Rock Identifier
Rough red garnets (Garnet-group minerals, likely almandine (Fe₃Al₂(SiO₄)₃) or pyrope–almandine; species cannot be confirmed from the photo alone) — gemstone
gemstone

Rough red garnets

Garnet-group minerals, likely almandine (Fe₃Al₂(SiO₄)₃) or pyrope–almandine; species cannot be confirmed from the photo alone

AI-generated identification · may be incorrect

Small, deep-red to purplish, translucent rough crystals with irregular to partly crystal-shaped surfaces and a vitreous luster. Garnets have Mohs hardness 6.5–7.5, cubic crystal structure, no cleavage, and specific gravity typically 3.5–4.3.

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Physical properties

Small, deep-red to purplish, translucent rough crystals with irregular to partly crystal-shaped surfaces and a vitreous luster. Garnets have Mohs hardness 6.5–7.5, cubic crystal structure, no cleavage, and specific gravity typically 3.5–4.3.

Formation & geological history

Garnets form in metamorphic rocks, especially schist and gneiss, and may also crystallize in some igneous rocks; weathering can concentrate them in stream or beach gravels. Their age depends on the host rock and cannot be determined from appearance.

Uses & applications

Gem-quality pieces are cut for jewelry; lower-grade garnet is used as an abrasive in blasting, waterjet cutting, and sandpaper.

Geological facts

Garnet is a mineral group, not a single mineral; its members span several colors, though red varieties are especially familiar.

Field identification & locations

The red color and lack of cleavage are consistent with garnet, but identification of these small rough pieces needs testing or gemological analysis. Garnets occur worldwide, including India, Sri Lanka, Madagascar, and the United States.