
mineral
Almandine Garnet
Almandine (Fe3Al2Si3O12)
Hardness: 7-7.5. Color: Dark red to brownish black. Luster: Vitreous to resinous. Crystal structure: Isometric (dodecahedron). Cleavage: None (conchoidal fracture). Specific gravity: 4.1-4.3.
- Hardness
- 7-7
- Color
- Dark red to brownish black
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 7-7.5. Color: Dark red to brownish black. Luster: Vitreous to resinous. Crystal structure: Isometric (dodecahedron). Cleavage: None (conchoidal fracture). Specific gravity: 4.1-4.3.
Formation & geological history
Formed in regional metamorphic rocks such as mica schists and gneisses under high pressure and temperature conditions. It can also be found in some igneous rocks like granites.
Uses & applications
Used widely as an abrasive (sandpaper, waterjet cutting), a gemstone for jewelry, and as a geological indicator of metamorphic conditions.
Geological facts
Almandine is the most common member of the garnet group. It is sometimes called 'Carbuncle' in historic texts. It is the birthstone for January.
Field identification & locations
Identify by its 'soccer ball' (dodecahedral) shape, high density, and lack of cleavage. Commonly found in metamorphic terrains such as the Adirondacks or the Alps.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Biotite Schist
Biotite-rich Schist [K(Mg,Fe)3AlSi3O10(F,OH)2]
metamorphic