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Berlinite (aluminium phosphate, chemical formula AlPO4 or Al(PO4)) is a rare high-temperature hydrothermal or metasomatic phosphate mineral. It has the same crystal structure as quartz with a low temperature polytype isostructural with α–quartz and a high temperature polytype isostructural with β–quartz. Berlinite can vary from colorless to greyish or pale pink and has translucent crystals.

Key facts

Mineral.name
Berlinite
Mineral.image
Berlinite.jpg
Mineral.imagesize
260px
Mineral.caption
Synthetic berlinite
Mineral.category
Phosphate mineral
Mineral.formula
AlPO4
Mineral.IMAsymbol
Ber
Mineral.strunz
8.AA.05
Mineral.system
Trigonal
Mineral.class
Trapezohedral (32) H-M symbol: (32)
Mineral.symmetry
P3121, P3221
Mineral.unit cell
a = 4.941 Å, c = 10.94 Å; Z = 3
Mineral.color
Colorless, pale gray, may be pale rose
Mineral.habit
Typically granular to massive
Mineral.twinning
Subparallel lamellae
Mineral.fracture
Conchoidal
Mineral.mohs
6.5
Mineral.luster
Vitreous

via Wikipedia infobox

Wikidata facts

Image
Blue Berlinite.jpg
Show 8 more facts
IMA Mineral Symbol
Ber
Strunz 8th edition (series ID, updated)
VII/A.01
Mohs' hardness
6.5
density
2.650
Commons category
Berlinite
chemical formula
AlPO₄
Nickel-Strunz 9th edition (updated 2009)
8.AA.05
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
8.AA.05
Sources (2)

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Article

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Contents
  • References
  • Further reading

Berlinite (aluminium phosphate, chemical formula AlPO4 or Al(PO4)) is a rare high-temperature hydrothermal or metasomatic phosphate mineral. It has the same crystal structure as quartz with a low temperature polytype isostructural with α–quartz and a high temperature polytype isostructural with β–quartz. Berlinite can vary from colorless to greyish or pale pink and has translucent crystals.

It was first described in 1868 for an occurrence in the Västanå iron mine, Scania, Sweden and named for Nils Johan Berlin (1812–1891) of Lund University.

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