Rock Identifier
Likely garnet-bearing rock (possibly almandine garnet in matrix) (Garnet, likely almandine (Fe₃Al₂Si₃O₁₂); host rock cannot be determined from the image) — metamorphic
metamorphic

Likely garnet-bearing rock (possibly almandine garnet in matrix)

Garnet, likely almandine (Fe₃Al₂Si₃O₁₂); host rock cannot be determined from the image

AI-generated identification · may be incorrect

Rough, reddish-brown specimen with a granular surface; garnet is typically Mohs 6.5–7.5, vitreous, cubic, and lacks cleavage, with uneven to conchoidal fracture. The photo does not show enough detail to confirm crystals or composition.

Identified More metamorphic →
Explore Likely garnet-bearing rock (possibly almandine garnet in matrix) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Rough, reddish-brown specimen with a granular surface; garnet is typically Mohs 6.5–7.5, vitreous, cubic, and lacks cleavage, with uneven to conchoidal fracture. The photo does not show enough detail to confirm crystals or composition.

Formation & geological history

Almandine commonly forms during regional metamorphism of aluminum-rich sediments, often in schist or gneiss; such rocks range from hundreds of millions to billions of years old. The specimen’s specific age and origin are unknown.

Uses & applications

Garnet is used as an abrasive and, when transparent and attractive, as a gemstone; garnet-bearing rock is also collected as a mineral specimen.

Geological facts

Garnet is a mineral group rather than a single mineral; almandine is among its most common species.

Field identification & locations

Look for distinct deep-red crystals with a glassy luster and no cleavage, often embedded in metamorphic rock. Common sources include India, Sri Lanka, Madagascar, and parts of the United States; the pictured piece is not identifiable to locality.