400 Grams Emerald Specimen on Matrixn - Swat Valley, Pakistan Chlorine Peridot found here occurs in

Peridot found here occurs in its primary geological setting: directly within the ultramafic host rock rather than as a loose or secondary deposit

these tourmaline crystals are untreated

specifically selected for faceting and cutting purposes

Fake ambers will have well defined and full perfect shapes of inclusions such as full insect

When examined under light

400 Grams Emerald Specimen on Matrixn - Swat Valley, Pakistan Chlorine Peridot found here occurs inThis specimen has natural emerald crystal clusters growing directly on well defined faces sit on a pale beige calcite matrix with dark biotite patches and schist host matrix. The back of the specimen has the full matrix predominantly dark schist with scattered small green crystal points and a white calcite vein running through the base. A slightly lower angle has the depth of the crystal clusters and the contrast between the green crystals and the