Polished Magnesite slab. MAP181 mookaite The quartz epidote axinite mineralisation

The quartz epidote axinite mineralisation was evidently caused by hydrothermal activity related to the doleritic sills which are in close proximity to the occurrence

The subtle lime green colouration is caused by the presence of nickel mineralisation

Weighs 435 grams

155 mm x 70 mm x 30 mm thick

RH250  A slab

Polished Magnesite slab. MAP181 mookaite The quartz epidote axinite mineralisationMAP181. Magnesite (Lemon chrysoprase) slab polished on one side. A mix of magnesite and chrysoprase ! The subtle lime green colouration is caused by the presence of nickel mineralisation. Dimensions at widest points approximately 80 mm x 40 mm x 9. 5 mm thick. Weighs 56 grams. From north of Kalgoorlie, Western Australia.