Article · Wikipedia archive · Last revised Jul 10, 2026

Carletonite

Carletonite is a rare phyllosilicate mineral with formula KNa4Ca4(CO3)4Si8O18(F,OH)·(H2O). Its tetragonal crystals are a translucent blue, white, colorless or pink with a vitreous to dull lustre. It has a density of 2.45 and a hardness of 4–4.5.

Last revised
Jul 10, 2026
Read time
≈ 1 min
Length
231 w
Citations
9
Source
Carletonite
Carletonite, Poudrette quarry, Mont Saint-Hilaire, Montérégie, Quebec, Canada
General
CategoryPhyllosilicate minerals
FormulaKNa4Ca4(CO3)4Si8O18(F,OH)·(H2O)
IMA symbolCto1
Strunz classification9.EB.20
Crystal systemTetragonal
Crystal classDitetragonal dipyramidal (4/mmm)
H–M symbol: (4/m 2/m 2/m)
Space groupP4/mbm
Unit cella = 13.17 Å, c = 16.69 Å; Z = 4
Identification
ColourColourless, light blue, dark blue, or pink
Crystal habitPrismatic crystals, massive
CleavagePerfect on {001}, good on {110}
FractureConchoidal
TenacityBrittle
Mohs scale hardness4 - 4+12
LustreVitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.45
Optical propertiesUniaxial (-)
Refractive indexnω = 1.521 nε = 1.517
Birefringenceδ = 0.004
PleochroismWeak; O = pale blue; E = pale pinkish brown
References2345

Carletonite is a rare phyllosilicate mineral with formula KNa4Ca4(CO3)4Si8O18(F,OH)·(H2O). Its tetragonal crystals are a translucent blue, white, colorless or pink with a vitreous to dull lustre. It has a density of 2.45 and a hardness of 4–4.5.

It was discovered by G.Y Chao and named for the school he attended, Carleton University of Ottawa.6 It was first described in 1969 for an occurrence at Mont Saint-Hilaire, Quebec. The type locality at Mont Saint–Hilaire is the only reported occurrence.34

It occurs in hornfels and siliceous marble xenoliths within and adjacent to a nepheline syenite intrusion. It occurs in association with quartz, narsarsukite, calcite, fluorite, ancylite, molybdenite, leucosphenite, lorenzenite, galena, albite, pectolite, apophyllite, leifite, microcline and arfvedsonite.3

References

References