Chambersite

Chambersite is a borate that is rare and is the manganese analogue of Boracite. It is an mineral that is extremely unusual faceted gems are nearly non-existent. The tetrahedral shaped crystals are so(up that is small 10mm on the side) that Chambersite gems are usually not ‘cut’ nevertheless the surfaces of the natural crystal shape are just polished. Many crystals are too small and/or too dark to be faceted. Chambersite ended up being discovered in 1962 in a salt brine storage well at Barbers Hill Salt Dome (Barbers Hill), Mont Belvieu, Chambers County, Texas, USA. The way that only finds the tiny crystals is by diving to depths of up to 70 feet in the salt brine.

Distribution: In the USA, from the Barber’s Hill salt dome, Mont Belvieu, Chambers County, Texas (Type Locality) and the Venice salt dome, Plaquemines Parish, Louisiana. In the Jixian Mn–B deposits, Hebei Province, China. From Pomyarka, near Truskarets, Carpathian Mountains, Ukraine.

Category: Tektoborates
Chemical Formula: Mn3B7O13Cl
Manganese Borate Chloride
Molecular Weight: 483.93 gm
Composition: Manganese 34.06 % Mn 43.98 % MnO
Boron 15.64 % B 50.35 % B2O3
Chlorine 7.33 % Cl 7.33 % Cl
 –  % Cl -1.65 % -O=Cl2
Oxygen 42.98 % O
  100.00 % 100.00 % = TOTAL OXIDE

 

Crystallography: Orthorhombic – Pyramidal
Crystal Habit: Crystals are pseudotetrahedral {111}, modified by {001}, {110}, and {111}, to 2 cm, paramorphous and composed of microscopically twinned aggregates of orthorhombic material inverted from the high-temperature form.
Twinning: Rare as interpenetrant twins on [111] with twin plane {111} (pseudocubic).

 

Cleavage: None
Fracture: Subconchoidal to Irregular/Uneven
Tenacity: Brittle
Moh’s Hardness: 7.0
Density: 3.49 (g/cm3)
Luminescence: None
Radioactivity: Not Radioactive

 

Color: Colorless, Lilac to dark Purple, Brownish Purple (may darken with exposure to sunlight)
Transparency: Transparent to Opaque
Luster: Vitreous (glassy)
Refractive Index: 1.732 – 1.744  Biaxial ( + )
Birefringence: 0.0120
Dispersion: r > v
Pleochroism: None