LI-FT POWER WKN: A3DQFE ISIN: CA53000A1066 Kürzel: WS0 Forum: Aktien User: oltimimo

Background on the Pontax Project The Pontax Lithium Project is located in the James Bay region of Quebec, approximately 300 km to the north of the town of Matagami, along the Billy Diamond Highway that provides access into the northern regions of Quebec. Matagami is a regional center with rail access. The Pontax Lithium Project is located along the Pontax River within the Anatacau-Pivert greenstone belt, a thin band of supracrustal rocks that occurs between the La Grande granitoid-gneiss terrane to the east and the Nemiscau sub-province to the west (Moukhsil et al., 2003). The Nemiscau sub-province is a large sedimentary basin which has undergone amphibolite to granulite facies metamorphism and is expressed in outcrop is diatexite and metatexites (rocks that have been subjected to high temperatures and have undergone some degree of partial melting and little to none of the primary textures remain). The Anatacau-Pivert greenstone belt is located to the east of the Nemiscau sub-province and is composed of lower amphibolite grade mafic to felsic volcanics, siltstone to wackes, iron formations, and local peridotite intrusions. Metamorphism is lower grade than the Nemiscau sedimentary rocks with primary textures being preserved and no onset of partial melting. The Pontax Formation is a conglomerate to wacke unit which sits unconformably on top of the Anatacau-Pivert supracrustal rocks. Clast composition is polymictic, ranging from granitic rocks to volcanic and sedimentary rocks. In some outcrops, quartz veins have been observed in the underlying volcanic rocks that terminate sharply against the Pontax Formation indicating the veining predated the deposition of the conglomerates. Polymictic conglomerates that unconformably overlie volcano-sedimentary rocks have been shown to mark major structural zones (e.g. the Timiskaming assemblage in the Abitibi greenstone belt). The east-west trend of the Pontax Formation suggests that there is an east-west trending structural zone that transects the Pontax Property; that trend is a prospective structural setting for hosting spodumene pegmatites.

February 27, 2025 – Vancouver, B.C., Li-FT Power Ltd. (“LIFT” or the “Company”) (TSXV: LIFT) (OTCQX: LIFFF) (Frankfurt: WS0) is pleased to provide an update on the exploration results from the Pontax Lithium Project (the “Project”), located in the James Bay region of Quebec, and also provide an update on the planned 2025 maiden drill program at the Project. The Pontax Lithium Project is comprised of claims that are 100% owned by LIFT as well as claims under an option agreement with Harfang Exploration Ltd. During the summers of 2023 and 2024 LIFT collected 336 till samples for indicator mineral analysis in areas with very little outcrop. The goal was to identify spodumene grains in the soil/till that would signal the presence of nearby spodumene pegmatites beneath the soil cover. The programs resulted in the definition of a 25 by 10 km area of high spodumene grain counts in glacial sediments. Francis MacDonald, CEO of LIFT, comments, “If spodumene is present in soils or glacial sediments, it is most likely sourced from lithium bearing spodumene pegmatites within close proximity. The areal extent of the Pontax spodumene anomaly is very impressive and suggests more than one pegmatite dyke is likely the cause of this. We believe there are at least three sizable targets, all within the same geological setting, all with high spodumene counts. The team is excited to get the drills started in April 2025 and are busily finalizing details for the program which is targeting the sources of this extensive spodumene anomaly.”

LIFT Prepares for Initial Diamond Drill Program at the 25 km Long Spodumene Anomaly at the Pontax Project, Quebec

https://www.li-ft.com/news/lift-prepares-for-initial-diamond-drill-program-at-the-25-km-long-spodumene-anomaly-at-the-pontax-project-quebec

Ich denke auch das Trump erstmal alle oder so viele wie möglich Quellen sichern möchte - und dann wird er plötzlich alles was mit Erneuerbaren Energie zu tun hat, es für gut befinden - denn wenn er das jetzt macht dann würden die Preise bereits enorm steigen - m.M.

🙈 Der Kampf um seltene Erden - siehe Ukraine Trump Deal ist im vollen Gange, vor allem der Fokus auf Lithium, nur an der Börse ist das scheinbar immer noch nicht angekommen ...

Scheinbar Nix 🤗

Was ist denn los aktuell

Jaa... für Explorer gerade schwierige Phase.... Fand Palantir bei 20 Euro zu teuer bzw zu hoch bewertet...und jetzt 🤣🤣🤣

Arger Sprung schon wieder

Hoffentlich lag der Boden bei etwa 1,80... jetzt kann es erstmal Richtung 2'30 - 2'50 gehen

📈😁 … aber warum ?

Was los heute?

Bin bei 1,50 Euro zurück.

The Moose 2 pegmatite has been mapped over a 450 m strike length and is up to 30 m wide. The pegmatite was bulk sampled, and test mined for its tantalum and niobium potential in the 1940’s and 1950’s, producing tantalum, niobium and lithium concentrates, but has never been evaluated or drilled for its lithium potential. Spodumene mineralization is common throughout the pegmatite, with elevated lithium analyses of up to 2.73% Li2O returned from samples along at least a 250 m strike length of the body. The Moose pegmatites are located within 1 km of Great Slave Lake, providing good year-round access to the property from both Yellowknife and Hay River on the south side of lake. Next steps for the property will include preparation for mapping, sampling and prospecting fieldwork ahead of initial drill testing of these mineralized spodumene pegmatites. LDG Lithium Project The LDG Project comprises 8,600 hectares of mineral claims and leases that are located 15 km southwest of Rio Tinto’s Diavik diamond mine. To date, 10 spodumene pegmatite occurrences have been discovered by prospecting which have outcropping dimensions of up to 20 m in width and 400 m in length. The project area is covered by till which can be used as an exploration medium to discover buried deposits. Mackay Lithium Project The MacKay Project is comprised of 8,600 hectares of mineral claims approximately 30 km to the south of the Rio Tinto’s Diavik diamond mine. To date, two spodumene occurrences have been discovered by prospecting. MK1 comprises a series of irregular sub-parallel pegmatite dykes ranging from 0.5 m to >10 m wide over a combined width of up to 150 m and traced over an interpreted strike extent of greater than 400 m; hand samples from four locations along a 120 m strike have returned 2.45%, 2.51%, 2.76% and 3.74% Li2O. MK3 (located ~ 4.5 km east northeast of MK1) is a prominent 15 to 20 m wide, white pegmatite exposure traced near continuously along strike for approximately 130 m; five representative grab samples returned 5.25%, 4.08%, 2.71%, 1.92% and 1.10% Li2O.

The DeStaffany mining claims are subject to a 2% gross overriding royalty of which one-half (1%) may be repurchased at anytime on payment of CAD $2,000,000 to the royalty holder. In addition, the LDG project is subject to a 2% gross overriding diamond royalty, and the lease forming a part of the LDG project is also subject to a 2% net smelter returns royalty. Both of those royalties contain buy-back provisions for one-half (1%) through payments to the royalty holder of CAD $2,000,000 and CAD $3,000,000 respectively. The transaction received the approval of the TSX Venture. DeStaffany Lithium Project The DeStaffany lithium property covers 1,843 ha located on the north central shore of Great Slave Lake, approximately 18 km northeast of the Nechalacho mine and 115 km east of Yellowknife. The property hosts the Moose 1 and Moose 2 lithium-tantalum-niobium bearing pegmatites. The pegmatites were initially evaluated in the 1940’s for tantalum and niobium but have never been subject to a focused evaluation of their lithium potential. New discoveries are possible within the property as highlighted by the identification of additional pegmatites by a predecessor company to North Arrow. At the time, these pegmatites were not described or evaluated for their lithium potential. The Moose 1 pegmatite has never been drilled but has been traced over a 370 m strike, averaging 4.5 m to 6.0 m in width with a maximum width of approximately 11 m, and hosts spodumene mineralization that returned 1.5% Li2O over 7.5 m from historic channel sampling in 2009. Additional historic surface samples have returned from background values to 4.1% Li2O.