Rock Identifier
Weathered quartz-rich metamorphic rock, possibly quartzite or gneiss (Quartz-dominant silicate rock; likely quartz (SiO₂) with feldspar, mica, and minor iron-oxide staining) — metamorphic
metamorphic

Weathered quartz-rich metamorphic rock, possibly quartzite or gneiss

Quartz-dominant silicate rock; likely quartz (SiO₂) with feldspar, mica, and minor iron-oxide staining

AI-generated identification · may be incorrect

Gray, tan, and brown, with a massive to weakly foliated texture, glassy-to-dull luster, and irregular fracture; quartz has Mohs hardness 7, while the whole rock is typically ~6–7. Crystals are interlocking and mostly too fine or weathered to distinguish clearly.

Identified More metamorphic
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Physical properties

Gray, tan, and brown, with a massive to weakly foliated texture, glassy-to-dull luster, and irregular fracture; quartz has Mohs hardness 7, while the whole rock is typically ~6–7. Crystals are interlocking and mostly too fine or weathered to distinguish clearly.

Formation & geological history

Likely formed when quartz-rich sandstone or igneous material was recrystallized under elevated temperature and pressure, then rounded and weathered at the surface. Its exact geological age cannot be determined from the photograph.

Uses & applications

Suitable mainly as a teaching or display specimen; quartzite can be used as aggregate, dimension stone, and landscaping rock, but this weathered piece has little commercial value.

Geological facts

The tan-to-brown patches are consistent with iron-oxide alteration, while the green spot may be chlorite, epidote, or another minor mineral. A glass-scratch test can help confirm abundant quartz.

Field identification & locations

Common in metamorphic terrains and stream gravels worldwide; inspect for visible foliation, quartz grains, and hardness. A fresh broken surface and streak, acid, or laboratory testing would be needed for confident identification.