
mineral
Garnet and Quartz
Pyrope or Almandine (Red Garnets) and Quartz (Center Stone)
AI-generated identification · may be incorrectGarnet hardness: 6.5-7.5. Color: deep burgundy red. Luster: vitreous to resinous. Crystal structure: Isometric (dodecahedral). Quartz center: hardness 7, colorless.
- Hardness
- 6
- Color
- deep burgundy red
- Luster
- vitreous to resinous
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Physical properties
Garnet hardness: 6.5-7.5. Color: deep burgundy red. Luster: vitreous to resinous. Crystal structure: Isometric (dodecahedral). Quartz center: hardness 7, colorless.
Formation & geological history
Garnets typically form in metamorphic rocks like schist or gneiss under high pressure/temperature, or in some igneous rocks. Common in Precambrian through Tertiary formations.
Uses & applications
Primary use as gemstones in jewelry. Industrial uses include abrasives (sandpaper, waterjet cutting) and filtration media.
Geological facts
Garnet is the birthstone for January and has been used as a gemstone since the Bronze Age. Natural red garnets were once widely known as carruncles.
Field identification & locations
Identify by deep red color that doesn't change much under various lighting, high hardness (scratches glass), and absence of cleavage. Found in metamorphic belts globally.
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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
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