Rock Identifier
Weathered quartz-rich rock, possibly quartzite or iron-stained quartz (Quartz (SiO₂), likely in a quartzite matrix with iron-oxide staining) — metamorphic
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 incorrect

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.

Identified More metamorphic
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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.