
metamorphic
Banded metamorphic rock, likely gneiss or foliated amphibolite
Quartz–feldspar–mica gneiss or amphibolite; exact identification requires testing
AI-generated identification · may be incorrectGray-green, fine- to medium-grained, strongly foliated and contorted, with a dull to slightly silky luster. Typical hardness is about 5–7 Mohs; mineral grains and specific gravity cannot be confirmed from the image.
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Physical properties
Gray-green, fine- to medium-grained, strongly foliated and contorted, with a dull to slightly silky luster. Typical hardness is about 5–7 Mohs; mineral grains and specific gravity cannot be confirmed from the image.
Formation & geological history
Formed when preexisting igneous or sedimentary rock underwent high-pressure, high-temperature metamorphism, producing folded mineral banding. Its geological age is indeterminate from appearance alone and may range from Precambrian to younger.
Uses & applications
Used locally as decorative stone, landscaping material, and aggregate; attractive polished pieces may be sold as specimens, though this example appears chiefly collectible rather than gem-quality.
Geological facts
The wavy light-and-dark fabric records ductile deformation during metamorphism. Green coloration may indicate amphibole, chlorite, epidote, or other mafic minerals.
Field identification & locations
Look for planar foliation, alternating light and dark mineral bands, and resistance to scratching with a steel knife; a streak, acid, hardness, and thin-section test would distinguish gneiss from amphibolite or schist. Common in ancient metamorphic belts worldwide.
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