Rock Identifier
Likely quartz-rich rock (possibly milky quartz or quartzite) (Quartz-rich aggregate, predominantly silicon dioxide (SiO₂); exact identification is uncertain from the image) — metamorphic
metamorphic

Likely quartz-rich rock (possibly milky quartz or quartzite)

Quartz-rich aggregate, predominantly silicon dioxide (SiO₂); exact identification is uncertain from the image

AI-generated identification · may be incorrect

White to pale gray, rough and granular with a dull to vitreous luster. Quartz has Mohs hardness 7, no cleavage, and a hexagonal crystal structure; the rock’s hardness depends on its other minerals.

Identified More metamorphic →
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Physical properties

White to pale gray, rough and granular with a dull to vitreous luster. Quartz has Mohs hardness 7, no cleavage, and a hexagonal crystal structure; the rock’s hardness depends on its other minerals.

Formation & geological history

Could be quartzite formed when sandstone was metamorphosed, or a massive quartz vein formed from silica-rich fluids. Age and origin cannot be determined from appearance alone.

Uses & applications

Quartzite is used as construction aggregate, paving stone, and sometimes dimension stone; attractive quartz specimens are collected or used decoratively.

Geological facts

A glass-scratch test can help distinguish hard quartz-rich material from softer rocks, but it is not definitive and may damage the specimen.

Field identification & locations

Look for interlocking or fused quartz grains and a scratch-resistant surface; quartzite is common in many metamorphic terrains, while massive quartz occurs in veins worldwide. A closer view or hardness test is needed for confident identification.