Musk Metals Corp. announced that approximately 100% of the remote sensing work is now completed at Ile Interdite Lithium Property, strategically located in James Bay, Quebec. The Ile Interdite property consists of 20 claims covering 1,089 hectares (10.9 km2) and extends over 5 km along the Nottaway River Shear Zone, a prominent regional structure that can be followed over 200 km.

Ile Interdite is near the contact between the Nemiscau Sedimentary and the Opatica Pluto-Volcanic Sub-Provinces, consisting of paragneiss and amphibolite rocks. The Ile InterdITE property hosts an important beryl showing that was identified in the 1960's by the same group of Quebec government geologists who reported spodumene at both Whabouchi and Cyr deposit's locations. Beryl is a relatively rare pathfinder mineral for lithium, often observed in pegmatites.

At Ile Interdite, beryl is disseminated in a pegmatite. The Ile Interdites showing is roughly 200 m southwest of the Nottaway River SheAR Zone. Satellite Imagery Study Results.

A total of 14 potential pegmatite dykes were identified and outlined, appearing as dome shaped linear features with positive relief. A sharp contrast with surrounding host rocks can also be observed and potential dykes are either oriented east-west, parallel or nearly parallel to the regional Nottaway River Shear zone. Of interest, 8 potential pegmatite dykes are within a one-kilometre radius from the reported Ile Interdite showing.

There are 3 potential pegmatite dykes' occurrences which are characterized by their length and width as follows: In addition, there are 3 isolated potential pegmatite dykes: A dyke 780 metres long and 90 metres wide that is located 200 m west of Dyke Swarm #2, a second dyke 365 m long by 45 metres wide located 300 m west of the Dyke Swarm #3, and a third dyke 810 m long by 100 metres wide located 1,600 m southeast of Dyke Swarm #3. Results are as follows: The information on these dykes will be transferred to a GIS system and a series of maps at scale 1:5,000 will be generated. Preccise satellite image interpreted pegmatites will be correlated with existing data for generating targeted areas that will be followed up on the field in the upcoming pegmatite sampling program in the summer of 2024. The remote sensing work consists of establishing spectral signatures for direct identification of lithium-bearing minerals that have distinctive emission bands in the thermal spectrum.

Lithium-bearing minerals, such as spodumene, are difficult to identify visually and to distinguish from common rock forming silicate minerals on the field. The Company was using Worldview satellites constellation with panchromatic data up to 31 cm in resolution and multispectral data with 1.24 m resolution for this work. algorithms will be applied on these images in order to unfold pegmatites and/or swarms of pegmatites that can take the shape of flat-lying or variably dipping dykes, pods, tabular and lenticular-shaped bodies.

Number of dykes, From, Up to, Up to, Length, width, metres, metres, metres, metres., Dyke Swarm #1, 5, 160, 850, 70, 260, 1 300, 650, 650, Dyke Swarm #2, 3, 205, 215, 750, 700, 700, Dyke Swarm #3, 3, 350, 665, 100, 1 000, 600, Length, width, width, metres, metres. Dyke Area, length, width, metres, metres; Dyke #1, 780, 90, 200, Dyke #2, 365, 45, 300, 100, 100, 1 600, 1 600, Distance from nearest Dyke Swarm metres. Next steps to establish.

Next steps to establish.