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Dominant species
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Colemanite
Colemanite
Chemical
Formula
CaB3O4(OH)3·H2O
Species
Borates
Crystal
System
Monoclinic
Mohs
Scale
4
Specific
Gravity
2.42
Color
Colorless, white, yellowish, grey
Streak
White
Luster
Adamantine, Vitreous
Refractive
Index
n = 1.586 n = 1.592 n = 1.614
Diaphaneity
Transparent, Translucent
Cleavage
PerfectOn perfect; on distinct.
Fracture
Irregular/Uneven, Sub-Conchoidal
Crystal Habit:Massive granular to coarsely crystalline, most commonly nodular.
Geological Setting:Borate deposits formed in arid alkalai lacustrine environments.
Colemanite (CaB3O4(OH)3·H2O) is a borate mineral found in evaporite deposits of alkaline lacustrine environments. Colemanite is a secondary mineral that forms by alteration of borax and ulexite.

It was first described in 1884 for an occurrence near Furnace Creek in Death Valley and was named after William Tell Coleman (1824–1893), owner of the mine Harmony Borax Works where it was first found. At the time, Coleman had alternatively proposed the name "smithite" instead after his business associate Francis Marion Smith.