Rock Identifier
Tumbled quartz-rich stone, possibly milky quartz or quartzite (Quartz (SiO₂), potentially quartzite if composed of recrystallized quartz grains) — mineral
mineral

Tumbled quartz-rich stone, possibly milky quartz or quartzite

Quartz (SiO₂), potentially quartzite if composed of recrystallized quartz grains

AI-generated identification · may be incorrect

Creamy white, translucent to opaque, with a glassy-to-waxy luster and rounded tumbled form; quartz hardness is Mohs 7, with no cleavage and conchoidal fracture. Exact identification is limited by the image and lack of testing.

Identified More mineral
Explore Tumbled quartz-rich stone, possibly milky quartz or quartzite in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Creamy white, translucent to opaque, with a glassy-to-waxy luster and rounded tumbled form; quartz hardness is Mohs 7, with no cleavage and conchoidal fracture. Exact identification is limited by the image and lack of testing.

Formation & geological history

Quartz crystallizes from silica-rich igneous, hydrothermal, and metamorphic fluids; quartzite forms when sandstone recrystallizes under heat and pressure. Quartz is geologically widespread and ranges from ancient Precambrian rocks to modern deposits.

Uses & applications

Used for decorative stones, countertops, abrasives, glass, ceramics, and jewelry; this small rounded specimen is mainly suitable for collecting or ornamentation.

Geological facts

Quartz is one of Earth’s most abundant minerals and is piezoelectric, generating an electrical charge under pressure.

Field identification & locations

Common in quartz veins, granite, sandstone, and river gravels worldwide. A steel file should not scratch it; glass is typically scratched by quartz, while acid produces no reaction.