Colemanite
Colemanite (Ca
2B
6O
11·5H
2O) is a
borate mineral found in evaporite deposits. Colemanite is a secondary mineral that forms when
borax is deposited, and then regularly covered with
boron containing water. The
boron remains after the water evaporates, and the
boron and
borax eventually form other minerals as for example Colemanite.
It was named after
William T. Coleman (
1824-
1893), owner of the mine where it was first found.
Group: Borates, Hardness: 4.5, Specific gravity: 2.42, cleavage: perfect, Fracture: uneven-conchoidal,mineral may be white, yellow, or gray. Streak: white. Transparent-translucent, luster: vitreous. Forms in evaporative deposites. Soluble in hydrochloric acid. Fuses easily, breaks up, and colors a flame green. It is monoclinic. Crystals are short and prismatic.