
metamorphic
Iron-stained quartz-rich rock
Likely quartzite with iron-oxide staining; identification is provisional from the image
AI-generated identification · may be incorrectMostly white to gray, glassy-to-dull quartz with rusty orange-brown iron staining and a rough, massive texture. Quartz has Mohs hardness 7, trigonal crystal structure, no cleavage, and specific gravity about 2.65; the rock appears fractured rather than cleaved.
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Physical properties
Mostly white to gray, glassy-to-dull quartz with rusty orange-brown iron staining and a rough, massive texture. Quartz has Mohs hardness 7, trigonal crystal structure, no cleavage, and specific gravity about 2.65; the rock appears fractured rather than cleaved.
Formation & geological history
If quartzite, it formed when quartz-rich sandstone was recrystallized by heat and pressure, typically during regional metamorphism. Its age and precise formation environment cannot be determined from the photograph.
Uses & applications
Quartzite is used as construction and decorative stone, aggregate, and occasionally for carving or collecting; this small rough specimen has little commercial value.
Geological facts
The orange coloration commonly results from hematite or goethite coating or staining quartz grains.
Field identification & locations
Look for a very hard, quartz-rich rock that scratches glass and does not fizz in dilute acid; quartzite typically breaks across grains rather than around them. Quartzite occurs worldwide in metamorphic belts, but this specimen’s locality is unknown.
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