the pegmatites are seemingly directly under low Li soil samples (the higher soil samples were further south), and they thicken up to the north where it’s open for 3km or so with little to no Li in the soil due to alluvial coverage. There was only a few select drill holes in that area to confirm the theory which proved right, so I’m quite interested in what management do next after assay results are received to enhance understanding of the area under coverage.
Due to the location of the 3km stretch (Goldilocks zone, alone strike from Manna), I think we could have some exciting exploration ahead. Dyor these are just my thoughts.
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