
mineral
Garnet (Almandine)
Almandine (Fe3Al2(SiO4)3)
AI-generated identification · may be incorrectHardness: 6.5-7.5 on Mohs scale. Color: Deep red to reddish-brown, sometimes nearly black. 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-brown, sometimes nearly black
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 6.5-7.5 on Mohs scale. Color: Deep red to reddish-brown, sometimes nearly black. Luster: Vitreous to resinous. Crystal Structure: Isometric (often dodecahedral). Cleavage: None (conchoidal fracture). Specific Gravity: 3.5 - 4.3.
Formation & geological history
Formed under high-pressure, high-temperature conditions during regional metamorphism of clay-rich sedimentary rocks (like shale) into schist or gneiss. It is also found in some igneous rocks.
Uses & applications
Commonly used as a gemstone in jewelry (birthstone for January), but its major industrial use is as an abrasive for waterjet cutting and sandblasting due to its hardness.
Geological facts
Garnet has been used as a gemstone for thousands of years; ancient Egyptians were buried with garnet necklaces, and it was widely used in Ancient Rome for signet rings and jewelry.
Field identification & locations
Identify by its high density (heavy for its size) and deep 'wine-red' color when held up to a strong light. Commonly found in metamorphic terrains like the Adirondack Mountains (NY) or India.
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