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as crystals must be removed without damage from narrow clefts in hard rock
The fluorescence is caused by the presence of trace impurities within the mineral
Unlike precious opal
there were no inclusions present in the "fibrous" structures at all
and subtle translucence unique to each piece
Natural Clinochlore (Seraphinite) Specimen TF3264 deities as crystals must be removedNatural Clinochlore (Seraphinite) Specimen Approx. Dimensions: 2x1. 25x1 inches Approx. Weight: 56. 4 grams Locality: Korshunovskiy Mine, Zheleznogorsk City, Irkutskaya Oblast, Russia Clinochlore is a green colored mineral belonging to the chlorite group, a subset of phyllosilicates. It forms in metamorphic environments, particularly in regions with low grade metamorphism, such as shale and slate deposits. Historically, clinochlore has been recognized
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