Eudialyte

Eudialyte, whose name derives from the Greek phrase Εὖ διάλυτος, eu dialytos, meaning "well decomposable", is a somewhat rare, nine-member-ring cyclosilicate mineral, which forms in alkaline igneous rocks, such as nepheline syenites. Its name alludes to its ready solubility in acid.

Eudialyte
General
CategoryCyclosilicate
Formula
(repeating unit)
Na15Ca6(Fe,Mn)3Zr3SiO(O,OH,H2O)3
(Si3O9)2(Si9O27)2(OH,Cl)2
IMA symbolEud
Strunz classification9.CO.10
Crystal systemTrigonal
Crystal classHexagonal scalenohedral (3m)
H-M symbol: (3 2/m)
Space groupR3m
Unit cella = 14.31, c = 30.15 [Å]; Z = 12
Identification
ColorRed, magenta, brown; also blue and yellow
Crystal habitCrystals short rhombohedral to long prismatic, granular, irregular masses
CleavageDistinct on {0001} imperfect on {1120}
FractureUneven
TenacityBrittle
Mohs scale hardness5–6
LusterVitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.74–3.10
Optical propertiesUniaxial (+/−)
Refractive indexnω = 1.606–1.610 nε = 1.610–1.613
Birefringenceδ = 0.004
PleochroismWeak: O= colorless, pale yellow, pink; E= pink to colorless
SolubilityH2SO4
Other characteristicsMildly Radioactive
References

Eudialyte was first described in 1819 for an occurrence in nepheline syenite of the Ilimaussaq intrusive complex of southwest Greenland.

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