Almandine

Almandine
General
CategoryNesosilicate
FormulaFe2+
3
Al
2
Si
3
O
12
IMA symbolAlm
Strunz classification9.AD.25
Crystal systemCubic
Crystal classHexoctahedral (m3m)
H–M symbol: (4/m 3 2/m)
Space groupIa3d
Identification
Colorreddish orange to red, slightly purplish red to reddish purple and usually dark in tone
Cleavagenone
Fractureconchoidal
Mohs scale hardness7.0–7.5
Lustergreasy to vitreous
Streakwhite
Specific gravity4.05+0.25
−0.12
Polish lustervitreous to subadamantine
Optical propertiesSingle refractive, and often anomalous double refractive
Refractive index1.790±0.030
Birefringencenone
Pleochroismnone
Dispersion0.024
Ultraviolet fluorescenceinert
Absorption spectrausually at 504, 520, and 573 nm, may also have faint lines at 423, 460, 610 and 680–690 nm
References

Almandine (/ˈælməndɪn/), also known as almandite, is a mineral belonging to the garnet group. The name is a corruption of alabandicus, which is the name applied by Pliny the Elder to a stone found or worked at Alabanda, a town in Caria in Asia Minor. Almandine is an iron aluminum garnet, of deep red color, inclining to purple. It is frequently cut with a convex face, or en cabochon, and is then known as carbuncle. Viewed through the spectroscope in a strong light, it generally shows three characteristic absorption bands.

Almandine is one end-member of a mineral solid solution series, with the other end member being the garnet pyrope. The almandine crystal formula is: Fe3Al2(SiO4)3. Magnesium substitutes for the iron with increasingly pyrope-rich composition.

Almandine, Fe2+
3
Al
2
Si
3
O
12
, is the ferrous iron end member of the class of garnet minerals representing an important group of rock-forming silicates, which are the main constituents of the Earth's crust, upper mantle and transition zone. Almandine crystallizes in the cubic space group Ia3d, with unit-cell parameter a  11.512 Å at 100 K.

Almandine is antiferromagnetic with the Néel temperature of 7.5 K. It contains two equivalent magnetic sublattices.