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

Discussion of exploration program and methodology LIFT initiated exploration on the Pontax Lithium Project during the summer of 2022. The initial exploration program consisted of a regional till geochemistry sampling program that covered all of LIFT’s Quebec properties (see press release dated November 15, 2022). During the spring of 2023, LIFT drill-tested two anomalies defined with till geochemistry on the Rupert Project (see press release dated March 29, 2023). Till geochemistry outlined spatially continuous anomalies in Li-Cs-Ta-Sn-Nb at Target A and Target B. Results from the drill program were disappointing; no spodumene pegmatites were intersected. LIFT’s technical team made the conclusion that till geochemistry was not an effective tool to define spodumene pegmatites under cover. During the summer of 2023, LIFT decided to trial mineral counting as a methodology to target spodumene in glacial sediments. Indicator mineral counts have been used for decades in diamond and gold exploration programs and have been fundamental tool for a number of discoveries in Canada (i.e. Ekati, Diavik, Gahcho Kue (diamonds), Rainy River, Meliadine, Casa Berardi (gold), Lac des Iles (PGE), and Voisey’s Bay (Ni sulphide)). The premise of this sampling technique is that unique minerals, and combinations of minerals, occur in mineral deposits. These minerals are transported along ice-flow during glaciation periods and get smeared across the landscape. Till samples (usually 5 – 50 kilograms of till) are collected and then processed in a way to isolate these indicator minerals, which are then counted. Areas with high “counts” typically indicate promising targets for further exploration. LIFT selected areas with high lithium value in till geochemistry (and associated pathfinder elements) as areas to collect sampling for spodumene grain counts within the Pontax and Rupert projects. Samples were collected both up-ice and down-ice of the Whabouchi lithium deposit (Rio Tinto – Investissement Quebec, 50/50 joint venture) on LIFT’s claims for orientation. The samples collected down-ice of Whabouchi returned hundreds of spodumene grains while the samples up-ice returned background values of less than 10 spodumene grains (see press release dated May 2, 2024). During the summer of 2024, LIFT collected an additional 336 till samples for spodumene counts, as well as conducted geologic mapping, prospecting, surficial mapping, and magnetics surveys.

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.