***Geology and geological interpretation.
The Gilbert Arc graphite deposit is located within Neoproterozoic Mozambique belt that extends throughout Eastern Africa. The host rocks consist of graphitic schists, quartzites and gneisses with minor bands of dolomite and felsic granulites. The high grade core of the deposit is dominated by graphitic schists.***
Schist is formed from compressed clay farmer the mines expert. When was the last time you saw an excavator dig a trench through solid concrete farmer. OMG. DYOR.
***Geology and geological interpretation. The Gilbert Arc...
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