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From our mining claims near Ora Banda in the Eastern Goldfields region of Western Australia
The quartz epidote axinite mineralisation was evidently caused by hydrothermal activity related to the doleritic sills which are in close proximity to the occurrence
Fossil stromatolite polished slab
Dimensions at widest points approximately 150 mm x 110 mm x 11 mm thick
From our mining lease on Turee Creek station
Epidote, Quartz & Axinite EPI58 lace agate From our mining claims nearEPI58 Epidote, Quartz & Axinite slab, cut and polished on one side. Epidote is the green mineral, Axinite is grey. Quartz is white. Dimensions 185 mm x 65 mm x 14 mm thick. Weighs 434 grams This stone occurs in the Pilbara region of Western Australia. It occurs as a single vein, no thicker than 250mm that cross cuts the Weeli Wolli formation, a banded iron formation, (commonly jaspilitic) which is also intruded by metadoleritic sills. The quartz
US$ 337.94
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