|
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 (CaB
3O
4(OH)
3·H
2O) 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.