RE:Phase XII - 7000 m drilledInteresting comment from Garth Drever :
“The exciting presence of the cesium mineral pollucite in the lithium zone intersected in DDH PL-057-22 suggests the Spark pegmatite is well evolved mineralogically, and may be approaching the degree of fractionation attained by the prolific Tanco pegmatite(1) at Bernic Lake, Manitoba where high-grade pollucite zones occur.” states Garth Drever, V.P. Exploration. “High fractionation could result in furthering the potential by-products beyond Lithium and Tantalum.