Garnet | |
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General | |
Category | Nesosilicate |
Formula | The general formula X3Y2(SiO4)3 |
IMA symbol | Grt[1] |
Crystal system | Isometric |
Crystal class | |
Space group | Ia3d |
Identification | |
Color | virtually all colors, blue is rare |
Crystal habit | Rhombic dodecahedron or cubic |
Cleavage | Indistinct |
Fracture | conchoidal to uneven |
Mohs scale hardness | 6.5–7.5 |
Luster | vitreous to resinous |
Streak | White |
Diaphaneity | Can form with any diaphaneity, translucent is common |
Specific gravity | 3.1–4.3 |
Polish luster | vitreous to subadamantine[2] |
Optical properties | Single refractive, often anomalous double refractive[2] |
Refractive index | 1.72–1.94 |
Birefringence | None |
Pleochroism | None |
Ultraviolet fluorescence | variable |
Other characteristics | variable magnetic attraction |
Major varieties | |
Pyrope | Mg3Al2Si3O12 |
Almandine | Fe3Al2Si3O12 |
Spessartine | Mn3Al2Si3O12 |
Andradite | Ca3Fe2Si3O12 |
Grossular | Ca3Al2Si3O12 |
Uvarovite | Ca3Cr2Si3O12 |
Garnets ( /ˈɡɑːrnɪt/) are a group of silicate minerals that have been used since the Bronze Age as gemstones and abrasives.
Garnet minerals, while sharing similar physical and crystallographic properties, exhibit a wide range of chemical compositions, defining distinct species. These species fall into two primary solid solution series: the pyralspite series (pyrope, almandine, spessartine), with the general formula [Mg,Fe,Mn]3Al2(SiO4)3; and the ugrandite series (uvarovite, grossular, andradite), with the general formula Ca3[Cr,Al,Fe]2(SiO4)3. Notable varieties of grossular include hessonite and tsavorite.
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