
metamorphic
Weathered quartz-rich rock, possibly quartzite or iron-stained quartz
Quartz (SiO₂), likely in a quartzite matrix with iron-oxide staining
AI-generated identification · may be incorrectOff-white to pale yellow-orange, granular and irregular, with a dull to weakly glassy luster; quartz hardness is about 7 Mohs, lacks cleavage, and has specific gravity near 2.65. The image is too limited for confident identification of texture or crystal structure.
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Physical properties
Off-white to pale yellow-orange, granular and irregular, with a dull to weakly glassy luster; quartz hardness is about 7 Mohs, lacks cleavage, and has specific gravity near 2.65. The image is too limited for confident identification of texture or crystal structure.
Formation & geological history
If quartzite, it formed when quartz-rich sandstone was metamorphosed and recrystallized, typically during regional mountain-building; iron oxides produced the orange staining through weathering. A precise geological age cannot be determined from the photograph.
Uses & applications
Common quartzite is used as aggregate, building stone, road material, and sometimes decorative stone; attractive quartz specimens may be collected but this piece appears low-grade.
Geological facts
Quartzite commonly breaks across quartz grains rather than around them, producing a sugary or splintery fracture. Orange coloration commonly comes from hematite or limonite coatings and staining.
Field identification & locations
Look for a very hard, quartz-rich surface that scratches glass and does not react with dilute hydrochloric acid; a steel nail should not scratch it. Common worldwide, especially in metamorphic belts and exposed sandstone formations.
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