The
sapphires of Myanmar occur in intimate association with rubies in virtually all
alluvial deposits throughout the Mogok area, but are found in quantity at only
a few localities, particularly 8 miles (13 km) west of Mogok, near Kathe. The
Myanmar Sapphires are formed in the igneous rocks that undergo contact and
regional metamorphosis. Normal and routine weathering causes the corundum down
from mountains to settle on the bottom of river beds and streams from where it
is recovered from the alluvial deposits. Not all Myanmar sapphires are deep in
color. The best display a rich, intense, slightly violetish blue, but some are
quite light. The key difference between Burma and sapphires from other
countries is saturation, with those from Myanmar possessing much more color in
the stone.
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