1.60 0.16 0.76 0.90 0.04 Sulphide
JD026 93.0 97.0 4.0 0.32 0.06 0.01 0.16 0.04 0.02 Sulphide
JD026 125.0 159.4 34.4 0.73 0.18 0.01 0.18 0.08 0.02 Sulphide
Incl 129.0 131.0 2.0 1.13 0.32 0.01 0.25 0.14 0.03 Sulphide
and 137.0 146.7 9.7 1.13 0.24 0.01 0.20 0.13 0.02 Sulphide
JRC006D 185.8 247.0 61.2 0.63 0.11 0.04 0.18 0.04 0.02 Sulphide
JRC006D 284.7 297.0 12.3 0.65 0.14 0.06 0.14 0.20 0.01 Sulphide
JRC081 1.0 22.0 21.0 1.40 0.45 0.03 0.27 0.23 0.06 Oxide
Incl 3.0 12.0 9.0 2.35 0.58 0.06 0.27 0.34 0.09 Oxide
JRC081 37.0 45.0 8.0 0.66 0.17 0.01 0.18 0.05 0.02 Sulphide
JRC081 54.0 126.0 72.0 0.58 0.14 0.01 0.17 0.03 0.02 Sulphide
Incl 95.0 103.0 8.0 1.18 0.28 0.02 0.20 0.03 0.02 Sulphide
JRC082 14.0 25.0 11.0 0.71 0.20 0.01 0.12 0.09 0.02 Oxide
JRC082 26.0 33.0 7.0 0.35 0.07 0.01 0.21 0.06 0.02 Sulphide
JRC082 40.0 83.0 43.0 0.63 0.14 0.01 0.13 0.06 0.01 Sulphide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 18

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
JRC082 96.0 113.0 17.0 0.60 0.13 0.03 0.16 0.06 0.01 Sulphide
Incl 103.0 106.0 3.0 1.13 0.23 0.07 0.21 0.17 0.02 Sulphide
JRC082 120.0 237.0 117.0 0.57 0.12 0.01 0.15 0.07 0.01 Sulphide
Incl 126.0 131.0 5.0 1.32 0.27 0.03 0.16 0.07 0.02 Sulphide
JRC082 253.0 264.0 11.0 0.40 0.08 0.01 0.13 0.04 0.01 Sulphide
JRC083 1.0 20.0 19.0 1.54 0.40 0.02 0.12 0.14 0.10 Oxide
Incl 3.0 11.0 8.0 2.70 0.58 0.03 0.14 0.25 0.20 Oxide
JRC083 25.0 30.0 5.0 0.53 0.14 0.02 0.12 0.05 0.01 Oxide
JRC083 35.0 80.0 45.0 0.47 0.10 0.01 0.15 0.04 0.02 Sulphide
Incl 49.0 52.0 3.0 2.13 0.33 0.01 0.55 0.08 0.05 Sulphide
JRC083 99.0 235.0 136.0 0.73 0.14 0.01 0.18 0.09 0.02 Sulphide
Incl 149.0 155.0 6.0 4.01 0.60 0.08 0.54 0.58 0.03 Sulphide
and 168.0 171.0 3.0 1.18 0.26 0.03 0.29 0.38 0.04 Sulphide
JRC084 3.0 14.0 11.0 0.39 0.06 0.01 0.05 0.13 0.03 Oxide
JRC085A 6.0 23.0 17.0 1.34 0.23 0.02 0.16 0.21 0.06 Oxide
Incl 8.0 18.0 10.0 1.91 0.27 0.03 0.20 0.27 0.09 Oxide
JRC085A 39.0 48.0 9.0 0.40 0.09 0.01 0.10 0.06 0.01 Sulphide
JRC085A 63.0 124.0 61.0 0.56 0.12 0.02 0.16 0.08 0.01 Sulphide
Incl 116.0 118.0 2.0 1.49 0.31 0.01 0.45 0.18 0.03 Sulphide
JRC086 10.0 30.0 20.0 0.81 0.30 0.02 0.24 0.18 0.08 Oxide
Incl 16.0 22.0 6.0 1.37 0.31 0.03 0.35 0.28 0.13 Oxide
JRC087 2.0 31.0 29.0 2.32 0.74 0.06 0.21 0.26 0.10 Oxide
Incl 5.0 23.0 18.0 3.37 1.08 0.08 0.28 0.38 0.15 Oxide
JRC087 31.0 38.0 7.0 1.55 0.26 0.01 0.19 0.18 0.02 Sulphide
Incl 32.0 34.0 2.0 4.17 0.58 0.03 0.35 0.52 0.03 Sulphide
JRC087 63.0 193.0 130.0 0.57 0.13 0.02 0.17 0.09 0.02 Sulphide
JRC087 200.0 230.0 30.0 0.47 0.10 0.02 0.16 0.10 0.02 Sulphide
JRC088 7.0 19.0 12.0 0.70 0.20 0.02 0.10 0.12 0.04 Oxide
JRC088 51.0 73.0 22.0 0.55 0.10 0.02 0.29 0.19 0.02 Sulphide
Incl 56.0 60.0 4.0 1.25 0.17 0.06 0.85 0.77 0.07 Sulphide
JRC088 78.0 98.0 20.0 0.49 0.20 0.03 0.13 0.10 0.01 Sulphide
JRC088 108.0 113.0 5.0 1.50 0.39 0.42 0.14 0.69 0.01 Sulphide
JRC088 119.0 136.0 17.0 0.84 0.18 0.15 0.13 0.35 0.01 Sulphide
Incl 127.0 136.0 9.0 1.12 0.29 0.20 0.15 0.48 0.01 Sulphide
JRC090 4.0 27.0 23.0 0.92 0.16 0.14 0.24 0.21 0.04 Oxide
Incl 6.0 11.0 5.0 1.71 0.24 0.18 0.22 0.24 0.08 Oxide
and 17.0 21.0 4.0 1.18 0.24 0.24 0.36 0.40 0.05 Oxide
JRC090 27.0 123.0 96.0 0.50 0.12 0.03 0.16 0.03 0.01 Sulphide
JRC090 147.0 174.0 27.0 0.45 0.11 0.01 0.16 0.02 0.01 Sulphide
JRC090 204.0 213.0 9.0 0.30 0.09 0.01 0.15 0.01 0.01 Sulphide
JRC090 217.0 226.0 9.0 0.44 0.11 0.01 0.15 0.07 0.02 Sulphide
JRC091 9.0 35.0 26.0 1.50 0.48 0.18 0.15 0.31 0.05 Oxide
Incl 12.0 23.0 11.0 2.39 0.77 0.29 0.21 0.39 0.09 Oxide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 19

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
and 29.0 35.0 6.0 1.26 0.34 0.07 0.15 0.35 0.02 Oxide
JRC091 35.0 45.0 10.0 0.42 0.09 0.02 0.17 0.11 0.02 Sulphide
JRC091A 10.0 30.0 20.0 1.35 0.37 0.14 0.13 0.29 0.03 Oxide
Incl 11.0 18.0 7.0 2.54 0.62 0.14 0.18 0.33 0.06 Oxide
JRC092 4.0 31.0 27.0 1.63 0.39 0.04 0.16 0.18 0.04 Oxide
Incl 8.0 30.0 22.0 1.86 0.43 0.05 0.18 0.20 0.05 Oxide
JRC092 38.0 93.0 55.0 0.88 0.19 0.03 0.16 0.20 0.02 Sulphide
Incl 47.0 63.0 16.0 1.11 0.24 0.06 0.20 0.21 0.02 Sulphide
and 79.0 93.0 14.0 1.08 0.23 0.03 0.15 0.11 0.02 Sulphide
JRC092 105.0 112.0 7.0 0.41 0.09 0.00 0.12 0.13 0.01 Sulphide
JRC092 119.0 175.0 56.0 0.81 0.15 0.01 0.13 0.05 0.01 Sulphide
Incl 120.0 126.0 6.0 2.91 0.42 0.01 0.14 0.04 0.01 Sulphide
and 156.0 165.0 9.0 1.26 0.22 0.02 0.19 0.09 0.02 Sulphide
JRC092 192.0 225.0 33.0 0.52 0.12 0.02 0.14 0.14 0.01 Sulphide
Incl 214.0 216.0 2.0 1.26 0.26 0.06 0.25 0.26 0.02 Sulphide
and 218.0 220.0 2.0 1.11 0.26 0.10 0.15 0.99 0.01 Sulphide
JRC093 4.0 19.0 15.0 0.52 0.06 0.01 0.05 0.10 0.01 Oxide
JRC094 8.0 33.0 25.0 1.35 0.39 0.06 0.14 0.20 0.05 Oxide
Incl 9.0 30.0 21.0 1.51 0.42 0.06 0.15 0.22 0.06 Oxide
JRC094 33.0 66.0 33.0 0.48 0.10 0.01 0.13 0.07 0.01 Sulphide
JRC094 90.0 119.0 29.0 0.51 0.11 0.01 0.14 0.07 0.02 Sulphide
Incl 93.0 95.0 2.0 1.17 0.27 0.02 0.22 0.21 0.02 Sulphide
JRC094 127.0 140.0 13.0 0.98 0.17 0.03 0.16 0.17 0.02 Sulphide
Incl 133.0 137.0 4.0 2.09 0.34 0.03 0.25 0.36 0.02 Sulphide
JRC094 147.0 202.0 55.0 0.49 0.12 0.01 0.14 0.07 0.02 Sulphide
Incl 147.0 150.0 3.0 1.20 0.32 0.07 0.22 0.18 0.02 Sulphide
JRC094 224.0 256.0 32.0 0.73 0.14 0.01 0.20 0.06 0.02 Sulphide
Incl 248.0 255.0 7.0 1.47 0.28 0.02 0.35 0.05 0.02 Sulphide
JRC095 10.0 24.0 14.0 0.95 0.72 0.02 0.20 0.20 0.08 Oxide
Incl 14.0 20.0 6.0 1.35 1.18 0.02 0.22 0.25 0.12 Oxide
JRC095 39.0 95.0 56.0 0.89 0.20 0.05 0.19 0.16 0.02 Sulphide
Incl 73.0 89.0 16.0 1.98 0.44 0.08 0.32 0.38 0.02 Sulphide
JRC095 101.0 121.0 20.0 0.33 0.08 0.02 0.14 0.04 0.01 Sulphide
JRC096 44.0 50.0 6.0 0.42 0.08 0.01 0.14 0.13 0.01 Sulphide
JRC096 60.0 193.0 133.0 0.61 0.13 0.02 0.13 0.08 0.01 Sulphide
Incl 84.0 86.0 2.0 1.30 0.23 0.02 0.18 0.09 0.02 Sulphide
and 119.0 124.0 5.0 1.14 0.22 0.01 0.15 0.06 0.01 Sulphide
and 144.0 147.0 3.0 1.13 0.20 0.24 0.17 0.58 0.02 Sulphide
and 152.0 154.0 2.0 1.05 0.18 0.03 0.19 0.11 0.02 Sulphide
and 178.0 180.0 2.0 1.48 0.29 0.06 0.17 0.14 0.02 Sulphide
JRC097 9.0 28.0 19.0 1.05 0.33 0.03 0.18 0.17 0.05 Oxide
Incl 9.0 22.0 13.0 1.24 0.43 0.03 0.19 0.20 0.07 Oxide
JRC097 28.0 71.0 43.0 0.44 0.10 0.01 0.16 0.02 0.01 Sulphide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 20

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
JRC097 82.0 111.0 29.0 1.08 0.16 0.03 0.22 0.13 0.02 Sulphide
Incl 100.0 105.0 5.0 4.21 0.49 0.12 0.71 0.58 0.06 Sulphide
JRC098 12.0 20.0 8.0 0.46 0.10 0.08 0.19 0.07 0.01 Oxide
JRC098 41.0 53.0 12.0 0.46 0.09 0.03 0.16 0.02 0.01 Sulphide
JRC098 82.0 95.0 13.0 0.44 0.10 0.01 0.15 0.02 0.01 Sulphide
JRC098 108.0 155.0 47.0 0.52 0.15 0.02 0.12 0.07 0.01 Sulphide
Incl 116.0 122.0 6.0 1.67 0.58 0.04 0.11 0.07 0.01 Sulphide
JRC098 162.0 194.0 32.0 0.43 0.11 0.03 0.13 0.07 0.01 Sulphide
JRC099 28.0 41.0 13.0 0.44 0.10 0.02 0.09 0.05 0.01 Oxide
JRC099 41.0 98.0 57.0 0.55 0.11 0.04 0.15 0.04 0.01 Sulphide
Incl 46.0 48.0 2.0 1.14 0.22 0.01 0.18 0.02 0.02 Sulphide
JRC099 105.0 131.0 26.0 0.67 0.15 0.03 0.17 0.10 0.02 Sulphide
JRC099 149.0 175.0 26.0 0.48 0.10 0.01 0.15 0.08 0.02 Sulphide
JRC099 180.0 206.0 26.0 0.56 0.11 0.01 0.15 0.06 0.02 Sulphide
JRC099 211.0 276.0 65.0 0.45 0.10 0.01 0.14 0.06 0.02 Sulphide
JRC100 4.0 26.0 22.0 0.84 0.22 0.03 0.18 0.13 0.04 Oxide
Incl 8.0 15.0 7.0 1.52 0.37 0.04 0.24 0.27 0.09 Oxide
JRC100 26.0 125.0 99.0 0.55 0.11 0.02 0.16 0.03 0.01 Sulphide
Incl 72.0 74.0 2.0 1.05 0.22 0.03 0.21 0.05 0.02 Sulphide
JRC100 130.0 156.0 26.0 0.59 0.15 0.02 0.15 0.10 0.02 Sulphide
JRC100 192.0 200.0 8.0 0.44 0.13 0.10 0.12 0.05 0.02 Sulphide
JRC100 206.0 215.0 9.0 0.79 0.19 0.14 0.10 0.12 0.01 Sulphide
JRC100A 7.0 24.0 17.0 0.98 0.24 0.03 0.20 0.16 0.04 Oxide
Incl 8.0 15.0 7.0 1.61 0.32 0.04 0.25 0.29 0.07 Oxide
JRC102 2.0 33.0 31.0 1.10 0.24 0.06 0.12 0.14 0.03 Oxide
Incl 11.0 32.0 21.0 1.32 0.31 0.05 0.16 0.17 0.04 Oxide
JRC102 33.0 42.0 9.0 0.69 0.16 0.02 0.16 0.06 0.02 Sulphide
JRC102 56.0 173.0 117.0 0.58 0.13 0.01 0.14 0.07 0.02 Sulphide
Incl 151.0 154.0 3.0 1.06 0.19 0.01 0.18 0.08 0.02 Sulphide
JRC102 178.0 211.0 33.0 0.39 0.09 0.00 0.13 0.05 0.01 Sulphide
JRC102 222.0 230.0 8.0 0.35 0.08 0.00 0.14 0.05 0.01 Sulphide
JRC102 240.0 251.0 11.0 0.40 0.08 0.00 0.12 0.06 0.01 Sulphide
JRC102 265.0 273.0 8.0 0.47 0.10 0.00 0.13 0.01 0.01 Sulphide
JRC103 4.0 30.0 26.0 1.74 0.42 0.06 0.09 0.12 0.04 Oxide
Incl 7.0 25.0 18.0 2.25 0.49 0.04 0.07 0.13 0.05 Oxide
JRC103 30.0 121.0 91.0 0.78 0.16 0.01 0.18 0.09 0.02 Sulphide
Incl 64.0 68.0 4.0 1.77 0.33 0.01 0.28 0.13 0.03 Sulphide
and 97.0 106.0 9.0 1.20 0.23 0.01 0.22 0.12 0.02 Sulphide
and 113.0 115.0 2.0 1.73 0.34 0.01 0.18 0.23 0.02 Sulphide
JRC103 127.0 133.0 6.0 0.59 0.15 0.00 0.16 0.08 0.02 Sulphide
Incl 127.0 129.0 2.0 1.33 0.34 0.01 0.33 0.20 0.04 Sulphide
JRC103 182.0 186.0 4.0 0.63 0.13 0.00 0.14 0.05 0.01 Sulphide
JRC103 194.0 199.0 5.0 0.42 0.08 0.00 0.14 0.03 0.01 Sulphide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 21

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
JRC103 204.0 286.0 82.0 0.58 0.14 0.00 0.14 0.06 0.01 Sulphide
Incl 266.0 279.0 13.0 1.13 0.29 0.01 0.22 0.11 0.02 Sulphide
JRC104 0.0 29.0 29.0 1.49 0.41 0.02 0.17 0.17 0.04 Oxide
Incl 2.0 21.0 19.0 1.72 0.45 0.02 0.11 0.18 0.04 Oxide
and 26.0 29.0 3.0 2.24 0.62 0.03 0.51 0.27 0.04 Oxide
JRC104 54.0 60.0 6.0 0.43 0.10 0.01 0.14 0.04 0.01 Sulphide
JRC104 164.0 185.0 21.0 0.87 0.19 0.06 0.12 0.18 0.01 Sulphide
Incl 175.0 181.0 6.0 2.06 0.48 0.15 0.13 0.36 0.01 Sulphide
JRC105 4.0 31.0 27.0 2.12 0.32 0.03 0.30 0.25 0.06 Oxide
Incl 5.0 28.0 23.0 2.38 0.34 0.04 0.33 0.28 0.06 Oxide
JRC105 31.0 69.0 38.0 0.34 0.12 0.01 0.12 0.05 0.01 Sulphide
JRC105 78.0 147.0 69.0 0.55 0.13 0.02 0.17 0.08 0.01 Sulphide
JRC105 169.0 221.0 52.0 0.71 0.19 0.05 0.15 0.15 0.02 Sulphide
Incl 176.0 183.0 7.0 2.59 0.85 0.13 0.16 0.38 0.01 Sulphide
JRC105 232.0 259.0 27.0 1.16 0.55 0.11 0.15 0.08 0.02 Sulphide
Incl 232.0 237.0 5.0 1.42 0.34 0.09 0.13 0.07 0.01 Sulphide
and 247.0 259.0 12.0 1.49 0.90 0.15 0.20 0.13 0.02 Sulphide
JRC106 6.0 26.0 20.0 1.59 0.44 0.01 0.08 0.18 0.04 Oxide
Incl 11.0 26.0 15.0 1.91 0.58 0.02 0.10 0.22 0.05 Oxide
JRC106 26.0 173.0 147.0 0.49 0.11 0.00 0.14 0.07 0.01 Sulphide
JRC106 198.0 251.0 53.0 0.43 0.09 0.01 0.13 0.06 0.01 Sulphide
JRC107 7.0 32.0 25.0 1.50 0.27 0.04 0.17 0.13 0.07 Oxide
Incl 8.0 18.0 10.0 2.04 0.40 0.06 0.19 0.22 0.16 Oxide
JRC107 32.0 123.0 91.0 0.73 0.16 0.03 0.16 0.10 0.01 Sulphide
Incl 99.0 112.0 13.0 2.24 0.54 0.05 0.27 0.16 0.02 Sulphide
and 118.0 121.0 3.0 2.83 0.36 0.07 0.19 0.90 0.02 Sulphide
JRC108 7.0 30.0 23.0 1.55 0.43 0.09 0.14 0.19 0.06 Oxide
Incl 12.0 24.0 12.0 2.38 0.74 0.09 0.15 0.22 0.04 Oxide
JRC108 30.0 72.0 42.0 0.82 0.21 0.03 0.12 0.03 0.01 Sulphide
Incl 50.0 52.0 2.0 1.74 0.61 0.06 0.11 0.02 0.01 Sulphide
and 59.0 71.0 12.0 1.68 0.40 0.04 0.12 0.03 0.01 Sulphide
JRC108 84.0 110.0 26.0 0.36 0.09 0.02 0.13 0.05 0.01 Sulphide
JRC108 130.0 132.0 2.0 7.69 1.05 0.14 1.10 0.15 0.09 Sulphide
JRC108 152.0 173.0 21.0 0.86 0.19 0.04 0.14 0.06 0.01 Sulphide
Incl 158.0 162.0 4.0 2.17 0.42 0.07 0.24 0.20 0.02 Sulphide
and 168.0 170.0 2.0 1.16 0.27 0.03 0.18 0.05 0.01 Sulphide
JRC109 6.0 31.0 25.0 1.33 0.23 0.01 0.06 0.09 0.04 Oxide
Incl 8.0 20.0 12.0 2.09 0.29 0.00 0.06 0.11 0.05 Oxide
and 26.0 29.0 3.0 1.13 0.08 0.01 0.10 0.14 0.02 Oxide
JRC109 31.0 61.0 30.0 0.54 0.10 0.00 0.11 0.08 0.01 Sulphide
JRC109 68.0 103.0 35.0 0.49 0.10 0.00 0.14 0.05 0.01 Sulphide
JRC109 109.0 204.0 95.0 0.50 0.11 0.01 0.16 0.07 0.01 Sulphide
Incl 193.0 195.0 2.0 2.47 0.25 0.07 0.34 0.85 0.03 Sulphide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 22

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
JRC109 251.0 258.0 7.0 0.76 0.22 0.01 0.14 0.03 0.01 Sulphide
Incl 255.0 257.0 2.0 1.16 0.44 0.01 0.13 0.02 0.01 Sulphide
JRC110 10.0 32.0 22.0 1.44 0.72 0.04 0.17 0.14 0.08 Oxide
Incl 11.0 22.0 11.0 2.32 1.29 0.06 0.19 0.22 0.14 Oxide
JRC110 32.0 64.0 32.0 0.43 0.18 0.02 0.12 0.04 0.01 Sulphide
JRC110 81.0 108.0 27.0 0.50 0.10 0.03 0.16 0.07 0.02 Sulphide
JRC110 143.0 155.0 12.0 1.94 0.97 0.06 0.26 0.12 0.02 Sulphide
Incl 144.0 154.0 10.0 2.15 1.13 0.06 0.28 0.12 0.02 Sulphide
JRC111 9.0 33.0 24.0 1.45 0.16 0.02 0.18 0.17 0.03 Oxide
Incl 14.0 27.0 13.0 2.17 0.27 0.03 0.19 0.24 0.03 Oxide
JRC111 66.0 125.0 59.0 0.43 0.09 0.02 0.15 0.05 0.01 Sulphide
JRC111 142.0 163.0 21.0 0.58 0.31 0.03 0.14 0.13 0.01 Sulphide
JRC112 0.0 32.0 32.0 1.52 0.41 0.01 0.17 0.17 0.03 Oxide
Incl 5.0 26.0 21.0 2.04 0.48 0.02 0.20 0.22 0.05 Oxide
JRC112 32.0 66.0 34.0 0.56 0.12 0.01 0.15 0.10 0.02 Sulphide
JRC112 97.0 169.0 72.0 1.45 0.20 0.01 0.19 0.06 0.02 Sulphide
Incl 121.0 139.0 18.0 4.57 0.53 0.02 0.36 0.12 0.03 Sulphide
JRC112 198.0 248.0 50.0 0.46 0.11 0.01 0.14 0.07 0.01 Sulphide
JRC113 78.0 88.0 10.0 0.50 0.09 0.02 0.16 0.10 0.01 Sulphide
JRC113 103.0 120.0 17.0 0.61 0.15 0.01 0.12 0.06 0.01 Sulphide
Incl 111.0 114.0 3.0 1.11 0.39 0.02 0.19 0.09 0.02 Sulphide
JRC113 135.0 153.0 18.0 0.62 0.18 0.02 0.14 0.07 0.01 Sulphide
Incl 141.0 143.0 2.0 1.20 0.58 0.02 0.11 0.09 0.01 Sulphide
JRC114 9.0 38.0 29.0 0.88 0.31 0.01 0.17 0.13 0.04 Oxide
Incl 13.0 26.0 13.0 1.36 0.47 0.02 0.19 0.21 0.07 Oxide
JRC114 38.0 49.0 11.0 0.39 0.08 0.00 0.16 0.02 0.01 Sulphide
JRC114 54.0 81.0 27.0 0.35 0.08 0.00 0.15 0.03 0.02 Sulphide
JRC114 106.0 150.0 44.0 0.96 0.22 0.03 0.21 0.19 0.02 Sulphide
Incl 106.0 111.0 5.0 2.11 0.34 0.01 0.53 0.16 0.04 Sulphide
and 120.0 125.0 5.0 1.15 0.22 0.04 0.22 0.11 0.02 Sulphide
and 137.0 143.0 6.0 1.59 0.46 0.04 0.32 0.47 0.02 Sulphide
JRC114 165.0 175.0 10.0 0.61 0.13 0.03 0.19 0.15 0.02 Sulphide
JRC114 206.0 233.0 27.0 0.42 0.12 0.02 0.10 0.05 0.01 Sulphide
Incl 211.0 215.0 4.0 1.32 0.31 0.03 0.09 0.02 0.01 Sulphide
JRC114 238.0 244.0 6.0 0.61 0.23 0.02 0.09 0.03 0.01 Sulphide
JRC115 13.0 33.0 20.0 0.94 0.34 0.00 0.23 0.13 0.05 Oxide
Incl 16.0 27.0 11.0 1.17 0.44 0.00 0.30 0.15 0.07 Oxide
JRC115 33.0 122.0 89.0 0.61 0.12 0.01 0.18 0.10 0.02 Sulphide
Incl 55.0 57.0 2.0 1.69 0.18 0.01 0.79 0.23 0.06 Sulphide
and 102.0 106.0 4.0 1.10 0.21 0.02 0.32 0.17 0.03 Sulphide
JRC115 242.0 279.0 37.0 0.35 0.11 0.02 0.12 0.06 0.01 Sulphide
JRC116 48.0 52.0 4.0 0.32 0.06 0.01 0.14 0.26 0.01 Sulphide
JRC117 6.0 32.0 26.0 0.84 0.30 0.02 0.23 0.13 0.06 Oxide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 23

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
Incl 7.0 19.0 12.0 1.24 0.47 0.02 0.28 0.19 0.09 Oxide
JRC117 33.0 41.0 8.0 0.41 0.09 0.01 0.16 0.02 0.02 Sulphide
JRC117 91.0 210.0 119.0 0.71 0.18 0.06 0.16 0.18 0.01 Sulphide
Incl 128.0 130.0 2.0 1.08 0.20 0.02 0.29 0.14 0.03 Sulphide
and 189.0 192.0 3.0 1.72 0.31 0.19 0.22 2.01 0.02 Sulphide
and 198.0 210.0 12.0 2.70 0.81 0.39 0.18 0.71 0.02 Sulphide
JRC118 10.0 34.0 24.0 0.58 0.16 0.01 0.14 0.12 0.03 Oxide
JRC118 34.0 62.0 28.0 0.47 0.12 0.01 0.16 0.08 0.01 Sulphide
JRC118 132.0 136.0 4.0 0.75 0.17 0.01 0.08 0.05 0.01 Sulphide
Incl 134.0 136.0 2.0 1.17 0.26 0.02 0.12 0.07 0.01 Sulphide
JRC118 142.0 157.0 15.0 0.40 0.09 0.02 0.12 0.02 0.01 Sulphide
JRC118 199.0 212.0 13.0 0.36 0.07 0.01 0.10 0.03 0.01 Sulphide
JRC118 217.0 222.0 5.0 0.60 0.30 0.09 0.09 0.03 0.01 Sulphide
JRC119 10.0 30.0 20.0 0.82 0.29 0.01 0.20 0.08 0.07 Oxide
Incl 15.0 18.0 3.0 1.28 0.63 0.01 0.21 0.16 0.20 Oxide
JRC119 30.0 119.0 89.0 0.92 0.61 0.06 0.13 0.06 0.01 Sulphide
Incl 39.0 41.0 2.0 1.64 0.62 0.02 0.13 0.05 0.01 Sulphide
and 76.0 79.0 3.0 2.25 0.14 0.12 0.41 0.15 0.04 Sulphide
and 91.0 118.0 27.0 1.56 1.66 0.13 0.11 0.04 0.01 Sulphide
JRC119 129.0 181.0 52.0 1.33 0.36 0.18 0.13 0.09 0.01 Sulphide
Incl 134.0 158.0 24.0 2.09 0.49 0.30 0.16 0.13 0.01 Sulphide
and 170.0 173.0 3.0 1.01 0.18 0.08 0.13 0.08 0.02 Sulphide
JRC120 7.0 24.0 17.0 1.27 0.32 0.04 0.24 0.17 0.06 Oxide
Incl 8.0 17.0 9.0 1.73 0.39 0.05 0.27 0.24 0.08 Oxide
JRC120 24.0 71.0 47.0 0.41 0.09 0.01 0.15 0.04 0.01 Sulphide
JRC120 77.0 104.0 27.0 0.46 0.13 0.01 0.17 0.03 0.01 Sulphide
JRC120 118.0 285.0 167.0 0.64 0.16 0.04 0.18 0.09 0.02 Sulphide
Incl 118.0 120.0 2.0 4.72 0.89 0.19 1.53 0.57 0.18 Sulphide
and 192.0 194.0 2.0 1.60 0.59 0.10 0.37 0.71 0.05 Sulphide
and 215.0 230.0 15.0 1.24 0.35 0.06 0.26 0.30 0.02 Sulphide
and 262.0 264.0 2.0 2.27 0.82 0.76 0.13 0.55 0.02 Sulphide
and 273.0 281.0 8.0 1.59 0.29 0.07 0.11 0.11 0.01 Sulphide
JRC121 9.0 24.0 15.0 1.73 0.29 0.01 0.13 0.09 0.10 Oxide
Incl 13.0 24.0 11.0 2.15 0.38 0.01 0.16 0.11 0.14 Oxide
JRC121 24.0 120.0 96.0 2.58 0.62 0.22 0.15 0.26 0.07 Sulphide
Incl 24.0 36.0 12.0 1.50 0.68 0.01 0.25 0.27 0.46 Sulphide
and 78.0 89.0 11.0 12.95 1.28 0.34 0.14 0.12 0.01 Sulphide
and 97.0 117.0 20.0 2.95 1.53 0.79 0.15 0.85 0.01 Sulphide
JRC121 129.0 147.0 18.0 0.61 0.16 0.16 0.08 0.13 0.01 Sulphide
JRC121 183.0 197.0 14.0 0.98 0.46 0.19 0.08 0.09 0.01 Sulphide
Incl 186.0 189.0 3.0 1.95 1.07 0.35 0.12 0.08 0.01 Sulphide
and 194.0 196.0 2.0 1.56 0.59 0.25 0.06 0.17 0.02 Sulphide
JRC122 9.0 28.0 19.0 2.40 0.77 0.02 0.29 0.29 0.10 Oxide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 24

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
Incl 10.0 27.0 17.0 2.61 0.83 0.02 0.30 0.29 0.11 Oxide
JRC122 28.0 109.0 81.0 0.51 0.11 0.01 0.19 0.13 0.02 Sulphide
Incl 35.0 38.0 3.0 2.69 0.42 0.12 0.95 1.00 0.07 Sulphide
JRC122 205.0 213.0 8.0 0.44 0.15 0.05 0.11 0.02 0.01 Sulphide
JRC122 228.0 234.0 6.0 0.49 0.12 0.02 0.11 0.03 0.01 Sulphide
JRC122 250.0 257.0 7.0 0.49 0.13 0.05 0.12 0.09 0.01 Sulphide
JRC123 0.0 25.0 25.0 1.43 0.21 0.00 0.05 0.07 0.01 Oxide
Incl 0.0 15.0 15.0 1.89 0.32 0.00 0.05 0.08 0.00 Oxide
JRC123 57.0 108.0 51.0 1.64 0.34 0.17 0.28 0.12 0.02 Sulphide
Incl 91.0 108.0 17.0 4.07 0.83 0.39 0.46 0.28 0.03 Sulphide
JRC123 123.0 138.0 15.0 0.49 0.11 0.03 0.15 0.07 0.01 Sulphide
JRC123 154.0 180.0 26.0 0.67 0.13 0.02 0.16 0.08 0.01 Sulphide
Incl 156.0 166.0 10.0 1.21 0.19 0.02 0.18 0.12 0.02 Sulphide
JRC123 186.0 210.0 24.0 0.37 0.12 0.02 0.12 0.05 0.01 Sulphide
JRC124 7.0 20.0 13.0 0.79 0.27 0.03 0.25 0.18 0.05 Oxide
Incl 8.0 11.0 3.0 1.08 0.46 0.04 0.22 0.24 0.07 Oxide
JRC124 20.0 203.0 183.0 0.44 0.11 0.02 0.16 0.06 0.02 Sulphide
JRC124 211.0 219.0 8.0 0.33 0.09 0.03 0.15 0.02 0.01 Sulphide
JRC125 6.0 39.0 33.0 1.35 0.32 0.02 0.17 0.16 0.03 Oxide
Incl 9.0 27.0 18.0 1.71 0.37 0.03 0.20 0.20 0.04 Oxide
and 34.0 38.0 4.0 1.39 0.31 0.01 0.17 0.11 0.02 Oxide
JRC125 52.0 64.0 12.0 0.41 0.12 0.02 0.11 0.08 0.01 Sulphide
JRC125 92.0 125.0 33.0 0.44 0.09 0.00 0.15 0.03 0.02 Sulphide
JRC125 132.0 153.0 21.0 0.50 0.12 0.01 0.16 0.08 0.01 Sulphide
JRC125 158.0 192.0 34.0 0.60 0.11 0.01 0.20 0.05 0.02 Sulphide
Incl 167.0 169.0 2.0 1.20 0.22 0.00 0.18 0.07 0.02 Sulphide
JRC125 212.0 248.0 36.0 0.60 0.12 0.02 0.18 0.06 0.02 Sulphide
JRC126 38.0 70.0 32.0 0.66 0.12 0.00 0.15 0.11 0.02 Sulphide
Incl 61.0 63.0 2.0 1.58 0.15 0.01 0.10 0.02 0.01 Sulphide
JRC126 236.0 243.0 7.0 0.58 0.10 0.05 0.10 0.05 0.01 Sulphide
JRC127 1.0 25.0 24.0 1.18 0.20 0.03 0.17 0.18 0.03 Oxide
Incl 4.0 9.0 5.0 2.76 0.30 0.03 0.10 0.23 0.05 Oxide
and 16.0 19.0 3.0 1.20 0.31 0.04 0.36 0.17 0.05 Oxide
JRC127 25.0 40.0 15.0 0.76 0.15 0.03 0.17 0.06 0.02 Sulphide
JRC127 53.0 57.0 4.0 0.33 0.07 0.01 0.15 0.01 0.01 Sulphide
JRC127 73.0 108.0 35.0 0.68 0.13 0.01 0.18 0.04 0.02 Sulphide
JRC127 114.0 182.0 68.0 0.46 0.10 0.02 0.17 0.06 0.02 Sulphide
Incl 134.0 136.0 2.0 1.10 0.23 0.04 0.21 0.15 0.02 Sulphide
JRC127 191.0 258.0 67.0 0.41 0.09 0.01 0.16 0.05 0.01 Sulphide
JRC128 62.0 75.0 13.0 0.54 0.13 0.00 0.14 0.03 0.01 Sulphide
JRC128 154.0 264.0 110.0 0.90 0.17 0.05 0.13 0.14 0.01 Sulphide
Incl 165.0 171.0 6.0 5.43 1.01 0.31 0.13 0.08 0.01 Sulphide
and 188.0 192.0 4.0 2.28 0.14 0.12 0.10 0.51 0.01 Sulphide

==> picture [595 x 5] intentionally omitted <==

Chalice Mining Limited ABN 47 116 648 956

ASX: CHN | OTCQB: CGMLF Page | 25

Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
and 213.0 215.0 2.0 1.45 0.02 0.11 0.12 0.62 0.01 Sulphide
and 226.0 233.0 7.0 1.15 0.27 0.05 0.15 0.22 0.01 Sulphide
JRC129 7.0 35.0 28.0 1.42 0.25 0.02 0.23 0.15 0.05 Oxide
Incl 7.0 21.0 14.0 2.20 0.37 0.02 0.24 0.20 0.08 Oxide
and 33.0 35.0 2.0 1.14 0.17 0.01 0.18 0.22 0.02 Oxide
JRC129 35.0 74.0 39.0 0.97 0.20 0.01 0.18 0.18 0.02 Sulphide
Incl 45.0 53.0 8.0 1.35 0.27 0.01 0.19 0.15 0.01 Sulphide
and 69.0 74.0 5.0 1.67 0.33 0.01 0.33 0.13 0.03 Sulphide
JRC129 81.0 93.0 12.0 0.66 0.13 0.01 0.16 0.08 0.02 Sulphide
Incl 88.0 90.0 2.0 1.57 0.06 0.02 0.42 0.16 0.05 Sulphide
JRC129 124.0 130.0 6.0 0.40 0.09 0.01 0.12 0.17 0.01 Sulphide
JRC129 162.0 167.0 5.0 0.32 0.08 0.00 0.13 0.04 0.02 Sulphide
JRC129 191.0 247.0 56.0 0.73 0.14 0.01 0.21 0.07 0.02 Sulphide
Incl 209.0 220.0 11.0 1.25 0.20 0.01 0.32 0.21 0.03 Sulphide
JRC130 111.0 125.0 14.0 0.38 0.10 0.00 0.10 0.08 0.01 Sulphide
JRC130 130.0 180.0 50.0 0.58 0.14 0.01 0.11 0.09 0.01 Sulphide
Incl 143.0 146.0 3.0 1.13 0.27 0.01 0.14 0.07 0.01 Sulphide
and 177.0 179.0 2.0 1.16 0.24 0.01 0.18 0.17 0.02 Sulphide
JRC130 186.0 194.0 8.0 0.66 0.15 0.01 0.14 0.13 0.01 Sulphide
JRC130 202.0 210.0 8.0 0.41 0.09 0.00 0.15 0.03 0.01 Sulphide
JRC130 216.0 223.0 7.0 0.48 0.12 0.00 0.14 0.05 0.01 Sulphide
JRC130 234.0 264.0 30.0 0.89 0.20 0.00 0.18 0.09 0.02 Sulphide
Incl 252.0 260.0 8.0 1.83 0.45 0.01 0.23 0.28 0.03 Sulphide
JRC131 27.0 50.0 23.0 1.04 0.22 0.00 0.36 0.13 0.03 Sulphide
Incl 30.0 38.0 8.0 1.76 0.36 0.00 0.67 0.23 0.05 Sulphide
JRC131 94.0 100.0 6.0 0.75 0.14 0.00 0.14 0.00 0.01 Sulphide
JRC131 126.0 132.0 6.0 0.32 0.06 0.00 0.12 0.02 0.01 Sulphide
JRC131 281.0 300.0 19.0 0.87 0.26 0.05 0.15 0.16 0.02 Sulphide
Incl 289.0 294.0 5.0 1.07 0.24 0.10 0.15 0.29 0.02 Sulphide
JRC132 7.0 21.0 14.0 1.10 0.37 0.06 0.13 0.20 0.03 Oxide
Incl 8.0 17.0 9.0 1.26 0.43 0.08 0.13 0.23 0.03 Oxide
JRC132 21.0 72.0 51.0 0.67 0.15 0.01 0.15 0.08 0.02 Sulphide
JRC132 155.0 164.0 9.0 0.43 0.10 0.01 0.14 0.03 0.02 Sulphide
JRC132A 6.0 20.0 14.0 0.72 0.26 0.04 0.12 0.17 0.03 Oxide
Incl 8.0 10.0 2.0 1.38 0.65 0.06 0.10 0.23 0.12 Oxide
JRC132A 20.0 30.0 10.0 0.63 0.16 0.01 0.13 0.09 0.01 Sulphide
JRC133 113.0 120.0 7.0 0.38 0.09 0.02 0.04 0.02 0.01 Sulphide
JRC133 132.0 152.0 20.0 0.35 0.09 0.03 0.13 0.13 0.01 Sulphide
JRC133 159.0 182.0 23.0 0.35 0.08 0.01 0.10 0.09 0.01 Sulphide
JRC133 223.0 233.0 10.0 0.50 0.11 0.00 0.14 0.05 0.01 Sulphide
JRC133 263.0 270.0 7.0 0.76 0.15 0.00 0.15 0.14 0.02 Sulphide
Incl 268.0 270.0 2.0 1.23 0.21 0.01 0.21 0.32 0.02 Sulphide
JRC134 10.0 27.0 17.0 1.04 0.25 0.00 0.09 0.10 0.08 Oxide

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Hole ID From
(m)
To
(m)
Interval
*(m) **
Pd
(g/t)
Pt
(g/t)
Au
(g/t)
Ni
(%)
Cu
(%)
Co
(%)
Geology
Incl 13.0 25.0 12.0 1.25 0.28 0.00 0.08 0.13 0.10 Oxide
JRC134 27.0 39.0 12.0 0.60 0.14 0.01 0.14 0.08 0.02 Sulphide
JRC134 69.0 128.0 59.0 0.58 0.13 0.00 0.16 0.05 0.02 Sulphide
Incl 89.0 91.0 2.0 2.44 0.70 0.00 0.59 0.23 0.06 Sulphide
JRC134 165.0 169.0 4.0 0.37 0.07 0.00 0.15 0.08 0.01 Sulphide
JRC134 197.0 258.0 61.0 0.85 0.15 0.03 0.19 0.11 0.02 Sulphide
Incl 200.0 204.0 4.0 6.01 0.62 0.14 0.59 0.53 0.04 Sulphide
JWB002 6.0 23.0 17.0 0.62 0.09 0.00 0.12 0.11 0.01 Oxide
JWB002 23.0 100.0 77.0 0.63 0.14 0.01 0.13 0.09 0.01 Sulphide
Incl 76.0 78.0 2.0 1.08 0.25 0.02 0.18 0.32 0.02 Sulphide
and 81.0 87.0 6.0 1.19 0.24 0.01 0.21 0.16 0.02 Sulphide
and 92.0 94.0 2.0 1.17 0.21 0.01 0.19 0.09 0.02 Sulphide
and 97.0 99.0 2.0 1.17 0.22 0.01 0.16 0.10 0.02 Sulphide
JWB003 7.0 18.0 11.0 0.54 0.05 0.00 0.13 0.20 0.01 Oxide
JWB003 29.0 100.0 71.0 0.75 0.15 0.01 0.15 0.09 0.02 Sulphide
Incl 48.0 50.0 2.0 1.18 0.24 0.01 0.21 0.06 0.02 Sulphide
and 62.0 78.0 16.0 1.05 0.19 0.01 0.19 0.14 0.02 Sulphide
and 88.0 90.0 2.0 1.12 0.21 0.01 0.21 0.14 0.02 Sulphide

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Appendix 2: New drill hole locations Julimar Ni-Cu-PGE Project.

Hole ID Easting Northing RL Azi
(°)
Dip Depth Survey
Type Assaying status
(m) (m) (m) (°) (m) type
JD009 Core 425049.4 6512590.2 242.8 91 -60.6 507.1 GPS-RTK Reported; hole extended
JD017 Core 424892.2 6512608.1 248.7 90 -65.0 618.5 GPS-RTK Reported
JD019 Core 425320 6512360 237.8 90 -60.6 242.0 GPS Reported
JD020 Core 425520 6512707 252.8 92 -61.6 285.8 GPS Reported
JD021 Core 425360 6512600 244.7 88 -63.1 333.8 GPS Reported
JD022 Core 424900 6512320 235.1 89 -61.4 474.8 GPS Reported
JD023 Core 424888 6512600 248.3 117 -61.0 509.31 GPS Reported
JD024 Core 425200 6512360 237.8 93 -61.3 313.1 GPS Pending
JD025 Core 425240 6512430 240.0 89 -61.4 280.6 GPS Pending
JD026 Core 424940 6512170 233.7 60 -60.0 200.3 GPS Reported
JD027 Core 425050 6512360 236.9 91 -56.8 348.8 GPS Pending
JD028 Core 425290 6513320 257.7 90 -63.3 468.78 GPS Pending
JD029 Core 424930 6512600 247.4 92 -61.3 564.8 GPS Pending
JD030 Core 425440 6512284 242.1 90 -60.0 183.7 GPS Pending
JD031 Core 425290 6513520 256.0 91 -59.9 450.42 GPS Pending
JD032 Core 424795 6512665 251.0 119 -61.5 660.7 GPS Pending
JD033 Core 425400 6512284 239.7 90 -59.9 210.8 GPS Pending
JD034 Core 425438 6513039 258.0 90 -60.0 226.2 GPS Pending
JRC006D Core 425075.9 6512317.2 239.5 93 -60 331 GPS-RTK Reported; hole extended
JRC081 RC 425132.9 6512214.3 232.6 272 -59.9 234 GPS-RTK Reported
JRC082 RC 424922.0 6512698.6 254.0 90 -61.1 264 GPS-RTK Reported
JRC083 RC 425075.9 6512511.2 239.9 88 -59.0 252 GPS-RTK Reported
JRC084 RC 425469.6 6512358.3 244.5 90 -58.0 174 GPS-RTK Reported(NSA)
JRC085A RC 425170.3 6512507.9 241.3 91 -59.5 132 GPS-RTK Reported
JRC086 RC 425437.4 6512357.7 242.2 91 -61.0 204 GPS-RTK Reported(NSA)
JRC087 RC 425257.0 6512507.6 241.8 90 -58.8 250 GPS-RTK Reported
JRC088 RC 425399.0 6512359.1 240.1 92 -59.5 228 GPS-RTK Reported
JRC090 RC 425121.2 6512371.4 239.7 90 -59.9 226 GPS-RTK Reported
JRC091 RC 425555.2 6512422.3 243.1 87 -67.3 216 GPS-RTK Reported
JRC091A RC 425555.3 6512424.3 242.6 90 -57.0 30 GPS-RTK Reported
JRC092 RC 425084.9 6512600.9 244.1 90 -57.6 250 GPS-RTK Reported
JRC093 RC 425462.6 6512428.8 243.2 90 -58.9 192 GPS-RTK Reported(NSA)
JRC094 RC 425125.4 6512600.0 244.0 90 -60.8 258 GPS-RTK Reported
JRC095 RC 425438.4 6512429.0 241.9 90 -61.5 240 GPS-RTK Reported
JRC096 RC 424838.5 6512699.1 253.9 88 -60.5 250 GPS-RTK Reported
JRC097 RC 425398.8 6512428.3 240.5 90 -60.4 250 GPS-RTK Reported
JRC098 RC 425359.0 6512428.7 239.6 89 -61.2 270 GPS-RTK Reported
JRC099 RC 424977.4 6512707.0 253.7 90 -57.5 276 GPS-RTK Reported
JRC100 RC 425314.2 6512428.6 238.9 91 -59.5 240 GPS-RTK Reported
JRC100A RC 425319.1 6512428.4 238.7 91 -60.0 24 GPS-RTK Reported(NSA)
JRC101 RC 425490 6512510 242.6 91 -59.7 222 GPS Reported(NSA)

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Hole ID Easting Northing RL Azi
(°)
Dip Depth Survey
Type Assaying status
(m) (m) (m) (°) (m) type
JRC102 RC 425080 6512700 249.9 90 -59.5 276 GPS Reported
JRC103 RC 425160 6512700 249.3 89 -58.4 288 GPS Reported
JRC104 RC 425410 6512510 242.5 95 -60.5 252 GPS Reported
JRC105 RC 425334 6512510 241.2 89 -60.8 264 GPS Reported
JRC106 RC 425240 6512700 249.3 92 -58.8 258 GPS Reported
JRC107 RC 425600 6512600 242.7 90 -60.2 204 GPS Reported
JRC108 RC 425560 6512600 244.3 90 -74.2 222 GPS Reported
JRC109 RC 425321 6512710 249.9 89 -60.4 258 GPS Reported
JRC110 RC 425560 6512600 244.3 93 -59.1 216 GPS Reported
JRC111 RC 425558 6512714 250.4 93 -60.6 192 GPS Reported
JRC112 RC 425280 6512600 244.9 90 -60.6 258 GPS Reported
JRC113 RC 425480 6512700 253.7 89 -60.0 252 GPS Reported
JRC114 RC 425320 6512600 244.4 90 -59.0 258 GPS Reported
JRC115 RC 425400 6512700 251.0 89 -60.8 294 GPS Reported
JRC116 RC 425472 6512600 247.5 89 -57.8 282 GPS Reported
JRC117 RC 425280 6512360 237.6 92 -60.0 252 GPS Reported
JRC118 RC 425440 6512600 246.5 85 -59.67 257 GPS Reported
JRC119 RC 425600 6512780 248.5 90 -60.0 258 GPS Reported
JRC120 RC 425160 6512365 238.7 91 -58.3 300 GPS Reported
JRC121 RC 425557 6512778 250.4 84 -60.0 252 GPS Reported
JRC122 RC 425403 6512601 245.5 85 -59.9 288 GPS Reported
JRC123 RC 425520 6512780 254.2 91 -59.8 258 GPS Reported
JRC124 RC 425230 6512361 237.3 90 -60.2 264 GPS Reported
JRC125 RC 425210 6512600 244.8 88 -60.0 248 GPS Reported(NSA)
JRC126 RC 425480 6512780 256.7 89 -62.2 264 GPS Reported
JRC127 RC 425201 6512446 241.3 91 -60.5 258 GPS Reported
JRC128 RC 425440 6512780 258.0 89 -61.2 294 GPS Reported
JRC129 RC 425171 6512601 244.2 90 -59.6 247 GPS Reported
JRC130 RC 425190 6513080 262.7 90 -60.3 264 GPS Reported
JRC131 RC 425400 6512780 257.0 90 -59.4 300 GPS Reported
JRC132 RC 425560 6513322 246.6 92 -60.1 213 GPS Reported
JRC133 RC 425110 6513080 264.5 91 -60.2 270 GPS Reported
JRC134 RC 425360 6512780 255.1 86 -60.0 258 GPS Reported
JRC135 RC 425313 6512790 254.6 89 -59.8 258 GPS Pending
JRC136 RC 425490 6513320 248.0 90 -60.0 216 GPS Pending
JRC137 RC 425280 6512430 239.6 88 -61.9 300 GPS Pending
JRC138 RC 425280 6512780 254.9 90 -60.2 288 GPS Pending
JRC139 RC 425410 6513320 251.4 84 -58.8 252 GPS Pending
JRC140 RC 425240 6512774 255.8 93 -59.1 282 GPS Pending
JRC141 RC 425149 6512431 240.8 89 -59.4 258 GPS Pending
JRC142 RC 425210 6513320 261.1 89 -59.1 234 GPS Pending
JRC143 RC 424960 6512780 258.3 88 -59.6 258 GPS Pending
JRC144 RC 425205 6512783 257.5 90 -59.6 244 GPS Pending

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Hole ID Easting Northing RL Azi
(°)
Dip Depth Survey
Type Assaying status
(m) (m) (m) (°) (m) type
JRC145 RC 425330 6513320 256.1 88 -59.8 246 GPS Pending
JRC146 RC 425116 6513000 265.8 93 -52.2 252 GPS Pending
JRC147 RC 425000 6512780 258.1 88 -59.3 246 GPS Pending
JRC148 RC 425130 6513320 265.4 89 -59.2 270 GPS Pending
JRC149 RC 425090 6513000 266.0 92 -61.8 264 GPS Pending
JRC150 RC 425010 6513320 269.7 91 -59.6 264 GPS Pending
JRC151 RC 424920 6512780 257.8 92 -59.4 276 GPS Pending
JRC152 RC 425490 6513520 249.6 90 -59.2 250 GPS Pending
JRC153 RC 425030 6513080 266.6 90 -60.0 252 GPS Pending
JRC154 RC 425150 6513080 263.4 90 -60.0 254 GPS Pending
JRC156 RC 425410 6513520 251.8 90 -60.0 36.0 GPS Pending- abandoned hole
JRC157 RC 425050 6513520 265.5 90 -60.0 252 GPS Pending
JRC158 RC 425330 6513520 254.3 90 -60.0 240 GPS Pending
JRC159 RC 424880 6512780 257.3 92 -60.3 249 GPS Pending
JRC160 RC 424840 6512780 256.6 86 -60.2 249 GPS Pending
JRC161 RC 425580 6512820 249.3 90 -59.9 249 GPS Pending
JRC162 RC 425560 6512865 251.0 81 -59.0 253 GPS Pending

NSA = no significant assay

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Figure 8. Gonneville Intrusion Plan View – Geology and new drill holes.

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Appendix 3: JORC Table 1 – Julimar Ni-Cu-PGE Project

Section 1Sampling Techniques and Data Section 1Sampling Techniques and Data
Criteria JORC Code explanation Commentary
Sampling
techniques

Nature and quality of sampling (eg. cut
channels, random chips, or specific
specialised industry standard measurement
tools appropriate to the minerals under
investigation, such as down hole gamma
sondes, or handheld XRF instruments, etc).
These examples should not be taken as
limiting the broad meaning of sampling.

Include reference to measures taken to
ensure sample representivity and the
appropriate calibration of any measurement
tools or systems used.

Aspects of the determination of
mineralisation that are Material to the Public
Report.

In cases where ‘industry standard’ work has
been done this would be relatively simple
(eg. ‘reverse circulation drilling was used to
obtain 1 m samples from which 3 kg was
pulverised to produce a 30 g charge for fire
assay’). In other cases more explanation
may be required, such as where there is
coarse gold that has inherent sampling
problems. Unusual commodities or
mineralisation types (eg. submarine nodules)
may warrant disclosure of detailed
information.

Diamond drill core samples were taken
over selective intervals ranging from 0.2m
to 1.2m (typically 1.0m). Qualitative care
taken when sampling diamond drill core
to sample the same half of the drill core.

Reverse Circulation (RC) drilling samples
were collected as 1m samples. Two 1m
assay samples were collected as a split
from the rig cyclone using a cone splitter
and are typically 3kg in weight.
Drilling
techniques

Drill type (eg. core, reverse circulation, open-
hole hammer, rotary air blast, auger,
Bangka, sonic, etc) and details (eg. core
diameter, triple or standard tube, depth of
diamond tails, face-sampling bit or other
type, whether core is oriented and if so, by
what method, etc).

Drilling has been undertaken by diamond
and Reverse Circulation (RC) techniques.

Diamond drill core is HQ size (63.5mm
diameter) with triple tube used from
surface and standard tube in competent
bedrock.

Core orientation is by an ACT Reflex (ACT II
RD) tool

RC Drilling uses a face-sampling hammer
drill bit with a diameter of 5.5 inches
(140mm).
Drill sample
recovery

Method of recording and assessing core and
chip sample recoveries and results assessed.

Measures taken to maximise sample
recovery and ensure representative nature
of the samples.

Whether a relationship exists between
sample recovery and grade and whether
sample bias may have occurred due to
preferential loss/gain of fine/coarse material.

Individual recoveries of diamond drill core
samples were recorded on a qualitative
basis. Generally sample weights are
comparable, and any bias is considered
negligible.

Individual recoveries for RC composite
samples were recorded on a qualitative
basis. Sample weights were slightly lower
through transported cover whereas drilling
through bedrock yielded samples with
more consistent weights.

No relationships have been evident
between diamond core, RC sample
grade andrecoveries.
Logging
Whether core and chip samples have been
geologically andgeotechnically logged to a

All drill holes were logged geologically
including,but not limited to;weathering,

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Criteria JORC Code explanation Commentary
level of detail to support appropriate Mineral
Resource estimation, mining studies and
metallurgical studies.

Whether logging is qualitative or quantitative
in nature. Core (or costean, channel, etc)
photography.

The total length and percentage of the
relevant intersections logged.
regolith, lithology, structure, texture,
alteration and mineralisation. Logging was
at an appropriate quantitative standard
for reconnaissance exploration.

Logging is considered qualitative in
nature.

All holes were geologically logged in full.

Diamond drill core is photographed wet
before cutting.
Sub-sampling
techniques
and sample
preparation

If core, whether cut or sawn and whether
quarter, half or all core taken.

If non-core, whether riffled, tube sampled,
rotary split, etc and whether sampled wet or
dry.

For all sample types, the nature, quality and
appropriateness of the sample preparation
technique.

Quality control procedures adopted for all
sub-sampling stages to maximise
representivity of samples.

Measures taken to ensure that the sampling
is representative of the in-situ material
collected, including for instance results for
field duplicate/second-half sampling.

Whether sample sizes are appropriate to the
grain size of the material being sampled.

Diamond core was sawn in half and one-
half quartered and selectively sampled
over 0.2-1.2m intervals (mostly 1m).

Diamond drill core field duplicates
collected as ¼ core.

RC assay samples were collected as two
1m splits from the rig cyclone via a cone
splitter. The cone splitter was horizontal to
ensure sample representivity. Wet or
damp samples were noted in the sample
logging sheet and a majority of samples
were dry.

Sample preparation is industry standard
and comprises oven drying, jaw crushing
and pulverising to -75 microns (80% pass).

Field duplicates were collected from
selected sulphide zones as a second 1m
split directly from the cone splitter.

Drill sample sizes are considered
appropriate for the style of mineralisation
sought and the nature of the drilling
program.
Quality of
assay data
and laboratory
tests

The nature, quality and appropriateness of
the assaying and laboratory procedures
used and whether the technique is
considered partial or total.

For geophysical tools, spectrometers,
handheld XRF instruments, etc, the
parameters used in determining the analysis
including instrument make and model,
reading times, calibrations factors applied
and their derivation, etc.

Nature of quality control procedures
adopted (eg. standards, blanks, duplicates,
external laboratory checks) and whether
acceptable levels of accuracy (ie. lack of
bias) and precision have been established.

Diamond drill core and RC samples
underwent sample preparation and
geochemical analysis by ALS Perth. Au-Pt-
Pd was analysed by 50g fire assay fusion
with an ICP-AES finish (ALS Method code
PGM-ICP24). A 48-element suite was
analysed by ICP-MS following a four-acid
digest (ALS method code ME-MS61)
including Ag, Al, As, Ba, Be, Bi, Ca, Cd, Ce,
Co, Cr, Cs, Cu, Fe, Ga, Ge, Hf, In, K, La, Li,
Mg, Mn, Mo, Na, Nb, Ni, P, Pb, Rb, Re, S,
Sb, Sc, Se, Sn, Sr, Ta, Te, Th, Ti, Tl, U, V, W, Y,
Zn, Zr. Additional ore-grade analysis was
performed as required for elements
reporting out of range for Ni, Cr, Cu (ALS
method code ME-OG-62) and Pd, Pt (ALS
method code PGM-ICP27).

Certified analytical standards and blanks
were inserted at appropriate intervals for
diamond, RC drill samples and auger soil
samples

Approximately 5% of samples submitted
for analysis comprised QAQC control
samples.
Verification of
sampling and
assaying

The verification of significant intersections by
either independent or alternative company
personnel.

Significant drill intersections are checked
by the Project Geologist and then by the
General Manager Exploration. Significant

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Criteria JORC Code explanation Commentary

The use of twinned holes.

Documentation of primary data, data entry
procedures, data verification, data storage
(physical and electronic) protocols.

Discuss any adjustment to assay data.
intersections are cross-checked with the
logged geology and drill core after final
assays are received.

Two RC holes have been twinned with a
diamond hole to provide a comparison
between grade/thickness variations over
a 5m separation between drill holes.

Primary drill data was collected digitally
using OCRIS software before being
transferredtothemasterSQLdatabase.
Location of
data points

Accuracy and quality of surveys used to
locate drill holes (collar and down-hole
surveys), trenches, mine workings and other
locations used in Mineral Resource
estimation.

Specification of the grid system used.

Quality and adequacy of topographic
control.

Diamond and RC drill hole collar locations
are initially recorded by Chalice
employees using a handheld GPS with a
+/- 3m margin of error.

DGPS collar pick-ups replace handheld
GPS collar pick-ups and have +/-20 mm
margin of error.

The grid system used for the location of all
drill holes is GDA94 - MGA (Zone 50).

RLs were assigned either from 1 sec (30m)
satellite data or DGPS pick-ups.
Data spacing
and
distribution

Data spacing for reporting of Exploration
Results.

Whether the data spacing and distribution is
sufficient to establish the degree of
geological and grade continuity appropriate
for the Mineral Resource and Ore Reserve
estimation procedure(s) and classifications
applied.

Whether sample compositing has been
applied.

Drill hole spacing varies from between
80m x 40 m in the south to 200m x 80m in
the north.

Results from the drilling to date are not
considered sufficient to assume any
geological or grade continuity
appropriate for Mineral Resource
estimation procedure(s) and
classifications.

No compositing undertaken for diamond
drillcore or RC samples.
Orientation of
data in
relation to
geological
structure

Whether the orientation of sampling
achieves unbiased sampling of possible
structures and the extent to which this is
known, considering the deposit type.

If the relationship between the drilling
orientation and the orientation of key
mineralised structures is considered to have
introduced a sampling bias, this should be
assessed and reported if material.

RC and Diamond drill holes were typically
oriented within 15° of orthogonal to the
interpreted dip and strike of the known
zone of mineralisation. However, drill holes
JD012, JD026, JRC60 JRC078 and JRC081
were drilled at less optimal azimuths due
to site access constraints.

The orientation of the drilling is not
considered to have introduced sampling
bias
Sample
security

The measures taken to ensure sample
security.

Samples are collected in polyweave bags
and delivered directly from site to ALS
laboratories in Wangara, Perth by a
Chalice contractor
Audits or
reviews

The results of any audits or reviews of
sampling techniques and data.

No review has been carried out to date.

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**Section 2 Reporting ** of Exploration Results
Criteria JORC Code explanation Commentary
Mineral tenement
and land tenure
status

Type, reference name/number, location
and ownership including agreements or
material issues with third parties such as
joint ventures, partnerships, overriding
royalties, native title interests, historical
sites, wilderness or national park and
environmental settings.

The security of the tenure held at the time
of reporting along with any known
impediments to obtaining a licence to
operate in the area.

Exploration activities are ongoing over
E70/5118 and 5119 on private property.
CGM (WA) Pty Ltd is a wholly owned
subsidiary of Chalice Mining Limited with
no known encumbrances.

Current drilling is on private land only,
however granted tenure covers both
private land and State Forest.

Access for non-ground disturbing
exploration in the Julimar State Forest
requires Ministerial approval which has
been obtained.

The Company has submitted a
Conservation Management Plan (CMP)
to the Department of Biodiversity,
Conservation and Attractions (DBCA). The
CMP details Chalice’s planned non-
ground disturbing reconnaissance
exploration activities across the Julimar
Complex.

Access for ground disturbing exploration
(including drilling) in the Julimar State
Forest requires an additional approval
which has not yet been obtained.

E70/5119 partially overlaps ML1SA, a State
Agreement covering Bauxite mineral
rights only.
Exploration done
by other parties

Acknowledgment and appraisal of
exploration by other parties.

Limited exploration has been completed
by other exploration parties in the vicinity
of the targets identified by Chalice to
date.

Chalice has compiled historical records
dating back to the early 1960’s which
indicate only three genuine explorers in
the area, all primarily targeting Fe-Ti-V
mineralisation.

Over 1971-1972, Garrick Agnew Pty Ltd
undertook reconnaissance surface
sampling over prominent aeromagnetic
anomalies in a search for ‘Coates deposit
style’ vanadium mineralisation. Surface
sampling methodology is not described in
detail, nor were analytical methods
specified, with samples analysed for V2O5,
Ni, Cu, Cr, Pb and Zn, results of which are
referred to in this announcement.

Three diamond holes were completed by
Bestbet Pty Ltd targeting Fe-Ti-V situated
approximately 3km NE of JRC001. No
elevated Ni-Cu-PGE assays were
reported.

Bestbet Pty Ltd undertook 27 stream
sediment samples within E70/5119.
Elevated levels of palladium were noted
in the coarse fraction (-5mm+2mm) are
reported in this release. Finer fraction
samples didnot replicatethe coarse

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Criteria JORC Code explanation Commentary
fraction results.

A local AMAG survey was flown in 1996
by Alcoa using 200m line spacing which
has been used by Chalice for targeting
purposes.
Geology
Deposit type, geological setting and style
of mineralisation.

The target deposit type is a magmatic Ni-
Cu-PGE sulphide deposit, within the
Yilgarn Craton. The style of sulphide
mineralisation intersected consists of
massive, matrix, stringer and disseminated
sulphides typical of metamorphosed and
structurally overprinted magmatic Ni
sulphide deposits.
Drill hole
Information

A summary of all information material to
the understanding of the exploration
results including a tabulation of the
following information for all Material drill
holes:
o easting and northing of the drill hole
collar
o elevation or RL (Reduced Level –
elevation above sea level in metres) of
the drill hole collar
o dip and azimuth of the hole
o down hole length and interception
depth
o hole length.

If the exclusion of this information is justified
on the basis that the information is not
Material and this exclusion does not
detract from the understanding of the
report, the Competent Person should
clearly explain why this is the case.

Provided in body of text
• No material information has been
excluded.
Data
aggregation
methods

In reporting Exploration Results, weighting
averaging techniques, maximum and/or
minimum grade truncations (eg. cutting of
high grades) and cut-off grades are
usually Material and should be stated.

Where aggregate intercepts incorporate
short lengths of high-grade results and
longer lengths of low grade results, the
procedure used for such aggregation
should be stated and some typical
examples of such aggregations should be
shown in detail.

The assumptions used for any reporting of
metal equivalent values should be clearly
stated.

Significant intercepts are reported using a
>0.3g/t Pd length-weighted cut off. A
maximum of 4m internal dilution has been
applied.

Metal equivalent values are not reported.
Relationship
between
mineralisation
widths and
intercept lengths

These relationships are particularly
important in the reporting of Exploration
Results.

If the geometry of the mineralisation with
respect to the drill hole angle is known, its
nature should be reported.

If it is not known and only the down hole
lengths are reported, there should be a
clear statement to this effect (eg. ‘down
_hole length, true width not known’). _

All widths are quoted down-hole.

All drill holes were orientated to be as
close as possible to orthogonal to the
interpreted strike and/or dip of the
mineralised zone(s) and/or targets except
for JD010, JD012, JD013, JD014, JD023,
JD032, JRC060, JRC078 and JRC081 due
to access constraints.

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Chalice Mining Limited ABN 47 116 648 956

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Criteria JORC Code explanation Commentary
Diagrams
Appropriate maps and sections (with
scales) and tabulations of intercepts
should be included for any significant
discovery being reported These should
include, but not be limited to a plan view
of drill hole collar locations and
appropriate sectional views.

Refer to figures in the body of text.
Balanced
reporting

Where comprehensive reporting of all
Exploration Results is not practicable,
representative reporting of both low and
high grades and/or widths should be
practiced to avoid misleading reporting of
Exploration Results.

All significant intercepts have been
reported.
Other substantive
exploration data
Other exploration data, if meaningful and
material, should be reported including (but
not limited to): geological observations;
geophysical survey results; geochemical
survey results; bulk samples – size and
method of treatment; metallurgical test
results; bulk density, groundwater,
geotechnical and rock characteristics;
potential deleterious or contaminating
substances.
Not applicable
Further work
The nature and scale of planned further
work (eg. tests for lateral extensions or
depth extensions or large-scale step-out
drilling).

Diagrams clearly highlighting the areas of
possible extensions, including the main
geological interpretations and future
drilling areas, provided this information is
not commercially sensitive.

Diamond and RC drilling will continue to
test high-priority targets including EM
conductors. Further drilling along strike
and down dip may occur at these and
other targets depending on results.

Down-hole EM surveying will be carried
out on the majority of diamond and
selective RC drill holes to test for off-hole
conductors. Subsequent holes will
undergo down-hole EM if required.

Any potential extensions to mineralisation
are shown in the figures in the body of the
text.

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Chalice Mining Limited ABN 47 116 648 956

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