Beyond Lithium Inc. announced the results of a comprehensive exploration program at its Ear Falls spodumene project which confirm the potential of this recent discovery. The work recently completed at Ear Falls consisted of: A stripping program designed to expose the extension of the spodumene pegmatites in all-directions and to potentially uncover more subparallel dykes; A drilling program targeted to further understand and delineate the characteristics and the densities of these subparallel spodumene pegmatite dykes; and An exploration and sampling program along the identified 13 km lithium exploration corridor. Grab samples from the area where the initial discovery was made (named the Wenasaga North Zone) assayed up to 4.54% lithium oxide ("Li2O").

Given the promising results announced at the time, team went back to the property and made significant additional discoveries. The company's field crew continued exploration was based on the geological data collected from the early field work. The stripping and channel sampling program was designed to further understand the grade distribution and continuity in the pegmatites and the host rocks for designing the follow-up exploration program to explore for additional and subparallel spodUMene-bearing pegmatites.

The channel sampling program consisted of a total of 64 channel samples from 15 channel locations ranging from 0.67m to 10.77m. The channel samples were collected from three different zones, EF-1, EF-2 and EF-3, along the Wenasaga North Zone. The stripping and channel sampling program was designed to further understand the grade distribution and continuity in the pegmatites and the host rocks for designing the follow-up exploration program to explore for additional and subparallel spodumene-bearing pegmatites.

The channel samples collected along the initial one-kilometer spodumene-bearing pegmatite trend known as the Wenasaga North Zone were divided into three zones: EF-1, EF-2 and EF-3. Zone EF-1 primarily tested the initial 150m strike length of the spodumene-bearing pegmatites zone. Channel sampling at zones EF-2 and EF-3 were step-outs samples testing the extent of the one- kilometer long spodumene zone. Since the spodumene discovery announced in September, Beyond Lithium field crew continued to explore for additional spodumene-bearing pegmatites following the strike orientation of the Ear Falls spodumene-bearing pegmatite system.

They were able to locate additional spodumene-bearing pegmatites towards the northeastern extension grading up to 1.00% Li2O and 107ppm Cs in grab sample mineralized with spodumene, muscovite, and fluorapatite. With the recognition of additional spodumene-bearing pegmatites towards the northeast direction, the Wenasaga North Zone at Ear Falls has now been extended by over 50%, from 1.0 km to 1.5 km at the northeast region of the 13 km exploration corridor. A pegmatite in the northern part of the EF-1 zone was mechanically stripped by a backhoe for a more continuous channel sampling across the spodumene-bearing pegmatite, EF-C-03.

This channel graded 0.54% Li2O and 186ppm Cs over 9.52m including 0.83% Li2O and 168ppm Cs over 2.47m and 0.85% Li2O and 157ppm Cs over 2.45m. The spodumene-bearing pegmatite is formed along the contact between the granite and the metasediments with local sliver of older micaceous granite. Generally, the pegmatites strike at 030 to 070 degrees azimuth and dip moderately at 60 to 70 degrees towards the northwest.

Based on field observation, the spodumene-bearing pegmatites at Ear Falls are strongly controlled by the orientation of the granite and the metasediments contact.