Outcropping and sub-outcropping pegmatite sills. 6 larger clusters of shallow artisanal workings. The main pegmatite has a discontinuous quartz core bordered by irregular cleavelandite zones with tantalite, lepidolite and zinnwaldite float. The pegmatite host is likely to be amphibolite.
License area: 312 ha
No. Licenses: 8
Li3 Ownership: 100%
- Lath of white spodumene in a fragment of pegmatite