Rock Identifier
Celsian (Barium aluminosilicate (BaAl2Si2O8))
mineral

Celsian

Barium aluminosilicate (BaAl2Si2O8)

A rare barium-rich feldspar that forms in manganese and barium-enriched metamorphic and hydrothermal deposits, the barium end-member of the feldspar family.

Mohs hardness
6-6.5
Color
Colorless, white, yellow, or pale gray
Type
mineral

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Overview

Celsian is a rare barium feldspar, the barium analogue of the more common potassium and sodium feldspars, with the composition BaAl2Si2O8. It is the barium end-member of a feldspar series that grades through hyalophane toward potassium feldspar.

Unusual among feldspars, celsian has aluminum and silicon in a 1:1 ratio (Al2Si2 rather than AlSi3), reflecting the substitution of barium for potassium. It crystallizes in the monoclinic system and is typically colorless, white, or pale yellow.

Because barium is concentrated only in special geological settings, celsian is uncommon and of primarily mineralogical and collector interest. It was named after the Swedish astronomer Anders Celsius.

Formation & geology

Celsian forms in barium- and manganese-rich metamorphic and hydrothermal environments. It is characteristically found in metamorphosed manganese deposits, where barium liberated during metamorphism combines with alumina and silica, and in some barium-bearing hydrothermal veins.

It commonly occurs alongside other barium minerals and manganese phases. Notable localities include manganese deposits in Sweden (such as Jakobsberg and Langban), Broken Hill in Australia, deposits in Japan and Scotland, and various metamorphosed manganese-barium ore bodies worldwide.

How to identify it

Celsian is colorless to white or pale yellow with a vitreous luster, hardness 6-6.5, white streak, and feldspar-like cleavage. It is notably denser than common feldspars because of its barium content, with a specific gravity around 3.1-3.4.

It is very difficult to distinguish from ordinary feldspar by eye; its higher density and its occurrence in barium-manganese deposits are the best practical clues, with chemical or X-ray analysis needed for confirmation. It grades into hyalophane as potassium replaces barium, so intermediate compositions are common.

Uses & significance

Celsian has no significant industrial or gem use and is too rare to be a commercial feldspar source. Its interest is essentially scientific and to mineral collectors, who prize well-characterized specimens from classic barium-manganese localities.

Synthetic celsian (and its hexagonal polymorph) is studied as a high-temperature ceramic material because of its thermal stability and low thermal expansion, finding niche use in advanced ceramics and as a component in some glass-ceramics. Natural celsian itself, however, is collected rather than mined.

Frequently asked questions

What is celsian?

Celsian is a rare barium feldspar, BaAl2Si2O8, the barium end-member of the feldspar family, found mainly in barium- and manganese-rich rocks.

How is celsian different from common feldspar?

It contains barium instead of potassium or sodium, has a 1:1 aluminum-to-silicon ratio, and is notably denser than ordinary feldspars.

Where is celsian found?

In metamorphosed manganese-barium deposits such as those in Sweden, Broken Hill in Australia, Japan, and Scotland.

Is celsian used in industry?

Natural celsian is too rare for industrial use, but synthetic celsian is studied as a heat-stable ceramic material.