
mineral
Garnet (Almandine/Pyrope)
Silicate Mineral (Group: X3Y2(SiO4)3 where X=Mg, Fe, Mn and Y=Al, Fe, Cr)
Hardness: 6.5-7.5 (Mohs), Color: Deep red to reddish-purple, Luster: Vitreous to resinous, Crystal Structure: Isometric (typically dodecahedral or trapezohedral), Cleavage: None (conchoidal fracture), Specific Gravity: 3.5-4.3
- Hardness
- 6
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Physical properties
Hardness: 6.5-7.5 (Mohs), Color: Deep red to reddish-purple, Luster: Vitreous to resinous, Crystal Structure: Isometric (typically dodecahedral or trapezohedral), Cleavage: None (conchoidal fracture), Specific Gravity: 3.5-4.3
Formation & geological history
Formed under high-pressure and high-temperature conditions in metamorphic rocks like schist and gneiss, or as an accessory mineral in igneous rocks such as granite or pegmatite. These specimens can range from millions to billions of years old.
Uses & applications
Widely used as an abrasive in sandblasting and water-jet cutting due to its hardness. High-quality transparent pieces are used as gemstones in jewelry. It is also the birthstone for January.
Geological facts
Garnet occupies a unique place in history; the ancient Romans used garnet signet rings to seal important documents. The name 'Garnet' is derived from the Latin word 'Garanatus,' meaning 'seedlike,' referencing its resemblance to pomegranate seeds.
Field identification & locations
Identified by its deep red color and high hardness (it will scratch glass). Often found in the field as embedded rounded crystals in metamorphic mica schists. Common locations include India, Madagascar, Sri Lanka, and the USA (Idaho/New York).
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