Anorthite

A variety of Minerals

Anorthite specimen - rock identification

What is Anorthite?

Anorthite is the calcium endmember of the plagioclase feldspar mineral series. The chemical formula of pure anorthite is CaAl2Si2O8. Anorthite is found in mafic igneous rocks. Anorthite is rare on the Earth but abundant on the Moon.

Optical Properties

Refractive Index
1.575-1.588
Birefringence
0.013
Optical Character
Biaxial negative

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Anorthite Localities Map

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North ZoneCentral RidgeSouth Basin

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Key Characteristics

Formation of Anorthite

Anorthite is a rare compositional variety of plagioclase. It occurs in mafic igneous rock. It also occurs in metamorphic rocks of granulite facies, in metamorphosed carbonate rocks, and corundum deposits. Its type localities are Monte Somma and Valle di Fassa, Italy. It was first described in 1823. It is more rare in surficial rocks than it normally would be due to its high weathering potential in the Goldich dissolution series. It also makes up much of the lunar highlands; the Genesis Rock is made of anorthosite, which is composed largely of anorthite. Anorthite was discovered in samples from comet Wild 2, and the mineral is an important constituent of Ca-Al-rich inclusions in rare varieties of chondritic meteorites.

More Images

Anorthite specimen 2
© Robert M. Lavinsky

Quick Facts

Physical Properties

Color
Colourless, reddish grey, white
Hardness (Mohs)
6 - 6.5
Density
2.76 g/cm³
Streak
White

Chemical Properties

Chemical Formula
Ca(Al2Si2O8)
Elements
Al, Ca, O, Si

Also Known As

AnorthiteAnorthoîteBasic PlagioclaseBeffoniteCalcic plagioclase
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