Boracite is a
magnesium borate chloride 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).
References