Colemanite is a borate mineral represented as CaB3O4(OH)3·H2O. It is found in evaporite deposits of alkaline lacustrine environment. It is considered as one of the stable borate minerals. It develops electric charge when there is a change in temperature. It was discovered first in 1884 in Eastern California. It is brittle and belongs to sedimentary rock type. The diaphaneity of Colemanite is transparent to translucent.
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