Maw-sit-sit
was discovered in Tawmaw, Myitkyina-Mogaung District, Kachin State, Myanmar
(Burma) in the
early 1960's near the historic imperial Jadeite mines
of northern Myanmar. It is a rock not a mineral. This
means it is composed of several minerals each containing
their own mixture of chemicals. It is a chromium-rich
metamorphic rock with a vivid green base color mixed
with black spots, bands, blotches and swirls. The dominant
mineral is Kosmochlor,
a sodium chromium pyroxene, that constitutes about 60%
of the Maw-sit-sit mixture. The next ingredient, about
15%, is chromium-enriched Jadeite
followed by chromium Ekermannite,
about 4%, and chromium Albite
at about 1%. The common element in each mineral is
chromium which is the strongest influence on the vivid,
emerald green color of Maw-sit-sit. It can also
contain other mineral impurities or inclusions such
as pure chromite, that can be seen as shiny "chrome"
looking flecks, and white Natrolite streaks
and bands. Maw-sit-sit is always opaque and makes
beautiful cabochons, beads and carvings.
The
only source of Maw-sit-sit is still the place where
it was discovered, Tawmaw, Myitkyina-Mogaung District, Kachin State, Myanmar
(Burma).
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