Rock Identifier
Polished red gemstone beads, possibly garnet (Unconfirmed; likely almandine garnet (Fe₃Al₂(SiO₄)₃)) — gemstone
gemstone

Polished red gemstone beads, possibly garnet

Unconfirmed; likely almandine garnet (Fe₃Al₂(SiO₄)₃)

AI-generated identification · may be incorrect

Opaque image detail limits identification; beads are dark red with a glossy polish. If garnet, hardness is about 6.5–7.5 Mohs and its crystals belong to the cubic system.

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Physical properties

Opaque image detail limits identification; beads are dark red with a glossy polish. If garnet, hardness is about 6.5–7.5 Mohs and its crystals belong to the cubic system.

Formation & geological history

If garnet, it formed during metamorphism or in igneous rocks; garnets occur in many geological ages and settings. The beads have been cut and polished from natural material.

Uses & applications

Used in jewelry and as collectible beads; garnet is also used as an abrasive and, in some varieties, as a gemstone.

Geological facts

Red garnet is a group of silicate minerals, not a single species. Bead color alone cannot distinguish garnet from other red stones or dyed materials.

Field identification & locations

The photo does not show diagnostic features, so identification is tentative. A hardness, translucency, and refractive-index test—or inspection by a gemologist—would help confirm the material.