
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 incorrectDark 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.
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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.
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