
metamorphic
Iron-stained quartzite pebble
Quartzite, composed predominantly of quartz (SiO₂) with iron-oxide staining
AI-generated identification · may be incorrectLikely hard (about 7 Mohs), rounded and fine-grained, with a gray-brown surface and rusty orange bands. Quartz has a trigonal crystal structure, but quartzite shows no obvious cleavage and typically breaks across interlocking grains; the image does not permit definitive identification.
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Physical properties
Likely hard (about 7 Mohs), rounded and fine-grained, with a gray-brown surface and rusty orange bands. Quartz has a trigonal crystal structure, but quartzite shows no obvious cleavage and typically breaks across interlocking grains; the image does not permit definitive identification.
Formation & geological history
Quartz-rich sandstone recrystallized under heat and pressure into quartzite; iron oxides likely produced the orange-brown staining. Its age and source cannot be determined from the photograph.
Uses & applications
Quartzite is used as aggregate, road stone, building stone, and decorative material; this small pebble is mainly suitable for collecting or landscaping.
Geological facts
Quartzite is generally harder and more resistant to weathering than its sandstone precursor.
Field identification & locations
The rounded shape suggests transport by water or glacial action. Look for a hard, gritty-to-glassy texture and grains that resist being scratched by a steel knife; similar pebbles occur in riverbeds and glacial deposits.
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