
metamorphic
Likely weathered quartzite or quartz-rich sandstone
Quartzite; predominantly microcrystalline quartz (SiO₂), possibly retaining sandstone texture
AI-generated identification · may be incorrectGray-tan, fine-grained, dull to subtly sparkling surface with irregular fractures and no obvious cleavage; quartz hardness is about Mohs 7, with generally high durability and specific gravity near 2.65.
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Physical properties
Gray-tan, fine-grained, dull to subtly sparkling surface with irregular fractures and no obvious cleavage; quartz hardness is about Mohs 7, with generally high durability and specific gravity near 2.65.
Formation & geological history
Likely formed when quartz-rich sandstone was compacted and recrystallized during metamorphism, commonly during mountain-building; its exact geological age cannot be determined from the photograph.
Uses & applications
Ordinary pieces have little commercial value, while quartzite is used as crushed stone, aggregate, landscaping rock, and durable building or paving material.
Geological facts
Quartzite commonly breaks across individual grains rather than around them and is typically harder than ordinary sandstone; this specimen may also be a strongly cemented sandstone rather than true quartzite.
Field identification & locations
Test with a steel knife: it should resist scratching; quartzite may scratch glass, whereas sandstone commonly powders or scratches more easily. Common in metamorphic belts worldwide, including the Appalachians, Rocky Mountains, India, and Scandinavia.
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