Lithium Hill
- Historical drilling ended hole in >28.5m wide pegmatite with K/Rb ratios as low as 54 and elevated Li2O (585 ppm), Cs-Ta-Nb.
- Remaining holes also intersected significant pegmatite widths over ~8km of strike, open in all directions.
- Access to historic core, high resolution magnetics and EM data
- Decreasing K/Rb Ratios down hole suggests increasing magmatic evolution
- End of Hole (209.1m) has the most evolved K/Rb ratio, with elevated Li-Ca-Ta-Nb signature
- Geochemistry and texture indicative of zoned LCT pegmatite at least 28.5m thick
- Similar stratigraphy to Greenbushes
- Hole intersected top of and terminated in pegmatite – pegmatite thickness unknown
WARNING: WE ARE NOT SUGGESTING LITHIUM HILL IS A GREENBUSHES ANALOG
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