Rock Identifier
Garnet (Almandine) (Almandine (Fe3Al2(SiO4)3)) — mineral
mineral

Garnet (Almandine)

Almandine (Fe3Al2(SiO4)3)

Hardness: 6.5-7.5. Color: Deep red, brownish-red, or blackish-red. Luster: Vitreous to resinous. Crystal structure: Isometric (dodecahedral). Cleavage: None (conchoidal fracture). Specific Gravity: 4.1-4.3.

Hardness
6
Color
Deep red, brownish-red, or blackish-red
Luster
Vitreous to resinous
Identified More mineral
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Physical properties

Hardness: 6.5-7.5. Color: Deep red, brownish-red, or blackish-red. Luster: Vitreous to resinous. Crystal structure: Isometric (dodecahedral). Cleavage: None (conchoidal fracture). Specific Gravity: 4.1-4.3.

Formation & geological history

Commonly formed during the regional metamorphism of argillaceous sediments. It is found in metamorphic rocks like mica schists and gneisses, as well as some igneous rocks.

Uses & applications

Used widely as an abrasive (sandblasting, waterjet cutting), as a gemstone in jewelry, and as a filter medium in water purification.

Geological facts

Garnet is the birthstone for January. Almandine is the most common variety of the garnet group. It has been used in jewelry since Ancient Egyptian and Roman times.

Field identification & locations

Identify by its characteristic 'pomegranate seed' color, high density, and lack of cleavage. Found globally, often in riverbeds as water-worn pebbles or embedded in schist matrices.