Description
The quartz epidote axinite mineralisation was evidently caused by hydrothermal activity related to the doleritic sills which are in close proximity to the occurrence
cut and polished on one side
Dimensions at widest points approximately 130 mm x 85 mm x 80 mm thick
Dimensions of entire nodule at widest points approx
Dendritic Opal rough. DOR 193 #brecciated The quartz epidote axinite mineralisationDOR193. Dimensions at widest points approximately 150 mm x 85 mm x 60 mm thick. Weighs 1,035 grams. From our mining claims at Grant's Patch, 55km NW of Kalgoorlie, Western Australia.
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