Chloritoid is a mineral named for its resemblance to minerals of the chlorite group. It can be distinguished from similar minerals by higher hardness, brittleness and optical parameters. It was first discovered in the Urals.
You can see chloritoid stone for sale and buy it in the Minerals of Russia online store.
General | |
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Category | Nesosilicates |
Formula (repeating unit) |
(Fe,Mg,Mn)2Al4Si2O10(OH)4 |
IMA symbol | Cld |
Strunz classification | 9.AF.85 |
Dana classification | 52.03.03.01 |
Crystal system | 1A polytype: triclinic 2M polytype: monoclinic |
Crystal class | 1A polytype: pinacoidal (1) 2M polytype: prismatic (2/m) |
Unit cell | 1A polytype: a = 9.46 Å, b = 5.50 Å, c = 9.15 Å; α = 97.05°, β = 101.56°, γ = 90.10° 2M polytype: a = 9.50 Å, b = 5.50 Å, c = 18.22 Å; β = 101.9°; Z = 4 |
Identification | |
Color | Dark gray, greenish gray, greenish black |
Crystal habit | Tabular pseudohexagonal crystals; rosettes, commonly coarsely foliated with foliae typically curved or bent; also massive |
Twinning | Common on {001}, polysynthetic may be lamellar |
Cleavage | Perfect on {001}, distinct on {110}; parting on {010} |
Tenacity | Brittle |
Mohs scale hardness | 6.5 |
Luster | pearly on cleavage surfaces |
Streak | White, grayish, or very slightly greenish |
Diaphaneity | Translucent |
Specific gravity | 3.46 – 3.80 |
Optical properties | Biaxial (+) or (–) |
Refractive index | nα = 1.713 - 1.730 nβ = 1.719 - 1.734 nγ = 1.723 - 1.740 |
Birefringence | δ = 0.010 |
Pleochroism | X = olive-green to yellow; Y = grayish blue to blue; Z = colorless to pale greenish yellow |
2V angle | Measured: 36° to 89° |
Dispersion | r > v; strong |