Fireweed Drills 12.5 m of 11.17% Zinc including 6.2 m of 15.84% Zinc at Boundary Main

Fireweed Metals CORP. ("Fireweed" or the "Company") (TSXV: FWZ; OTCQB: FWEDF, formerly Fireweed Zinc Ltd.) is pleased to announce further results from the 2022 drill program at Macmillan Pass, Yukon, Canada (Map 1).

Highlights

At Boundary Main step-out drillhole NB22-006 intersected 12.5 m of 11.17% zinc including 6.2 m of 15.84% zinc.
A new laminated zone in hole NB22-008 returned 14.55% zinc, 1.50% lead, and 28.8 g/t silver over 2.65 m.
Copper-zinc mineralization was intersected in NB22-006 over 10.5 m grading 0.45% copper and 2.32% zinc.
Assay results from 24 additional drill holes at Boundary and Tom Zones are pending.

CEO Statement

Brandon Macdonald, CEO, stated, "Drilling continues to extend the Boundary Zones with high-grade step-out drill results, including the discovery of a new stratiform zone. The zones remain open along trend and to depth for further extension. Many additional 2022 drill results are pending and we have started planning the biggest drill program in the history of the project for 2023."

New Boundary Drillholes Results

NB22-008

Laminated sphalerite-galena-barite-pyrite mineralization was intersected in NB22-008 within only 35 m from surface and occurs within the same late-Devonian stratigraphy that hosts the Tom and Jason deposits. This zone graded 8.08% zinc, 0.82% lead, and 17.8 g/t silver over 5.58 m, containing a higher grade 2.65 m interval of 14.55% zinc, 1.50% lead and 28.8 g/t silver (Table 1). This represents a new discovery of a high-grade laminated zone at Boundary Main and remains open to the north and west.

Deeper in NB22-008, a broad zone of sphalerite mineralization was intersected, grading 3.32% zinc over 30.68 m (including higher grade intervals listed in Table 1), representing a ~65 m step-out down-dip from the historic Cominco hole NB91-25 (Map 2). This zone comprised replacement of matrix and some clasts by pyrite and red sphalerite in coarse clastic rocks and breccias cemented by sphalerite-pyrite with minor sphalerite-quartz veins. The textures in this step out intersection are typical of the zinc mineralization at Boundary Main.

NB22-005

This hole intersected several narrow (2.84 m to 4.7 m wide) intervals of stockwork sphalerite-siderite veins grading 4.20% to 5.55% zinc (Table 1) within a sequence of coarse volcaniclastic rocks and conglomerates, typical of mineralization at Boundary Main. These intersections are 30 m to 40 m step-outs up-dip from mineralization in historic Cominco hole NB91-25 (Map 2).

Deeper in NB22-005 an 18.4 m intersection of 2.84% zinc was made in a sequence of black mudstones and lapillistones of the Road River Group comprising many thin red sphalerite-quartz-siderite veins and selective replacement of lapilli by red sphalerite. This intersection is a ~45 m step-out from similar mineralization intersected in 2021 Fireweed drillhole NB21-010.

NB22-006

This hole intersected matrix and clast replacement sphalerite mineralization and sphalerite vein mineralization in several wide intervals typical of the style seen at Boundary Main (Table 1). A higher-grade portion of one of these intervals graded 11.17% zinc over 12.5 m including 6.22 m of 15.84% zinc. Hole NB22-006 is a step-out hole, stepping-out 55 m to 70 m away from zinc mineralization in historic Cominco drillhole NB90-20 (Map 2, Cross Section E-E').

In hole NB22-006, copper-zinc mineralization was intersected over 10.5 m at 0.45% copper and 2.32% zinc within semi-massive pyrite replacing diamictite clasts and matrix. This intersection is 145 m along strike from the intersection of 1.54% copper and 5.42% zinc over 2.00 m reported from 2021 drillhole NB21-005 (see Fireweed news release dated November 18, 2021) and it is unclear whether there is any continuity between these intersections.

Table 1: NB22-005, NB22-006 and NB22-008 drill results.

Drill hole	Zone	Interval	From (m)	To (m)	Width* (m)	Zn (%)	Pb (%)	Ag (g/t)	Cu (%)	Bulk Density (t/m ³ )
NB22-008	BM	primary	40.92	46.50	5.58	8.08	0.82	17.8	0.06	3.02
NB22-008	BM	>incl.	40.92	43.57	2.65	14.55	1.50	28.8	0.10	3.32
NB22-008	BM	primary	132.47	163.15	30.68	3.32	0.03	7.7	0.01	3.15
NB22-008	BM	>incl.	156.00	163.15	7.15	6.18	0.03	9.9	0.01	3.14
NB22-008	BM	>>incl.	157.76	160.33	2.57	10.33	0.05	15.0	0.01	3.21
NB22-006	BM	primary	132.50	231.50	99.00	2.86	0.02	4.4	0.05	3.19
NB22-006	BM	>incl.	132.50	143.00	10.50	2.32	0.05	6.1	0.45	3.26
NB22-006	BM	>and	143.00	231.50	88.50	2.93	0.02	4.2	0.01	3.18
NB22-006	BM	>>incl.	146.00	151.00	5.00	8.23	0.04	14.1	0.02	3.59
NB22-006	BM	>>>incl.	147.90	150.00	2.10	12.56	0.05	15.3	0.02	3.72
NB22-006	BM	>>and	219.00	231.50	12.50	11.17	0.02	11.0	0.01	2.90
NB22-006	BM	>>>incl.	219.78	226.00	6.22	15.84	0.04	15.8	0.02	2.98
NB22-006	BM	primary	255.87	282.91	27.04	3.45	0.02	5.0	0.01	2.74
NB22-005	BM	primary	24.11	26.95	2.84	4.81	0.02	8.8	0.06	2.88
NB22-005	BM	primary	93.20	96.19	2.99	4.20	0.01	6.8	0.02	2.88
NB22-005	BM	primary	99.30	104.00	4.70	5.55	0.09	14.9	0.02	2.99
NB22-005	BM	>incl.	101.20	102.40	1.20	14.41	0.22	32.0	0.03	3.49
NB22-005	BM	primary	115.08	118.13	3.05	4.31	0.10	7.4	0.01	2.92
NB22-005	BW	primary	267.50	285.90	18.40	2.84	0.04	6.2	0.01	3.00

Zones: BM= Boundary Main; BW= Boundary West.
*Intersected thicknesses, not true thicknesses, are stated for all intersections in Table 1. Most intersections in Table 1 are vein stockwork or replacement styles of mineralization and have undetermined true thicknesses. The laminated mineralization in NB22-008, 40.92 m to 46.50 m is assumed to be stratiform and true thickness is estimated to be approximately 30% to 85% of intersected thickness, based on bedding angles to core axis in and around the mineralized intersection.
Note – an interval of core in NB22-006 from 232.82 m to 255.87 m and an interval from 57.0 m to 66.87 m in hole NB22-008 were not assayed as these intervals were lost to a windstorm that up-ended several core tables, spilling the core on the ground prior to logging and sampling.

Data verification

The diamond drill core logging and sampling program was carried out under a rigorous quality assurance / quality control program using industry best practices. Drill intersections in this release are HQ3 (split tube) size core (61.1mm / 2.406-inch diameter) (drill hole NB22-008) and NQ2 size core (50.5 mm/ 1.99-inch diameter) (drill holes NB22-005 and NB22-006) with recoveries typically above 85% unless otherwise noted in the table of results. After drilling, core was cleaned, scanned with a core scanning machine, logged for geology, structure, and geotechnical characteristics, then marked for sampling and photographed on site. The cores for analyses were marked for sampling based on geological intervals with individual samples 1.5 m or less in length. Drill core was cut lengthwise in half with a core saw; half-core was sent for assays reported in this news release, and the other half is stored on site for reference. Bulk density was determined on site for the entire length of each sample assayed by measurement of mass in air and mass in water. Sample duplicate bulk density determinations and in-house bulk density standard determinations were each made at a rate of 5%. Since 2017, four in-house bulk density standards (mineralized drill core from the Tom deposit that span a range of densities) have been used and show an acceptable long-term precision. Certified standard masses are used to calibrate the scale balance used for bulk density determinations.

A total of 5% assay standards or blanks and 5% core duplicates are included in the sample stream as a quality control measure and are reviewed after analyses are received. Standards and blanks in 2022 drill results to date have been approved as acceptable. Duplicate data add to the long-term estimates of precision for assay data on the project and precision for drill results reported is deemed to be within acceptable levels. Samples were sent to the Bureau Veritas preparation laboratory in Whitehorse, Yukon, where the samples were crushed and a 500 g split was sent to the Bureau Veritas laboratory in Vancouver, B.C to be pulverized to 85% passing 200 mesh size pulps. Clean crush material was passed through the crusher and clean silica was pulverized between each sample. The pulps were analyzed by 1:1:1 Aqua Regia digestion followed by Inductively Coupled Plasma Mass Spectrometry (ICP-ES/ICP-MS) multi-element analyses (BV Code AQ270). All samples were also analyzed for multiple elements by lithium borate fusion and X-ray fluorescence analysis (XRF) finish (BV Code LF725). Over-limit Pb (>25.0%) and Zn (>24.0%) were analyzed by lithium borate fusion with XRF finish (BV Code LF726). Silver and copper are reported in this news release by method AQ270, and zinc and lead are reported by LF725 or LF726. Bureau Veritas (Vancouver) is an independent, international ISO/IEC 17025:2005 accredited laboratory.

Results in this news release are length and bulk-density weighted averages as would be used in a Mineral Resource estimate. Readers are cautioned that in Fireweed news releases prior to 2020, only length weighted assay averages were reported which may result in slightly lower (under-reported) average values. Length and bulk-density weighted averages have been reported as these most accurately represent the average metal-content of the intersections.

Qualified Person Statement

Technical information in this news release has been approved by Fireweed Metals Chief Geologist, Jack Milton, Ph.D., P.Geo (BC), and a ‘Qualified Person' as defined under Canadian National Instrument 43-101.

Updated Private Placement Information

Further to the Company's news releases of 21 December 2022 and 30 December 2022 announcing closing of the $35 million private placement and related finders' fees, the correct cash finders' fees totalled $403,346.99.

About Fireweed Metals Corp. (TSXV: FWZ; OTCQB: FWEDF; FSE:20F): Fireweed Metals is a public mineral exploration company on the leading edge of Critical Minerals project development. The Company has three projects located in northern Canada:

Macmillan Pass Zinc-Lead-Silver Project: Fireweed owns 100% of the district-scale 940 km ² Macmillan Pass project in Yukon, Canada, which is host to the Tom and Jason zinc-lead-silver deposits with current Mineral Resources and a PEA economic study (see Fireweed news releases dated 10 ^th January 2018, and 23 ^rd May 2018, respectively, and reports filed on www.sedar.com for details) as well as the Boundary Zone, Boundary Zone West, Tom North Zone and End Zone which have significant zinc-lead-silver mineralization drilled but not yet classified as mineral resources. The project also includes large blocks of adjacent claims with known showings and significant upside exploration potential. The large 2022 drill program utilizing four drills is complete and assay results are being announced as they are received and interpreted.
Mactung Tungsten Project: The Company has a binding Letter of Intent to acquire 100% interest in the 37.6 km ² Mactung Tungsten Project located adjacent to the Macmillan Pass Project. Mactung contains historic resources that make it one of the largest and highest-grade undeveloped resources in the world of the Critical Mineral Tungsten. Located in Canada, it is one of the rare large tungsten resources outside of China. Due diligence and validation work on historic data has been completed and a second phase of relogging and sampling of historic drill core has begun and will support a new mineral resource estimate.
Gayna River Zinc-Lead-Gallium-Germanium Project: Fireweed has 100% of the 128.75 km ² Gayna River project located 180 kilometres north of the Macmillan Pass project. It is host to extensive mineralization including Critical Minerals zinc, gallium and germanium as well as lead and silver, outlined by 28,000 metres of historic drilling and significant upside potential. The 2022 field program of geochemical sampling, airborne LiDAR topographic surveying and ground geophysics is now complete and data is being interpreted toward defining drill targets.

In Canada, Fireweed (TSXV: FWZ) trades on the TSX Venture Exchange. In the USA, Fireweed (OTCQB: FWEDF) trades on the OTCQB Venture Market for early stage and developing U.S. and international companies and is DTC eligible for enhanced electronic clearing and settlement. The Company is current in its reporting, and undergoes an annual verification and management certification process. Investors can find Real-Time quotes and market information for the Company on www.otcmarkets.com . In Europe, Fireweed (FSE: 20F) trades on the Frankfurt Stock Exchange.

Additional information about Fireweed and its projects can be found on the Company's website at FireweedMetals.com and at www.sedar.com .

ON BEHALF OF Fireweed Metals CORP.

" Brandon Macdonald "

CEO & Director

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Statements

Forward Looking Statements

This news release contains "forward-looking" statements and information ("forward-looking statements"). All statements, other than statements of historical facts, included herein, including, without limitation, statements relating to interpretation of drill results, future work plans, the use of funds, and the potential of the Company's projects, are forward looking statements. Forward-looking statements are frequently, but not always, identified by words such as "expects", "anticipates", "believes", "intends", "estimates", "potential", "possible", and similar expressions, or statements that events, conditions, or results "will", "may", "could", or "should" occur or be achieved. Forward-looking statements are based on the beliefs of Company management, as well as assumptions made by and information currently available to Company management and reflect the beliefs, opinions, and projections on the date the statements are made. Forward-looking statements involve various risks and uncertainties and accordingly, readers are advised not to place undue reliance on forward-looking statements. 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 but are not limited to, exploration and development risks, unanticipated reclamation expenses, expenditure and financing requirements, general economic conditions, changes in financial markets, the ability to properly and efficiently staff the Company's operations, the sufficiency of working capital and funding for continued operations, title matters, First Nations relations, operating hazards, political and economic factors, competitive factors, metal prices, relationships with vendors and strategic partners, governmental regulations and oversight, permitting, seasonality and weather, technological change, industry practices, uncertainties involved in the interpretation of drilling results and laboratory tests, and one-time events. The Company assumes no obligation to update forward ‐ looking statements or beliefs, opinions, projections or other factors, except as required by law.

Contact:
Brandon Macdonald
Phone: (604) 646-8361

Map 1: Macmillan Pass and Mactung location map: https://www.globenewswire.com/NewsRoom/AttachmentNg/691f034b-73de-4594-b9de-03dffcfcee0d

Map 2: Boundary Zone drilling map: https://www.globenewswire.com/NewsRoom/AttachmentNg/77a0fb6a-fa6e-4d56-a0f2-6d87d4f54353

Cross Section E-E': Results from NB22-006 and historic Cominco hole NB90-20: https://www.globenewswire.com/NewsRoom/AttachmentNg/431c4b3b-b487-47a7-a05a-dcc77bc16c8f

Table 2: Summary of drill results from 2022 program.

Drill hole	Zone	Hole length (m)	Significant intersections	Type
NB22-001	BW	463	Reported in Nov. 22, 2022 news release	Infill & Step-out
NB22-002	BW	491	Reported in Nov. 22, 2022 news release	Step-out & New Discovery
NB22-003	BW	64	Hole abandoned	-
NB22-004	BW	403	Moderate zone	Step-out
NB22-005	BM	326	Reported in this release	Step-out
NB22-006	BM	375	Reported in this release	Step-out
NB22-007	BW	365	Narrow zones	Step-out
NB22-008	BM	213	Reported in this release	Step-out & New Discovery
NB22-009	BM	147.5	Wide zone	Infill
NB22-010	BM	91	Wide zone	Infill
NB22-011	BM	265.3	Wide zone	Infill & Step-out
NB22-012	BM	353	Wide zone	Step-out
NB22-013	BM	125.4	Moderate zone	Infill
NB22-014	BM	31	Hole abandoned	-
NB22-015	BM	145	Moderate zone	Infill
NB22-016	BM	57.4	Hole abandoned	-
NB22-017	BM	80	Wide zone	Infill
NB22-018	BM	270	Wide zone	Infill, Step-out & New Discovery
NB22-019	BW	340	Wide zone	Infill & Step-out
NB22-020	BM	149	Wide zone	Infill
NB22-021	BM	112	Wide zone	Infill
NB22-022	BM	327	Wide zone	Step-out & New Discovery
NB22-023	BM	367	Wide zone	Step-out & New Discovery
TS22-001	TW	200	Wide zone	Infill
TS22-002	TE	170.9	Wide zone	Infill
TS22-003	TW	125	Wide zone	Infill
TS22-004	TW	214.2	Wide zone	Infill
TS22-005	TW	128	Wide zone	Infill
TS22-006	TW	190.5	Wide zone	Infill
TS22-007	TW	86	Wide zone	Infill
TS22-008	TW	61	Wide zone	Infill
TS22-009	TW	335	Wide zone	Infill

All assays pending unless otherwise indicated. BM: Boundary Main; BW: Boundary West; TW: Tom West; TE: Tom East.

Table 3: 2022 Drill Collar Details.

Drill hole	Target	Length (m)	Easting	Northing	Elevation (m.s.l)	Azimuth (°)	Dip (°)
NB22-001	Boundary	463	421861	7010461	1178	030	-58
NB22-002	Boundary	491	421940	7010405	1164	033	-57
NB22-003	Boundary	64	422105	7010683	1238	211	-76
NB22-004	Boundary	403	422105	7010683	1238	211	-76
NB22-005	Boundary	326	422230	7010524	1193	214	-50
NB22-006	Boundary	375	422539	7010536	1195	207	-55
NB22-007	Boundary	365	421940	7010405	1164	036	-47
NB22-008	Boundary	213	422274	7010600	1217	209	-68
NB22-009	Boundary	147.5	422438	7010417	1165	208	-50
NB22-010	Boundary	91	422390	7010385	1152	205	-50
NB22-011	Boundary	265.3	422440	7010419	1164	208	-69
NB22-012	Boundary	353	422342	7010620	1219	201	-65
NB22-013	Boundary	125.4	422390	7010386	1150	205	-70
NB22-014	Boundary	31	422330	7010384	1146	212	-50
NB22-015	Boundary	145	422331	7010385	1146	212	-75
NB22-016	Boundary	57.4	422330	7010384	1146	212	-55
NB22-017	Boundary	80	422331	7010385	1147	212	-85
NB22-018	Boundary	270	422308	7010434	1166	216	-58
NB22-019	Boundary	340	421948	7010672	1232	180	-57
NB22-020	Boundary	149	422308	7010435	1166	216	-72
NB22-021	Boundary	112	422309	7010435	1167	216	-82
NB22-022	Boundary	327	422292	7010474	1182	211	-56
NB22-023	Boundary	367	422292	7010474	1182	211	-70
TS22-001	Tom West	200	441994	7003679	1545	060	-80
TS22-002	Tom East	170.9	442063	7004322	1677	060	-90
TS22-003	Tom West	125	441994	7003680	1545	065	-55
TS22-004	Tom West	214.2	441993	7003679	1545	065	-89
TS22-005	Tom West	128	442046	7003767	1533	063	-50
TS22-006	Tom West	190.5	442044	7003582	1581	049	-75
TS22-007	Tom West	86	441943	7003969	1538	066	-80
TS22-008	Tom West	61	441945	7003970	1538	066	-45
TS22-009	Tom West	335	442043	7003581	1581	049	-89

Coordinate reference system: UTM Zone 9 NAD83. North reference: UTM grid north.

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Altair Minerals Limited New Central Porphyry System Identified at Venatica

Sydney, Australia (ABN Newswire) - Altair Minerals Limited (ASX:ALR) (OTCMKTS:CHKMF) is pleased to announce preliminary findings following a site visit where the Company has identified a significant outcrop of stockwork system at Central Porphyry. Outcropping quartzite, magnetite and secondary biotite veined porphyry stockwork which is part of a new separate Central Porphyry - 3km Southwest of the high-grade Irka NE Porphyry.

Key Highlights:

- Identification of new Central Porphyry | Venatica West a Porphyry Cluster

Site visit has discovered a significant outcrop of leached porphyry stockwork and ultra-potassic vein system which identifies a Central Porphyry intrusive part of a cluster system at Venatica West. Typical alteration and veining present within Bornite-Gold rich Copper Porphyry systems.

- Extremely dense veining and stockwork | Multi-stage Mineralisation

Stockwork of A-type quartz, magnetite and secondary biotite on Central Porphyry is the densest identified to date across Venatica West, suggesting significant hydrothermal activity, overlapping events, fracturing and multi-stage mineralisation at Central Porphyry, ideal for copper enrichment.

- Small portion of a much larger system | Central Porphyry Remains Open

Identification of Central Porphyry is an outstanding outcome, due to only a portion of the potassic stockwork zone outcropping, which could've easily been missed. Ultra-potassic alteration with dense stockwork as seen within this outcrop, generally tends to expand kilometres, with remaining footprint of alteration sitting under soil cover. Further fieldwork can identify full extent of this Central Porphyry.

- Potential for regional Porphyry system | SW - NE Regional Porphyry System

Preliminary fieldwork analysis on-going, with already a new Central Porphyry system being identified within virgin grounds at Venatica West, sitting ~3km Southwest of the high-grade Irka NE Porphyry and ~2km Northeast of the Irka SW Porphyry-Skarn system. Suggestive of a regional SW to NE trending porphyry cluster, filling the intersection of two district faults.

- Community Engagement Commenced | Early Community Approval

Early engagement has commenced with the local community, with multiple local members showing support for on-going exploration works. Altair's exploration team has also met with the President of the Community with very positive preliminary discussions. Altair has received initial community approval for exploration works with intention of putting forward long-term proposal of work programs, community incentive programs, project scheduling and local training.

Discovery of New Central Porphyry at Venatica West

The Central Porphyry is located on the Irka permit, situated ~3km southwest of the high-grade Irka NE Porphyry target and is a new intrusion system identified within Venatica West during initial site visit.

The upper zone of a new Central Porphyry has been identified through outcrop which consists of leached ultra-potassic stockwork of quartz, magnetite and secondary biotite dense veining, and surrounded by phyllic alteration halo and hosted within overprinted argillic alteration.

The ultra-potassic alteration suggests Altair is standing above the core of the Central Porphyry. The overprinting of strong argillic alteration has occurred from later stage hydrothermal fluids which has replaced the feldspars with clay material while maintaining the stockwork veining - suggesting a multistage mineralisation event which can significantly enrich the grades of copper sulphide and hypogene zone below. This leached stockwork from late-stage argillic alteration indicates the copper has been remobilized and disseminated into structurally favourable zones below, with potential to enhance grades within the contacts and breccia's at the core of the Central Porphyry.

The ultra-potassic zone generally sits right above the core of a Porphyry intrusion and in the case of the Central Porphyry, it is the densest set of stockwork, and veinlets discovered so far at Venatica West, with high alteration suggesting this area is the key part of hydrothermal activity and potentially the feeder to multiple other Porphyry systems.

The presence of dense secondary biotite veining on altered ultra-potassic outcrop not only indicates the presence of a new Porphyry system sitting below but also is an essential element for developing a large-scale Porphyry deposit within this particular belt.

Within other billion-tonne deposits proximal to Venatica, the presence of secondary biotite into the plays a key role in developing "scale" as its presence within porphyry stock and outwards into diorite host rock, tends to allow substitution of Fe2+ and Mg2+ with Cu2+, which can extend the copper mineral deposit footprint by a further ~500m radius in each direction from the main Porphyry core.

Key Takeaways

- Identification of new Central Porphyry akin to Bornite-Gold rich Copper Porphyries

- Ultra-potassic stockwork suggests we are standing above the core of the system

- Argillic overprint indicates a later-stage hydrothermal fluid enacted on Central Porphyry, leading to multi-phase mineralisation events.

- Leached outcrop, indicates copper has re-mobilized below into more structurally favourable zones allowing secondary enrichment in the porphyry core - which leads to higher grades.

- Presence of secondary biotite halo zone and veining in porphyry stock & diorite host is critical in developing scale within this belt for a large Cu-Au mineralisation zone beyond just the porphyry core.

- Structural alignment in SW-NE direction hosting a regional copper porphyry cluster. Irka NE Porphyry, the Central Porphyry and the SE Porphyry makes a potential corridor over more than 10km length.

This new Porphyry discovery adds on to the targets at Venatica, with 4x highly prospective undrilled targets for discovery being uncovered in this new district which is an extension of the belt which hosts multiple billion-tonne copper deposits, these targets at Venatica currently include:

- Irka NE Porphyry: Over 3.4km strike, with high-grade samples including:

- 7.0% Copper and 33g/t Silver
- 5.7% Copper and 43g/t Silver

- Irka SE Porphyry-Skarn: Large 6km2 anomalous area, with high-grade samples including:

- 4.8% Copper & 0.40g/t Gold
- 6.5% Copper & 0.52g/t Gold

- Central Porphyry: Newly discovered initial outcrop from field visit, part of a significantly larger system sitting under colluvial and soil cover. Ultra-potassic and advanced argillic alteration with significant stockwork and veining part of a separate porphyry intrusive.

- Venatica East: Over 17km of anomalous strike of copper stream sediments which are 5x background levels. Virgin grounds with potential to identify source of copper mineralisation feeding the streams and new major targets.

The identification of this Central Porphyry is significant and a result of the diligent fieldwork of the exploration team, as the outcrop is exposed over a minimal area and could've easily been missed. The degree of stockwork veining and hydrothermal activity suggests this alteration likely expands kilometres in each direction - with most of it sitting under post-mineral soil cover. Further detailed mapping and fieldwork will look to identify the true extent of this potassic alteration zone.

Venatica West is shaping up to be a regional porphyry system, hosting numerous high-quality targets for discovery. The Central Porphyry sits ~3km southwest of Irka NE and ~2km northeast of Irka SW, which indicates a structurally controlled regional porphyry trend SW - NE at Venatica West.

Community Engagement

Altair has received positive initial feedback from the community regarding its preliminary exploration activities and future plans. The community board has provided their approval and remains supportive with great relations built with local miners in the region who are eager for Altair to continue further exploration work.

Altair has also had an introduction and a very positive initial meeting with the President of the local community. Following from this, Altair representatives attended the initial community meeting and received approval to continue exploration works, with local members ready to assist. Altair continues to build upon existing supportive relationships within the community and will seek to provide a longterm formal proposal of its anticipated work programs, community incentive programs, project scheduling and local training. This proposal will be reviewed by the local community and President and will then be used to form the basis of monthly meetings with the community to build upon existing support.

Altair believes its early approach to engage the community and developing upon relationships which have been built over 10-years by the vendor of Irka will be key in fast-tracking exploration and development programs. Furthermore, this engagement is key to Altair's ESG core values and is expected to pay dividends in the future for both the Company and community. The early engagement with the community will also be critical in ensuring a smooth transition into its discovery programs.

Steps Forward at Venatica

The key anticipated steps forward aim to establish maximum value for shareholders through a scientific, systematic and diligent approach to exploration with the target of making a large-scale and globally significant discovery.

Venatica sits in the right the geological formation with all the key indicators capable of making such discovery. Altair plans to immediately initiate a comprehensive program to further evaluate the full potential of Venatica. The next key steps as part of the Venatica execution program includes:

- Evaluation of regional potential and detailed mapping

- On-going community engagement at Venatica West & Venatica East

- Rock chip and geochemical sampling program at Venatica West

Altair Chief Executive Officer, Faheem Ahmed comments:

"This is an outstanding find by our geological team within the high-grade Venatica Copper Project. This is now our third Porphyry target at Venatica West, and we are treading virgin and unexplored grounds here with potential to discover further mineralised outcrops and Porphyry's.

There is consistent dense veining across the outcrop which is exactly what you would like to see within a porphyry intrusion, suggesting significant magmatic fluid activity. More importantly, it appears the Central Porphyry has gone through multi-stage mineralisation, which not only introduces more copper into the intrusion, but also indicates copper has been leached from the outcrop and has potential to go through secondary enrichment below. These are all key indicators we are onto an exceptional exploration target, both with scale and potential to be high-grade.

We now have three key targets at Venatica West, two of them which has shown exceptional copper grades ranging 4 - 9% at surface across a large area. With the latest addition being this Central Porphyry, which has gone through significant leaching. Due to the leaching, we're looking for anomalous levels of copper at surface within the Central Porphyry, which will confirm to us this stockwork is likely to be significant mineralised at depth from remobilization of copper ions.

Furthermore, we are yet to even touch Venatica East, which hosts 17km strike of anomalous copper stream sediments. I'm incredibly excited to get boots on ground at Venatica East which is a pure greenfield opportunity and has never been systematically treaded or even sampled, and no one has ever followed up these prominent copper anomalies. We'll be the first Company to take an experienced geological team down to Venatica East, so the possibilities and upside is quite endless.

Simultaneously, we continue to progress works at Olympic Domain, our latest announcement on the project, 4 December 2024, has indicated a robust conductive ovoid, with historic drilling narrowly missing the core of the target. We are in intending to complete a follow-up TEM survey which can identify the precise depth of this ovoid, which will be critical for our drill program and targeting."

*To view tables and figures, please visit:
https://abnnewswire.net/lnk/BB53832O

About Altair Minerals Limited:

Altair Minerals Limited (ASX:ALR) (OTCMKTS:CHKMF) is listed on the Australian Securities Exchange (ASX) with the primary focus of investing in the resource sector through direct tenement acquisition, joint ventures, farm in arrangements and new project generation. The Company has projects located in South Australia, Western Australia and Queensland with a key focus on its Olympic Domain tenements located in South Australia.

Source:
Altair Minerals Limited

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Vertex Minerals Limited Strengthens Board with Appointment of Mining Executive Sean Richardson

Perth, Australia (ABN Newswire) - Vertex Minerals Limited (ASX:VTX) (OTCMKTS:VTXXF) is pleased to announce the appointment of experienced mining executive Sean Richardson as an Independent Non-Executive Director.

Details of Mr Richardson's qualifications and experience are as set out below.

Commenting on the appointment, Chairman Roger Jackson said:

We are delighted to have Sean joining the Vertex Board at such an exciting time for the Company as we transition into high-grade gold production from stockpiles at Reward and beyond. He brings a wealth of relevant experience and we expect him to supplement the existing Board and Management team well.

SEAN RICHARDSON

MEng MSc MBA FAusIMM MEIAust GAICD

Sean Richardson is a mining professional with a career spanning over 30 years. Mr Richardson experience extends from operations through to consultancy and managerial roles where he has been involved in the exploration and development of mineral projects in Australia, North America, Africa, South-East and Central Asia.

Mr Richardson's notable roles include Managing Director of Empire Resources (ASX:ERL), Chief Operating Officer for Bardoc Gold (ASX:BDC) and Operations Manager for Shaw River Manganese (ASX:SRR).

Mr Richardson is passionate about the mining industry and its role in the advance of society, an enthusiasm that has led Mr Richardson to a seek out and attain greater knowledge of the global minerals industry.

Mr Richardson holds a Master of Engineering Technology (Mining Engineering), a Master of Business Administration (Curtin), a Master of Science in Mineral Economics (WASM), a Graduate Diploma in Mining (WASM) and an Advanced Diploma in Engineering and Mine Surveying (TAFE).

Mr Richardson is also a Graduate Member of the Australian Institute of Company Directors (GAICD), a Fellow of the Australasian Institute of Mining and Metallurgy (FAusIMM) and a Member of Engineers Australia (MEIAust).

About Vertex Minerals Limited:

Vertex Minerals Limited (ASX:VTX) is an Australian based gold exploration company developing its advanced Hargraves and Hill End gold projects located in the highly prospective Eastern Lachlan Fold Belt of Central West NSW. Other Company assets include the Pride of Elvire gold project and Taylors Rock gold/nickel/lithium project both located in the Eastern Goldfields of WA. The focus of Vertex Minerals is to advance the commercial production of gold from its NSW projects embracing an ethical and environmentally sustainable approach.

Source:
Vertex Minerals Limited

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Questcorp Mining Announces Private Placement

Questcorp Mining Inc. (CSE: QQQ) (the "Company" or "Questcorp") is pleased to announce that it intends to complete a non-brokered private placement offering (the "Offering") of up to 33,000,000 units (each, a "Unit") at a price of $0.06 per Unit for gross proceeds of $1,980,000. Each Unit will consist of one common share of the Company and one common share purchase warrant entitling the holder to acquire a further common share of the Company at a price of $0.10 per share for a period of two years.

The net proceeds of the Offering will be used by the Company to complete the acquisition of the La Union Project from Riverside Resources Inc., (see news release dated September 6, 2024), to continue a small exploration program at its North Island Copper Property, to retire existing payables and for general working capital purposes. Finders' fees or commissions may be paid in connection with the completion of the Offering, and all securities issued in the Offering will be subject to a four-month-and-one-day statutory hold period.

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Group Eleven Intersects 15.6m of 11.6% Zn+Pb, 122 g/t Ag and 0.19% Cu, incl. 3.5m of 21.3% Zn+Pb, 395 g/t Ag and 0.73% Cu at Ballywire; Silver and Copper Values Continue to Impress

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) ("Group Eleven" or the "Company") is pleased to announce results from the latest two holes of the ongoing drill program at the Company's 100%-owned Ballywire zinc-lead-silver discovery ("Ballywire"), PG West Project ("PG West"), Republic of Ireland.

Highlights:

G11-3552-27 intersected (from 213.0m):
- 24.8m of 8.1% Zn+Pb (5.8% Zn and 2.3% Pb), 80 g/t Ag and 0.12% Cu, including
- 15.6m of 11.6% Zn+Pb (8.3% Zn and 3.3% Pb), 122 g/t Ag and 0.19% Cu, including
- 6.6m of 16.7% Zn+Pb (11.1% Zn and 5.7% Pb), 240 g/t Ag and 0.42% Cu, including
- 3.5m of 21.3% Zn+Pb (13.3% Zn and 8.0% Pb), 395 g/t Ag and 0.73% Cu
- Located in middle of 270m gap between two previously released drill fences
G11-3552-25 intersected (from 187.2m):
- 16.2m of 2.8% Zn+Pb (2.1% Zn and 0.7% Pb) and 8 g/t Ag, including
- 4.6m of 7.4% Zn+Pb (5.6% Zn and 1.8% Pb) and 21 g/t Ag, including
- 1.9m of 12.9% Zn+Pb (9.6% Zn and 3.3% Pb) and 39 g/t Ag
- Located 50m NNW from G11-3552-27
Above results confirm the extent of the recently announced flat-lying zone of zinc-rich massive sulphide lenses at least 360m along strike and remaining open to the NE
Massive sulphide zone is pierced by G11-3552-27 and seven previously released holes, of which three are referenced below:
- G11-3552-12: 29.6m of 10.6% Zn+Pb and 78 g/t Ag (released 11-Jun-24)
- G11-3552-18: 11.8m of 11.6% Zn+Pb and 48 g/t Ag (released 22-Oct-24)
- G11-3552-19: 15.3m of 14.5% Zn+Pb and 56 g/t Ag (released 14-Nov-24)
Drilling continues at Ballywire with two rigs testing further down-dip of the two holes released today, plus the NE extension; assay results are expected in due course

"It is great to see the NE massive sulphide zone now consistently intersected by eight high-grade holes over a strike length of 360m and open to the NE," stated Bart Jaworski, CEO. "Excellent silver and significant copper values are also noteworthy because they increasingly point to a stratigraphically deeper horizon known to be highly prospective for copper and silver in this part of Ireland. Namely, the Gortdrum Cu-Ag mine, active in the 1960s and 70s, is located 10km NE of Ballywire, whereas, the Denison and Tullacondra Cu-Ag historic occurrences are 5km SE and 45km SW of Ballywire, respectively. A deeper Cu-Ag horizon at Ballywire is one of our key targets for 2025.

Our two other key targets include: (i) exploration drilling along strike from the drilled 2.6km-long discovery area towards the encompassing 6km long prospective trend and (ii) up and down dip from the discovery trend in search of parallel zones of mineralization. We eagerly await results from drilling down dip of today's results and along the NE extension."

Exhibit 1. Cross-Section A-A' of G11-3552-25, -27 (Filling In 270m Gap Between Fences) at Ballywire

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/239839_figure1.png

Exhibit 2. Plan Map Showing Key New Drilling (G11-3552-25, -27) at Ballywire

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/239839_figure2.png

Exhibit 3. Emerging Massive Sulphide Zone and Upcoming Drill Results at Ballywire

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/239839_5ca5f11594e49b67_004full.jpg

Recent Holes from Ballywire Discovery

The Ballywire prospect at the Company's 100%-owned PG West Project in Republic of Ireland, is a relatively new zinc-lead-silver discovery (first announced Sept-2022). In addition to 42 holes drilled and reported by Group Eleven to date, the most recent two holes (G11-3552-25 to -27) are reported today (see Exhibits 1 to 6). Note, a second batch of assays totalling over 50m within G11-3552-27 is still pending.

High-grade mineralization from G11-3552-25 and -27 consists predominantly of massive and semi-massive sulphide (sphalerite, galena, pyrite, chalcopyrite and suspected tennantite-tetrahedrite), as well as, disseminated and vein hosted sulphide mineralization. Mineralization occurs along and/or close to the base of the Waulsortian Limestone (see Exhibit 1).

Exhibit 4. Summary of Assays from G11-3552-25 and -27 at Ballywire

Item	From (m)	To (m)	Int (m)	Zn (%)	Pb (%)	Zn+Pb (%)	Ag (g/t)	Cu (%)
G11-3552-25	187.15	203.35	16.20	2.14	0.69	2.83	8.00	-
Incl.	187.15	195.51	8.36	3.59	1.11	4.70	14.49	-
Incl.	190.87	195.51	4.64	5.59	1.82	7.41	20.97	-
Incl.	192.69	194.60	1.91	9.59	3.32	12.92	39.19	-
G11-3552-27	213.00	237.81	24.81	5.84	2.28	8.11	80.4	0.12
Incl.	219.42	235.06	15.64	8.30	3.28	11.59	122.1	0.19
Incl.	219.42	222.21	2.79	15.57	3.77	19.35	92.79	0.03
And	228.51	235.06	6.55	11.06	5.65	16.71	240.0	0.42
Incl.	230.36	233.90	3.54	13.26	8.01	21.27	395.1	0.73

Note: True width of the overall mineralized package in all holes above is estimated at approx. 90-100% of the intersected interval

Overall, recent drilling suggests the emergence of two distinct styles of mineralization. First, relatively flat-lying zinc-rich massive sulphide lenses and second, 'other high-grade mineralization', dominated by variably dipping massive sulphides, as well as, vein-hosted and disseminated mineralization (see Exhibits 1-3). Both styles occur at or near the base of the Waulsortian Limestone and offer great exploration opportunities as drilling progresses.

Looking forward, seven (7) drill holes (G11-3552-24, -26, -28 and 29 to -32; see Exhibit 3) are in progress with results expected in due course. Exhibit 3 shows drilling to date across 1.25km of the overall 2.6km long trend (see Exhibit 2) of significantly mineralized drill intercepts (open in all directions). This in turn is hosted within a 6km long prospective trend defined by four gravity high anomalies, only one of which (anomaly 'C') is systematically drilled to date (see Exhibit 5).

Exhibit 5. Regional Gravity at Ballywire Showing 6km Long Prospective Trend

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/239839_figure5.png

Notes to Exhibit 6: (a) Pallas Green MRE is owned by Glencore (see Glencore's Resources and Reserves Report dated December 31, 2023); (b) Stonepark MRE: see the 'NI 43-101 Independent Report on the Zinc-Lead Exploration Project at Stonepark, County Limerick, Ireland', by Gordon, Kelly and van Lente, with an effective date of April 26, 2018, as found on SEDAR; and (c) the historic estimate at Denison was reported by Westland Exploration Limited in 'Report on Prospecting Licence 464' by Dermot Hughes dated May, 1988; the historic estimate at Gortdrum was reported in 'The Geology and Genesis of the Gortdrum Cu-Ag-Hg Orebody' by G.M. Steed dated 1986; and the historic estimate at Tullacondra was first reported by Munster Base Metals Ltd in 'Report on Mallow Property' by David Wilbur, dated December 1973; and later summarized in 'Cu-Ag Mineralization at Tullacondra, Mallow, Co. Cork' by Wilbur and Carter in 1986; the above three historic estimates have not been verified as current mineral resources; none of the key assumptions, parameters and methods used to prepare the historic estimates were reported and no resource categories were used; significant data compilation, re-drilling and data verification may be required by a Qualified Person before the historic estimates can be verified and upgraded to be compliant with current NI 43-101 standards; a Qualified Person has not done sufficient work to classify them as a current mineral resource and the Company is not treating the historic estimates as current mineral resources. 'Rathdowney Trend' is the south-westerly projection of the Rathdowney Trend, hosting the historic Lisheen and Galmoy mines.

Exhibit 6. Regional Map of PG West (100% Interest) and Stonepark (77.64% Interest)

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/239839_figure6.png

Note: Two westernmost prospecting licenses were surrendered in December 2024 from the Stonepark Project, reflecting decreasing prospectivity and the Company's preference to focus on core prospects (Ballywire and Carrickittle West)

Consultant

The Company has engaged ProConsul Capital Ltd. ("ProConsul") to provide investment marketing consulting services (the "Services") commencing February 6th, 2025. In consideration for the Services, the Company will pay a fee of C$6,000/month and has agreed to grant stock options to ProConsul, the number and terms of which stock options will be determined at a later date. The agreement is subject to TSX Venture Exchange acceptance and renewable on a month-to-month basis unless terminated by either party on 30 days written notice.

Qualified Person

Technical information in this news release has been approved by Professor Garth Earls, Eur Geol, P.Geo, FSEG, geological consultant at IGS (International Geoscience Services) Limited, and independent 'Qualified Person' as defined under Canadian National Instrument 43-101.

Quality Assurance/Quality Control (QA/QC) Information

Group Eleven inserts certified reference materials ("CRMs" or "Standards") as well as blank material, to its sample stream as part of its industry-standard QA/QC programme. The QC results have been reviewed by the Qualified Person, who is satisfied that all the results are within acceptable parameters. The Qualified Person has validated the sampling and chain of custody protocols used by Group Eleven.

About Group Eleven Resources

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) and (FSE: 3GE) is a mineral exploration company focused on advanced stage zinc exploration in the Republic of Ireland. Group Eleven announced the Ballywire discovery in September 2022. Key intercepts to date include:

10.8m of 10.0% Zn+Pb and 109 g/t Ag (G11-468-03)
10.1m of 8.6% Zn+Pb and 46 g/t Ag (G11-468-06)
10.5m of 14.7% Zn+Pb, 399 g/t Ag and 0.31% Cu (G11-468-12)
11.2m of 8.9% Zn+Pb and 83 g/t Ag (G11-3552-03)
29.6m of 10.6% Zn+Pb, 78 g/t Ag and 0.15% Cu (G11-3552-12) and
11.8m of 11.6% Zn+Pb, 48 g/t Ag (G11-3552-18)
15.6m of 11.6% Zn+Pb, 122 g/t Ag and 0.19% Cu (G11-3552-27)

Ballywire is located 20km from Company's 77.64%-owned Stonepark zinc-lead deposit¹, which itself is located adjacent to Glencore's Pallas Green zinc-lead deposit². The Company's two largest shareholders are Glencore Canada Corp. (17.1% interest) and Michael Gentile (16.5%). Additional information about the Company is available at www.groupelevenresources.com.

ON BEHALF OF THE BOARD OF DIRECTORS
Bart Jaworski, P.Geo.
Chief Executive Officer

E: b.jaworski@groupelevenresources.com | T: +353-85-833-2463
E: j.webb@groupelevenresources.com | T: 604-644-9514

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Information

This press release contains forward-looking statements within the meaning of applicable securities legislation. Such statements include, without limitation, statements regarding the future results of operations, performance and achievements of the Company, including the timing, content, cost and results of proposed work programs, the discovery and delineation of mineral deposits/resources/ reserves and geological interpretations. Although the Company believes that such statements are reasonable, it can give no assurance that such expectations will prove to be correct. Forward-looking statements are typically identified by words such as: believe, expect, anticipate, intend, estimate, postulate and similar expressions, or are those, which, by their nature, refer to future events. The Company cautions investors that any forward-looking statements by the Company are not guarantees of future results or performance, and that actual results may differ materially from those in forward looking statements as a result of various factors, including, but not limited to, variations in the nature, quality and quantity of any mineral deposits that may be located. All of the Company's public disclosure filings may be accessed via www.sedar.com and readers are urged to review these materials, including the technical reports filed with respect to the Company's mineral properties.

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Fireweed Drills 12.5 m of 11.17% Zinc including 6.2 m of 15.84% Zinc at Boundary Main

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