Glaucochroite

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Glaucochroite
Glaucochroite-270038.jpg
Glaucochroite found in New Jersey
General
Category Silicate mineral
Formula
(repeating unit)
CaMnSiO4
Strunz classification 9.AC.05
Dana classification51.3.2.3
Crystal system Orthorhombic
Identification
ColorBluish-gray, pink, brown, or white
Fracture Conchoidal, Sub-Conchoidal
Mohs scale hardness6
Luster ResinVitreous, Sub-Vitreous, Resinousous
Streak white
Optical propertiesBiaxial (-)
References [1]

Glaucochroite is a calcium manganese nesosilicate mineral with formula CaMnSiO4. It occurs in metamorphosed limestones.

It was first described in 1899 in Franklin Furnace, Sussex County, New Jersey.

Related Research Articles

Kombat is a mine and its associated settlement at the southern margin of the Otavi Mountain Range in northern Namibia. It is situated 37 kilometres (23 mi) East of Otavi on the B8 to Grootfontein. Kombat at its peak had over 1,000 inhabitants. As of 2015 it is almost abandoned, although Kombat Primary School still operates at reduced capacity, and a clinic is serving the remaining inhabitants.

<span class="mw-page-title-main">Bustamite</span>

Bustamite is a calcium manganese inosilicate (chain silicate) and a member of the wollastonite group. Magnesium, zinc and iron are common impurities substituting for manganese. Bustamite is the high-temperature polymorph of CaMnSi2O6 and johannsenite is the low temperature polymorph. The inversion takes place at 830 °C (1,530 °F), but may be very slow.
Bustamite could be confused with light-colored rhodonite or pyroxmangite, but both these minerals are biaxial (+) whereas bustamite is biaxial (-).

References