Polished Rainforest Jasper slab RFJ138 Irregully formation The quartz epidote axinite mineralisation
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
Dimensions at widest points approximately 85 mm x 50 mm x 35 mm thick
60 mm x 40 mm x 35 mm
Approximate dimensions at widest points 125 mm x 60 mm x 40 mm thick
DO184 Dendritic Opal slab polished on one side
Polished Rainforest Jasper slab RFJ138 Irregully formation The quartz epidote axinite mineralisationRFJ138. Rain Forest Jasper (Spherulitic rhyolite) slab, polished on one side. Dimensions at widest points approximately 95 mm x 75 mm x 9 mm thick Weighs 104 grams. From Mt. Hay, Queensland.
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