Rock Identifier
Likely garnet-bearing metamorphic rock (Garnet-mica schist or amphibolite; probable garnet-group mineral (X3Y2(SiO4)3) with mica/amphibole) — metamorphic
metamorphic

Likely garnet-bearing metamorphic rock

Garnet-mica schist or amphibolite; probable garnet-group mineral (X3Y2(SiO4)3) with mica/amphibole

AI-generated identification · may be incorrect

Dark gray-green, coarse-grained, with pale reflective cleavage surfaces and possible granular garnet; mica has Mohs hardness 2–3, garnet 6.5–7.5. Luster is vitreous to pearly, and foliation may be present.

Identified More metamorphic
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Physical properties

Dark gray-green, coarse-grained, with pale reflective cleavage surfaces and possible granular garnet; mica has Mohs hardness 2–3, garnet 6.5–7.5. Luster is vitreous to pearly, and foliation may be present.

Formation & geological history

Formed when clay-rich or mafic rocks were subjected to elevated heat and pressure during regional metamorphism, commonly during mountain building. Exact age cannot be determined from the photograph.

Uses & applications

Primarily a teaching and collecting specimen; garnet-rich material may be used abrasively, while sound schist or amphibolite can serve as decorative stone or aggregate.

Geological facts

The pale, shiny areas may be mica or feldspar rather than a gemstone. A streak, hardness, and close examination of crystal shape would distinguish garnet schist from amphibolite.

Field identification & locations

Look for foliation, sparkly platy mica, and hard rounded garnet grains; garnet will scratch glass, while mica will not. Common in metamorphic belts worldwide, including New England, the Appalachians, Scandinavia, and India.