Rock Identifier
Red Garnet (Pyrope or Almandine) (Magnesium aluminum silicate (Mg3Al2(SiO4)3) or Iron aluminum silicate (Fe3Al2(SiO4)3)) — mineral
mineral

Red Garnet (Pyrope or Almandine)

Magnesium aluminum silicate (Mg3Al2(SiO4)3) or Iron aluminum silicate (Fe3Al2(SiO4)3)

Hardness: 6.5–7.5 on the Mohs scale. Color: Deep red/burgundy. Luster: Vitreous (glassy). Crystal Structure: Isometric/Cubic. Cleavage: Indistinct. Specific Gravity: 3.6–4.3.

Hardness
6
Color
Deep red/burgundy
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 6.5–7.5 on the Mohs scale. Color: Deep red/burgundy. Luster: Vitreous (glassy). Crystal Structure: Isometric/Cubic. Cleavage: Indistinct. Specific Gravity: 3.6–4.3.

Formation & geological history

Formed under high temperatures and pressures during regional metamorphism of clay-rich rocks (shales) or within igneous environments like pegmatites and kimberlites.

Uses & applications

Primarily used as a gemstone in jewelry (rings, earrings, pendants) and as a birthstone for January. Industrially, it is used as an abrasive in waterjet cutting and sandblasting due to its hardness.

Geological facts

Garnets have been used since the Bronze Age as gemstones and abrasives. Warriors in some cultures believed garnets would protect them from wounds during battle and bring victory.

Field identification & locations

Identify in the field by its dodecahedral (12-sided) crystal habit and lack of cleavage. Common locations include metamorphic belts in the USA (New York, Idaho), India, Sri Lanka, and Madagascar.