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Dominant species
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Boracite
Boracite
Chemical
Formula
Mg3B7O13Cl
Species
Borates
Crystal
System
Orthorhombic
Mohs
Scale
7
Specific
Gravity
2.95
Color
Blue green, colorless, gray, yellow, orange, brown, white, blue, pale green, dark green; colorless in transmitted light
Streak
White
Luster
Adamantine, Vitreous
Refractive
Index
n = 1.658 - 1.662 n = 1.662 - 1.667 n = 1.668 - 1.673
Diaphaneity
Transparent, Translucent
Cleavage
None Observed
Fracture
Irregular/Uneven, Conchoidal
Crystal Habit:Crystalline, disseminated
Geological Setting:Bedded sedimentary deposits of gypsum and anhydrite; salt deposits; potash deposits of the oceanic type.
Boracite is a magnesium borate mineral with formula: Mg3B7O13Cl. It occurs as blue green, colorless, gray, yellow to white crystals in the orthorhombic - pyramidal crystal system. Boracite also shows pseudo-isometric cubical and octahedral forms. These are thought to be the result of transition from an unstable high temperature isometric form on cooling. Penetration twins are not unusual. It occurs as well formed crystals and dispersed grains often embedded within gypsum and anhydrite crystals. It has a Mohs hardness of 7 to 7.5 and a specific gravity of 2.9. Refractive index values are nα = 1.658 - 1.662, nβ = 1.662 - 1.667 and nγ = 1.668 - 1.673. It has a conchoidal fracture and does not show cleavage. It is soluble in water.

Boracite is typically found in evaporite sequences associated with gypsum, anhydrite, halite, sylvite, carnallite, kainite and hilgardite. It was first described in 1789 for specimens from its type locality of Kalkberg hill, Lüneburg, Lower Saxony, Germany. The name is obviously derived from its boron content (19 to 20% boron by mass).