
mineral
Garnet (almandine or pyrope variety)
Silicate mineral Group: (Fe, Mg, Mn, Ca)3(Al, Fe, Cr)2(SiO4)3
Hardness: 6.5–7.5 on Mohs scale; Color: Deep reddish-brown to dark purple-red; Luster: Vitreous to sub-vitreous; Crystal Structure: Isometric (dodecahedral); Cleavage: Indistinct; Specific Gravity: 3.5–4.3
- Hardness
- 6
- Color
- Deep reddish-brown to dark purple-red
- Luster
- Vitreous to sub-vitreous
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Physical properties
Hardness: 6.5–7.5 on Mohs scale; Color: Deep reddish-brown to dark purple-red; Luster: Vitreous to sub-vitreous; Crystal Structure: Isometric (dodecahedral); Cleavage: Indistinct; Specific Gravity: 3.5–4.3
Formation & geological history
Usually forms in metamorphic rocks (such as schist or gneiss) under high temperature and pressure, or in some igneous rocks. They are found across a wide range of geological ages from Precambrian to Cenozoic.
Uses & applications
Primary use is in jewelry as a gemstone. Industrial uses include abrasive blasting (sandblasting alternative), water jet cutting, and water filtration granules due to its hardness and chemical resistance.
Geological facts
Garnet is the birthstone for January. The name 'garnet' comes from the Latin 'granatus' (grain), likely a reference to the 'punica granatum' (pomegranate), as its crystals resemble the fruit's red seeds.
Field identification & locations
Identify in the field by its characteristic red-to-brown color, lack of cleavage, and dodecahedral crystal habit. It often pops out as harder, raised bumps on the surface of weathered metamorphic rock. Commonly found in India, Madagascar, and the USA.
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