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Quantum Critical Metals Reports 150 Meters of 38GPT Gallium, 694GPT Rubidium, 72GPT Niobium, 8GPT Cesium, and 9GPT Tantalum from Diamond Drilling at Discovery Project, Quebec

Drill Results

PO BOX 31880

Steveston Village, BC, V7E 0B5, Canada

tel: 604.428.2900

[email protected]

www.quantumcriticalmetals.com

QUANTUM CRITICAL METALS REPORTS 150 METERS OF 38GPT GALLIUM, 694GPT RUBIDIUM,

72GPT NIOBIUM, 8GPT CESIUM, AND 9GPT TANTALUM FROM DIAMOND DRILLING AT

DISCOVERY PROJECT, QUEBEC

Vancouver, BC / April 9th, 2025 / The Newswire – Quantum Critical Metals Corp. (TSX.V: LEAP) (OTCQB:

ATOXF) (Frankfurt: 86A1) (“Quantum” or the “Company”) is pleased to announce that it has re-examined

its drill core assays at its 100% owned Discovery project, located in the Eeyou Istchee (James Bay) region

of Québec, and has discovered elevated and consistent intervals of gallium, rubidium, cesium, niobium,

and tantalum. Notably, the Company intersected:

● 37gpt gallium, 936gpt rubidium, 72gpt niobium, 8gpt cesium, and 10gpt tantalum over 30

meters from 9m to 39m.

● 38gpt gallium, 694gpt rubidium, 72gpt niobium, 8gpt cesium, 9gpt tantalum over 150 meters

from 44 to 194 meters.

● 37gpt gallium, 651gpt rubidium, 57gpt niobium, 15gpt cesium, 11gpt tantalum over 73 meters

from 17 to 90 meters.

● 44gpt gallium, 801gpt rubidium, 66gpt niobium, 16gpt cesium, 36gpt tantalum over 43 meters

from 16 to 59 meters.

The Company’s 2018 and 2022 drill programs totalled approximately 2,432 meters, and 1,696 meters

respectively, for a total of 4,128 meters across 22 holes (Figure 1). These programs were originally initiated

for gold exploration, but given recent geopoliti cal developments regarding critical metals, the Company

revisited these results to investigate any further potential that may exist than what was originally

considered in the past.

As a function of this review, management believes it has uncovered its second gallium -rubidium-cesium

discovery, joining the NMX East gallium -rubidium-cesium project in the Company’s portfolio

https://www.quantumcriticalmetals.com/blogs/news/durango-reports-107-68-meters-of-38-85-gpt-

gallium-701-gpt-rubidium-24-98-gpt-cesium-and-3-61-gpt-thallium-from-surface-in-diamond-drilling-at-

nmx-east-critical-metals-project. The zones containing anomalous gallium, rubidium, cesium, tantalum

and niobium were mostly pegmatite dykes, however several intercepts contained metasediments, granite

and granophyre rock types. Meanwhile the Company has also identified indicators of a potential VMS

system intersecting these results, including anomalous lead-copper-zinc, which management believes also

warrant further attention and investigation. The Company is encouraged by these results and will provide

more detail once this additional review has been completed.

Summaries of both these drill program results and the Discovery project are below. Access to the full

results are available on the Company’s website at

https://www.quantumcriticalmetals.com/pages/discovery-polymetallic-project-quebec

PO BOX 31880

Steveston Village, BC, V7E 0B5, Canada

tel: 604.428.2900

[email protected]

www.quantumcriticalmetals.com

Figure 1. Discovery property 2018 and 2022 drill program locations.

PO BOX 31880

Steveston Village, BC, V7E 0B5, Canada

tel: 604.428.2900

[email protected]

www.quantumcriticalmetals.com

Summary of Discovery Drill Results

Table 1. 2018 Drill hole intervals with gallium, rubidium, niobium, cesium and tantalum.

PO BOX 31880

Steveston Village, BC, V7E 0B5, Canada

tel: 604.428.2900

[email protected]

www.quantumcriticalmetals.com

Table 2. 2022 Drill hole intervals with gallium, rubidium, niobium, cesium and tantalum.

PO BOX 31880

Steveston Village, BC, V7E 0B5, Canada

tel: 604.428.2900

[email protected]

www.quantumcriticalmetals.com

Table 3. Discovery Property drill hole coordinates, lengths, and orientation.

PO BOX 31880

Steveston Village, BC, V7E 0B5, Canada

tel: 604.428.2900

[email protected]

www.quantumcriticalmetals.com

Figure 2. Discovery property 2018 and 2022 drill program locations and claim area map.

Assay QA/QC

Drill core was sawed in half and core samples were collected every 1 metre. Samples were not collected

across lithology types. Geological plastic bags were used with sample tags placed inside the bag and the

sample ID was written on the outside of the bag using waterproof marker.

In 2018 the samples were shipped to ALS Canada Ltd in Val D’Or for gold and multi-element analysis. Gold

was analysed by fire assay with an ICP-AES finish. Multi elements were analysed by Aqua Regia digestion

and ICP-AES.

PO BOX 31880

Steveston Village, BC, V7E 0B5, Canada

tel: 604.428.2900

[email protected]

www.quantumcriticalmetals.com

In 2022 the samples were sent to Northern Mining Analytical Laboratory (NMAL) in Timmins, Ontario for

gold fire assay – atomic absorption spectrometry and gravimetric analysis. The samples were then sent

on to Activation Laboratories in Ancaster, Ontario. Samples were digested using sodium peroxide fusion

and analysed for trace elements using ICP -OES/MS. For the drilling campaign , a blank, standard and

duplicate were inserted every 30 samples.

A review of the QAQC samples submitted during the drilling campaigns was completed. QAQC samples

were submitted every 30 samples in the sample series, alternating between standards, blanks and

duplicate order. Review of the results indicates that acceptabl e levels of error were received from Act

Labs for the sets of QAQC samples.

About the Discovery Project

The 100% owned Discovery Project spans 6,082 hectares and is located southwest of the past producing

Troilus gold and copper mine (TSX-TLG), as well as the Moblan lithium deposit. The Discovery property is

situated in the Frotet-Evans Greenstone belt, a volcanic-sedimentary assemblage which contains a central

sedimentary basin. The Discovery property is located in the eastern region of the belt (Simard,1987;

Brisson et al.,1997; Brisson et al.,1998 a,b,c). Multiple stages of deformation affected the rocks at

Discovery and produced folds with axes of ENE -WSW to EW in orientation and destroy strike slip faults

with an E-W trend.

Several rounds of geophysical surveys (EM and Mag, AMT, Gravity ) and soil geochemistry lines were

completed on the Discovery property from 2013 to 2017. Exploratory drilling was completed in 2018 and

2022 to try to locate the source of the gold occurrences at surface. In 2014, an exploration campaign was

conducted and returned up to 41.6 and 46.6 gpt gold in channels samples located 36 metres apart. Field

mapping was completed in 2022, 2023, and 2024.

The Discovery Property Polymetallic Potential

The Discovery Project covers an important geological NE -SW regional structure and the Company

recognizes this property for its polymetallic potential.

Gold: found within quartz veins hosted within a metabasalt, up to 46.6 g/pt. Historically, elevated gold

contents have been found in veins which appear to have an orange, brown iron -stained appearance and

are typically deformed, sheared and locally folded. These veins vary from <1 cm in size up to 1m+ scales.

The mineralized veins are known to have a West-East orientation and have a steep dip.

Critical Metals : While reviewing the historical drill data and assays of the Discovery Property, the

geological team noticed anomalous gallium, rubidium, niobium, cesium and tantalum values in the drill

core assays. Gallium, rubidium, cesium, tantalum, niobium have been found in 2018 and 2022 drill holes,

hosted mostly in pegmatites. Over 50 pegmatites outcrops have been mapped to date on the property.

The pegmatites of the property occur in multiple orientations but the majority of large outcrops are found

in a NE/SW orientation and NW/SE orientation. Contacts of pegmatites are typically bulbous indicating a

deep and relatively hot emplacement setting but are typically sharp and show little evidence of extensive

host rock contamination of melt from the pristine pegmatite compositions. Pegmatites are heavily

PO BOX 31880

Steveston Village, BC, V7E 0B5, Canada

tel: 604.428.2900

[email protected]

www.quantumcriticalmetals.com

deformed leading to internal flow -like structures which surround large phenocrysts of microclines.

Pegmatite emplacement predates quartz vein formation of the region as quartz veins can be seen cross

cutting pegmatites at several locations.

Base Metals (Zn, Cu, Ni, Pb): several zinc soil anomalies, banded magnetite in outcrop, outcrops containing

massive and breccia in-fill pyrite and pyrrhotite, and possible Cu, Pb, Ni, Zn anomalies in drill core are also

present and require further investigation.

Sources:

Simard, A. 1987. Stratigraphie et volcanisme dans la partie orientale de la bande volcanosédimentaire

archéenne de Frotet-Evans. Ministère des Ressources Naturelles du Québec.MB 87-17, 300 pp

Brisson H., Gaulin, R., Lefebvre, D., Dion, D -J., Gosselin, C. and Beaumier, M. 1997. Géologie dela région

du lac Assinica, Ministère des Ressources Naturelles. RG 96-11, 28pp.

Brisson, H., Gosselin, C., Fallara, F., Gaulin, R., and Dion, D.J. 1998a. Géologie de la région dulac Théodat

(SNRC 32K/16). Ministère des Ressources naturelles du Quebec. RG 98-07, 24pp.

Brisson, H., Gosselin, C., Fallara, F., Gaulin, R., and Dion, D.J. 1998b. Géologie de la région dulac Evans

(SNRC 32K/15). Ministère des Ressources naturelles du Quebec. RG 98-06, 23pp.

Brisson, H., Gosselin, C., Fallara, F., Gaulin, R., and Dion, D.J. 1998c. Géologie de la région du lac Rocher

(SNRC 32K/09). Ministère des Ressources naturelles du Québec. RG 98-05, 22pp.

Discovery Project Gallium Comparable

The Cordero Deposit in Nevada is possibly the only primary gallium project with a well -defined resource

(15 Mt at 47.7 ppm gallium). Gallium mineralization here is associated with low -sulfidation epithermal

silver-mercury deposits, with Ga hosted in alunit e (KAl(SO 4)2(OH)6) and other aluminous phosphate

minerals.

Source: https://www.geologyforinvestors.com/gallium-the-unicorn-of-critical-mineral-deposits/

Why This Project Matters:

● Breakthrough Discovery in Critical Metals: The Discovery Project now hosts confirmed intervals

of gallium, rubidium, cesium, niobium, and tantalum—strategic critical metals essential to global

supply chains and energy transition technologies.

● Strengthening North American Critical Mineral Security: With China’s recent export restrictions

on several critical elements, discoveries like this in Canada are vital to national and allied efforts

to localize and secure supply chains.

● High-Grade and Long Intervals: Assays returned consistent, elevated grades across long

intercepts—up to 150 meters—with particularly impressive grades of rubidium, gallium, and