
mineral
Almandine Garnet
Iron aluminum silicate (Fe3Al2(SiO4)3)
Hardness: 7-7.5 (Mohs scale); Color: Deep red to reddish-brown/purple; Luster: Vitreous to resinous; Crystal structure: Isometric (dodecahedral); Cleavage: Indistinct; Specific gravity: 3.93 - 4.30
- Hardness
- 7-7
- Color
- Deep red to reddish-brown/purple
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 7-7.5 (Mohs scale); Color: Deep red to reddish-brown/purple; Luster: Vitreous to resinous; Crystal structure: Isometric (dodecahedral); Cleavage: Indistinct; Specific gravity: 3.93 - 4.30
Formation & geological history
Formed primarily in metamorphic rocks like mica schists and gneisses through the regional metamorphism of clay-rich sediments. It can also occur in some igneous rocks like granites.
Uses & applications
Predominantly used as a gemstone in jewelry (cabochons and faceted stones) and as an industrial abrasive for sandblasting and water-jet cutting due to its hardness.
Geological facts
Almandine is the most common garnet and is the traditional birthstone for January. It was historically called 'Carbuncle' in ancient times. Some rare specimens exhibit asterism (the star effect).
Field identification & locations
Identify in the field by its distinct crystal shape (12-sided dodecahedrons), its lack of cleavage, and its high hardness relative to surrounding rock. Common in metamorphic belts worldwide like those in New York, Idaho, and India.
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Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)
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