Announcement • Jun 16
Canamera Energy Metals Corp Reports Assay Results From Southern Zone At Turvolândia Ionic Clay Rare Earth Project Canamera Energy Metals Corp. announced assay results from its Southern Zone, highlighting auger drill hole TUV-AUG-0036 at its Turvolândia Ionic Clay Rare Earth Project in Minas Gerais, Brazil. TUV-AUG-0036 returned rare earth mineralisation concentrated in the deepest 6 metres of the hole, with grades increasing toward the bottom and the hole terminating in mineralised material, remaining open at depth. Of the holes for which results have been received at the Southern Zone, TUV-AUG-0036 is the most promising result to date, returning rare earth enrichment concentrated below 16 metres depth and continuing through end of hole. Two additional holes - TUV-AUG-0033 (6 metres total depth) and TUV-AUG-0034 (7 metres total depth) - terminated in peak mineralisation, with the last metre of TUV-AUG-0033 returning 575 ppm MREO + Y2O3 and the last two metres of TUV-AUG-0034 returning 355 ppm MREO + Y2O3, indicating that magenetic REO mineralisation is present across multiple drill locations at the South Target. Hole TUV-AUG-0036 was drilled vertically to a total depth of 22.0 metres. Rare earth enrichment is concentrated below 16 metres depth, where grades increase substantially relative to the upper profile and continue to improve toward the base of the hole. The final 2-metre interval (19-21 m) represents the highest-grade zone drilled at the South Target to date, averaging 1,293.3 ppm MREO + Y2O3 and 2,793.8 ppm TREO. The hole terminated in mineralised material; the base of the weathered profile was not reached. All 22 samples returned Chemical Index of Alteration values above 93.8%, consistent with advanced weathering profiles characteristic of ionic adsorption clay-hosted REE deposits. The South Target demonstrates a strong radiometric signature, with total-count radiometric responses comparable to those observed at the Cordis, Linda, and Marita targets. Assay results for TUV-AUG-0036 are presented in Table 1. Analytical results from TUV-AUG-0036 identified gallium concentrations throughout the hole. Gallium values for 20 of the 22 one-metre intervals ranged from 17.4 to 44.3 ppm. The two remaining intervals (19-20 m and 20-21 m) returned an 'I.N.F.' result in the source data; the basis for this flag and its appropriate treatment in calculating a full-hole average are subject to final confirmation by the Company's QP. The full-hole average is stated as 29 ppm over 22 metres, pending that confirmation. Gallium is recognised as a critical mineral by Canada, the United States, and the European Union. The distribution of gallium is present throughout the full vertical profile, in contrast to the REE enrichment which is concentrated below 16 metres. The Company's primary exploration focus remains ionic adsorption clay-hosted rare earth mineralisation. The economic significance of the gallium values identified to date is unknown. No metallurgical studies have been completed to evaluate gallium recovery. The Company anticipates reporting assay results from the four additional holes drilled at the South Target upon receipt and validation. The Company is also evaluating follow-up exploration programmes to further define the South Target, including potential deeper drilling to evaluate mineralisation below the 22-metre depth of TUV-AUG-0036. There can be no assurance that future exploration programmes will define economically recoverable mineral resources. Auger drill samples were collected at one-metre intervals and submitted to SGS Geosol Laboratórios Ltda., Vespasiano, Minas Gerais, Brazil (ISO/IEC 17025 accredited), an independent laboratory, for multi-element analysis by ICP-OES/MS including all rare earth elements. The QA/QC programme included the regular insertion of certified reference materials, blank standards, and field duplicates. Elemental values were converted to rare earth oxide equivalents using standard conversion factors. The adjustments to the data were made as needed, converting the rare earth element values to the industry-standard rare earth format. Announcement • Apr 10
Canamera Energy Metals Corp Identifies High-Priority Rare Earth Element Target At Garrow Project as Airborne Survey Reveals Broad Magnetic Anomaly Aligned with Elevated Rare Earth Lake Sediment Values Canamera Energy Metals Corp. has announced the completion of a 463.7 line-kilometre airborne magnetic survey over its Garrow rare earth element project located in eastern Ontario, approximately 16 kilometres west of Timiskaming. The survey has identified a broad magnetic anomaly on the western portion of the Property that is spatially coincident with elevated total rare earth element values reported in regional lake sediment sampling conducted by the Ontario Geological Survey. The Garrow Project is an REE and niobium exploration property situated within the Grenville Province, a geological terrane known to host alkaline and carbonatite-related mineralization across eastern Ontario. The airborne survey represents the first modern geophysical dataset acquired over the Property and provides the Company with a foundational tool for targeting ground-level exploration programs. The airborne magnetic survey was conducted by Rosor Explorations and comprised 463.7 line-kilometres of data acquisition flown at 100-metre line spacing and an average flight height of 50 metres. The magnetic data obtained displays a strong correlation between magnetic response and the metamorphic and plutonic rock units underlying the Property, providing a clear representation of the general structural fabric and lithological trends. Of particular significance is a broad magnetic high located on the western half of the Property and trending to the southeast. This magnetic high is interpreted to represent the extent of a gneissic granite mapped as Intermediate to Felsic Intrusive Rocks of the McDougal and Associated Plutons (circa 1250 Ma), as documented in published geological mapping by the Ontario Geological Survey. Lake sediment geochemistry is a widely used regional-scale exploration tool in which the chemical composition of lake-bottom sediments serves as an indicator of the mineralogy of surrounding and upstream bedrock. In REE-prospective terranes, elevated rare earth concentrations in lake sediments can reflect the weathering and transport of REE-bearing minerals from proximal bedrock sources. Coincident with the magnetic high is a series of lake sediment samples collected by the OGS in 2001 that yielded elevated total rare earth element values. The convergence of two independent datasets - a geophysical anomaly defining a distinct lithological unit and a geochemical signature indicating elevated rare earth concentrations - strengthens the interpretation that the western portion of the Property warrants priority follow-up investigation. The Company will integrate the airborne magnetic data and its structural interpretations with the regional lake sediment geochemical dataset to delineate priority target areas for ground follow-up. Planned activities include geological mapping, prospecting, and soil geochemistry designed to further define the distribution of rare earth element mineralization and identify host lithologies on the Property. Announcement • Mar 27
Canamera Energy Metals Corp. announced that it has received CAD 4.613947 million in funding On March 26, 2026, Canamera Energy Metals Corp. closed the transaction. In connection with the LIFE Offering, the Company paid CAD 50,688.00 in cash finder's fees and issued 92,160 finder's warrants. In connection with the Concurrent Offering, the Company paid CAD 60,000.14 in cash finder's fees and issued 90,909 finder's warrants 
