
metamorphic
Polished dark metamorphic cobble
Likely amphibolite or hornblende-rich schist; exact identification requires thin-section or chemical testing
AI-generated identification · may be incorrectDark gray-black, fine- to medium-grained, with subtle bronzy-brown streaks and a satiny luster from polishing; likely Mohs 5–6, with weak foliation and no obvious cleavage visible on the rounded surface. Composition is probably hornblende, plagioclase, biotite, and minor iron oxides.
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Physical properties
Dark gray-black, fine- to medium-grained, with subtle bronzy-brown streaks and a satiny luster from polishing; likely Mohs 5–6, with weak foliation and no obvious cleavage visible on the rounded surface. Composition is probably hornblende, plagioclase, biotite, and minor iron oxides.
Formation & geological history
Formed when basaltic or gabbroic rock underwent medium- to high-grade regional metamorphism, commonly during Precambrian or Paleozoic mountain-building; the specimen was later rounded by stream or glacial transport and polished.
Uses & applications
Used as decorative stone, landscaping material, polished display specimens, and occasionally aggregate; generally not a gemstone.
Geological facts
Amphibolite can resemble dark basalt, but aligned amphibole crystals or faint foliation distinguish many specimens. Brown-gold zones may reflect weathered biotite or iron-oxide staining.
Field identification & locations
Common in metamorphic belts and glacial or river gravels worldwide. Look for elongated hornblende grains, faint planar alignment, dense weight, and a scratch resistance near that of steel; acid testing is unhelpful.
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