
metamorphic
Banded gneiss pebble
Quartz–feldspar gneiss, possibly with biotite or amphibole
AI-generated identification · may be incorrectRounded, tan-pink pebble with a dark mineral-rich band and faint foliation; likely quartz and feldspar with darker mica or amphibole. Quartz hardness is 7 and feldspar about 6; exact composition and specific gravity cannot be determined from the image.
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Physical properties
Rounded, tan-pink pebble with a dark mineral-rich band and faint foliation; likely quartz and feldspar with darker mica or amphibole. Quartz hardness is 7 and feldspar about 6; exact composition and specific gravity cannot be determined from the image.
Formation & geological history
Formed when pre-existing rock was recrystallized under high heat and pressure, producing mineral banding; its precise age and source are not identifiable from the photo.
Uses & applications
Primarily a collecting specimen or decorative pebble; gneiss is also used as building and dimension stone.
Geological facts
Gneissic banding reflects the segregation of light and dark minerals during metamorphism.
Field identification & locations
Look for alternating pale quartz–feldspar and darker mineral bands, often with a foliated texture; similar pebbles occur in glacial deposits, river gravels, and regions underlain by metamorphic rocks.
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