
mineral
Garnet (likely Almandine)
Almandine Garnet, Fe3Al2(SiO4)3
Hardness: 6.5–7.5 on Mohs scale; Color: Deep red to brownish-red; Luster: Vitreous to resinous; Crystal structure: Isometric (dodecahedral habits); Cleavage: None (conchoidal fracture); Specific gravity: 3.5–4.3.
- Hardness
- 6
- Color
- Deep red to brownish-red
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 6.5–7.5 on Mohs scale; Color: Deep red to brownish-red; Luster: Vitreous to resinous; Crystal structure: Isometric (dodecahedral habits); Cleavage: None (conchoidal fracture); Specific gravity: 3.5–4.3.
Formation & geological history
Formed under high-pressure and high-temperature conditions during regional metamorphism of clay-rich sedimentary rocks (shales). Often found in metamorphic schists and gneisses, or as detrital grains in river sands.
Uses & applications
Used primarily in jewelry as a gemstone and in industry as an abrasive (sandpaper, waterjet cutting) due to its hardness and lack of cleavage.
Geological facts
Garnets have been used as gemstones since the Bronze Age. The name 'garnet' comes from the Latin 'granatus' (grain/seed), likely referencing its resemblance to pomegranate seeds. It is the birthstone for January.
Field identification & locations
Identify in the field by its distinct 12-sided (dodecahedral) or 24-sided (trapezohedral) crystal shape, deep red color, and lack of cleavage. Common locations include New York (USA), India, Brazil, and Madagascar.
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