
mineral
Garnet
Almandine formula: Fe3Al2(SiO4)3
AI-generated identification · may be incorrectHardness: 6.5-7.5 on Mohs scale. Color: Deep red to reddish-purple. Luster: Vitreous to resinous. Crystal structure: Isometric (often dodecahedral). Cleavage: None (conchoidal fracture). Specific gravity: 3.5-4.3.
- Hardness
- 6
- Color
- Deep red to reddish-purple
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 6.5-7.5 on Mohs scale. Color: Deep red to reddish-purple. Luster: Vitreous to resinous. Crystal structure: Isometric (often dodecahedral). Cleavage: None (conchoidal fracture). Specific gravity: 3.5-4.3.
Formation & geological history
Formed most commonly in metamorphic rocks such as mica schist or gneiss during high-pressure and high-temperature regional metamorphism. Can also be found in igneous rocks like pegmatites.
Uses & applications
Used widely as a gemstone in jewelry. In industry, it is used as an abrasive in sandblasting, waterjet cutting, and for water filtration media due to its hardness and angular fracture.
Geological facts
Garnets have been used as gemstones and abrasives since the Bronze Age. While red is most common, garnets actually occur in every color except pure blue. It is the birthstone for January.
Field identification & locations
Identify in the field by its characteristic red color and glassy, fractured appearance in host rock. It frequently forms distinct, rounder 'grains' compared to surrounding minerals. Common locations include New York, Idaho, India, and Brazil.
More like this
Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous