
metamorphic
Weathered, foliated metamorphic rock (likely gneiss)
Quartz–feldspar–mica gneiss; exact identification requires closer examination
AI-generated identification · may be incorrectCoarse, pale gray to tan, with darker mineral flecks and weakly visible banding or foliation. Likely contains quartz, feldspar, and mica; typical gneiss hardness is about 6–7 Mohs, with no consistent cleavage at the rock scale.
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Physical properties
Coarse, pale gray to tan, with darker mineral flecks and weakly visible banding or foliation. Likely contains quartz, feldspar, and mica; typical gneiss hardness is about 6–7 Mohs, with no consistent cleavage at the rock scale.
Formation & geological history
Forms when pre-existing rocks undergo high-temperature, high-pressure metamorphism, commonly deep in continental crust. Its age cannot be determined from appearance alone.
Uses & applications
Gneiss is used as dimension stone, crushed aggregate, and landscaping stone; attractive pieces may be collected or polished.
Geological facts
Gneiss commonly develops alternating light and dark mineral bands, though weathering can obscure them.
Field identification & locations
Look for coarse interlocking grains and compositional banding; distinguish it from granite by foliation. Gneiss occurs widely in ancient continental mountain belts and exposed basement rocks.
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