Article · Wikipedia archive · Last revised Jun 25, 2026

Greifensteinite

Greifensteinite is beryllium phosphate mineral with formula: Ca2Fe2+5Be4(PO4)6(OH)4·6H2O. It is the Fe2+ dominant member of the roscherite group. It crystallizes in the monoclinic crystal system and typically forms prismatic dark olive green crystals.

Last revised
Jun 25, 2026
Read time
≈ 1 min
Length
186 w
Citations
8
Source
Greifensteinite
Greifensteinite (picture size: 3 mm)
General
CategoryPhosphate mineral
Roscherite group
FormulaCa2Fe2+5Be4(PO4)6(OH)4·6H2O
IMA symbolGfs1
Strunz classification8.DA.10
Dana classification42.7.7.4
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/c
Unit cella = 15.903, b = 11.885
c = 6.677 [Å]; β = 94.68°; Z = 2
Identification
ColorYellow green, olive green, light brown
Crystal habitPrismatic
CleavageGood on {100} (or parting on {100})2
FractureUneven
Tenacitybrittle
Mohs scale hardness4.5
LusterVitreous
StreakWhite, greenish
DiaphaneityTransparent to translucent
Specific gravity2.93
Optical propertiesBiaxial (-)
Refractive indexnα: 1.624
nβ: 1.634
nγ: 1.638
Birefringence0.014
2V angle80°
References234

Greifensteinite is beryllium phosphate mineral with formula: Ca2Fe2+5Be4(PO4)6(OH)4·6H2O. It is the Fe2+ dominant member of the roscherite group.5 It crystallizes in the monoclinic crystal system and typically forms prismatic dark olive green crystals.2

It was first described in Germany at Greifenstein Rocks, Ehrenfriedersdorf, and was named for the location. At the type locality, it occurs within a lithium-rich pegmatite in miarolitic cavities. It was approved by the International Mineralogical Association in 2002.2

References

References

  • Rastsvetaeva R K, Gurbanova O A, Chukanov N V (2006) Crystal structure of greifensteinite Ca2Fe2+☐Mg2Fe2+2Be4(PO4)6(OH)4·6H2O. Doklady Chemistry 41, 18-25 [1] Archived 2013-04-02 at the Wayback Machine