
mineral
Garnet
Almandine Garnet (Fe3Al2(SiO4)3)
AI-generated identification · may be incorrectHardness: 6.5–7.5 Mohs scale. Color: Deep reddish-brown to dark purple/black. Luster: Vitreous to resinous. Crystal structure: Isometric (dodecahedral). Cleavage: None. Specific gravity: 3.5–4.3.
- Hardness
- 6
- Color
- Deep reddish-brown to dark purple/black
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 6.5–7.5 Mohs scale. Color: Deep reddish-brown to dark purple/black. Luster: Vitreous to resinous. Crystal structure: Isometric (dodecahedral). Cleavage: None. Specific gravity: 3.5–4.3.
Formation & geological history
Formed under high-pressure, high-temperature metamorphic conditions, typically in mica schists or gneisses. Found in regions of plate tectonic convergence.
Uses & applications
Abrasives (sandblasting, waterjet cutting), gemstones for jewelry to celebrate January birthdays, and as an index mineral for determining metamorphic grade.
Geological facts
Garnets have been used as gemstones since the Bronze Age. They are the official birthstone for January and are famous for being found as perfectly formed twelve-sided crystals (dodecahedrons).
Field identification & locations
Identify by its distinctive crystal habit (soccer ball-like shape), lack of cleavage, and high hardness. Commonly found in metamorphic terrains like the Adirondack Mountains or the Alps.
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
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