Announcement • Apr 10
Future Fuels Inc. announced that it has received CAD 1.999999 million in funding On April 8, 2026. Future Fuels Inc. announced that it has closed the transaction. Announcement • Feb 27
Future Fuels Inc. (TSXV:FTUR) entered into an agreement to acquire Hatchet Uranium Corp. from ValOre Metals Corp. (TSXV:VO). Future Fuels Inc. (TSXV:FTUR) entered into an agreement to acquire Hatchet Uranium Corp. from ValOre Metals Corp. (TSXV:VO) on February 26, 2026. Under the terms of the Amalgamation Agreement, HUC will amalgamate with Subco, and Future Fuels will acquire all of the outstanding securities of HUC on the following basis: (i) each common share of HUC will be exchanged for 0.760836 of a common share in the capital of Future Fuels and (ii) each common share purchase warrant of HUC will be exchanged for 0.760836 of a common share purchase warrant of Future Fuels. In total, it is expected that there will be 19.7 million HUC Shares and 1.4 million HUC Warrants issued and outstanding immediately prior to the completion of the Acquisition, and that approximately 15 million Consideration Shares and 1.1 million Consideration Warrants will be issued to the former securityholders of HUC upon completion of the Acquisition. HUC holds interests in five claim blocks, which are Hatchet Lake, CBX/Shoe, Usam, Genie and Highway.
Upon completion of the Acquisition, HUC will continue as a wholly-owned subsidiary of Future Fuels and is expected to change its name to “Future Fuels Athabasca Inc.”
The completion of the acquisition is subject to certain conditions, which are: (a) the Exchange shall have conditionally approved the Acquisition (b) the shareholders of HUC shall have approved the Acquisition and Amalgamation at a special meeting of the HUC
shareholders; (c) rights of dissent with respect to the amalgamation shall not have been exercised by HUC shareholders holding more than 10% of the outstanding HUC Shares; and (d) HUC shall have a working capital deficit of not more than $200,000 and no long-term debt as at the Closing Date. Announcement • Jan 16
Future Fuels Inc. Announces the Results of Its 2025 Ground Gravity Survey At Its 100%-Owned Hornby Basin Uranium Project Future Fuels Inc. announced the results of its 2025 ground gravity survey (the "Survey") at its 100%-owned Hornby Basin Uranium Project (the "Hornby Project" or the "Project"), located approximately 95 kilometres southwest of Kugluktuk, Nunavut. The Survey was completed by EarthEx Geophysical Solutions Inc. (EarthEx) and represents the most detailed gravity dataset ever acquired across the Hornby Basin uranium district. The program successfully delineated several high-priority gravity anomalies spatially associated with major structural corridors, stratigraphic boundaries, and known uranium mineralization, significantly advancing Future Fuels' understan Ding of subsurface density architecture across the Mountain Lake area. The 2025 program forms part of Future Fuels' broader district-scale exploration strategy at the Hornby Project, supporting the Company's objective of expanding on the historical Mountain Lake uranium system and identifying additional mineralized zones along the Helmut-Imperial structural corridor. Field operations were conducted between mid-September and early October. The Company more than doubled the size of the historical IsoEnergy gravity data set, and EarthEx merged the new data together with the datasets from 2022 and 2024. The field program deployed multiple Scintrex CG-5 gravimeters and a dual-frequency Emlid Reach RS2/RS2+ RTK GNSS system. The 2025 campaign included establishing and verifying control stations, drift testing all instruments through extended 24-hour warm-up cycles, and performing daily tie-ins to the Gravity Control Station (GCS) established during the 2024 program. Raw GNSS and gravity data were quality-controlled daily, uploaded from camp, and processed off-site using the Oasis Montaj Gravity and Terrain Correction Module. All newly acquired gravity data were corrected for instrument drift, levelled to the GCS, and merged with the 2022 and 2024 data. Elevation corrections were calculated using high-resolution ArcticDEM models reprojected for NAD83 (CSRS) UTM Zone 11N, and Complete Bouguer Anomaly ("CBA") values were generated at a density of 2.67 g/cm3. The merged dataset was gridded at 12.5-metre resolution, and tilt-derivative filtering was applied to enhance subtle density contrasts. The resulting product is a unified, district-scale gravity dataset that correlates strongly with mapped stratigraphy, topographic breaks, and major structural features across the Helmut -Imperial corridor. A pronounced northeast-southwest trending gravity fabric dominates the survey area, consistent with the regional structural grain of the Hornby Basin. EarthEx interprets the dataset across three principal structural domains. North of the Helmut Fault, the gravity field is relatively smooth and subdued, likely reflecting significant overburden thickness rather than bedrock density variations. No features in this northern domain are interpreted to be directly related to uranium mineralization. Between the Helmut and Imperial Faults, the survey reveals several discrete gravity highs and lows that correspond with mapped Unit 11 -Unit 12 contacts and subordinate faults. Within this central structural block, four priority anomalies (Grav_Anom_1 through Grav_Anom_4) were highlighted, two of which occur immediately adjacent to stratigraphic boundaries known to influence uranium emplacement. In the southwestern portion of this domain, two of the anomalies remain open beyond the 2025 survey limits, suggesting potential extension into areas requiring additional infill and edge closure work. The most significant results arise from the structurally complex zone south of the Imperial Fault, which hosts the historical Mountain Lake uranium system. Here, the CBA data show a pronounced, localized gravity high (Grav_Anom™?) that spatially coincides with the known systems footprint. This response is particularly notable because the system occurs at surface within low-density Unit 12 sediments and areas of presumed thick overburden. The persistence of a strong, positive gravity anomaly in the region of the large, positive gravity anomaly in the area. 
