
mineral
Garnet
Almandine (Fe3Al2(SiO4)3)
AI-generated identification · may be incorrectHardness: 6.5-7.5 on the Mohs scale. Color: Deep reddish-brown. Luster: Vitreous to resinous. Crystal structure: Isometric (dodecahedral). Cleavage: None. Specific gravity: 3.5-4.3.
- Hardness
- 6
- Color
- Deep reddish-brown
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 6.5-7.5 on the Mohs scale. Color: Deep reddish-brown. Luster: Vitreous to resinous. Crystal structure: Isometric (dodecahedral). Cleavage: None. Specific gravity: 3.5-4.3.
Formation & geological history
Formed through high-pressure and high-temperature regional metamorphism of clay-rich sedimentary rocks like shale. Commonly found in metamorphic rocks such as mica schists and gneisses.
Uses & applications
Used as an abrasive in sandpaper and waterjet cutting, as a gemstone in jewelry, and for geological dating and thermobarometry research.
Geological facts
Garnets are the birthstone for January and have been used in jewelry since the Bronze Age. The name comes from the Latin word 'granatus', meaning seed-like, referring to pomegranate seeds.
Field identification & locations
Identify by its 'soccer ball' shape (dodecahedron), high hardness making it resistant to scratches, and lack of cleavage. Common in heavy mineral sand deposits.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary