Rock Identifier
Rounded quartz-rich pebble (Likely quartzite or quartz-rich metamorphic rock; exact identification requires testing) — metamorphic
metamorphic

Rounded quartz-rich pebble

Likely quartzite or quartz-rich metamorphic rock; exact identification requires testing

AI-generated identification · may be incorrect

Tan-gray, fine- to medium-grained, dull to slightly sparkly surface with rounded water-worn form; likely Mohs hardness 6.5–7, no obvious cleavage, and specific gravity about 2.6–2.7. The pale grains and possible quartz sparkle are consistent with quartzite, though weathered sandstone is also possible.

Identified More metamorphic
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Physical properties

Tan-gray, fine- to medium-grained, dull to slightly sparkly surface with rounded water-worn form; likely Mohs hardness 6.5–7, no obvious cleavage, and specific gravity about 2.6–2.7. The pale grains and possible quartz sparkle are consistent with quartzite, though weathered sandstone is also possible.

Formation & geological history

If quartzite, it formed when quartz sandstone was recrystallized under heat and pressure, commonly during regional mountain-building; its age cannot be determined from the image. The current rounded shape reflects erosion and transport in a river, beach, or gravel deposit.

Uses & applications

Suitable as a decorative pebble, landscaping stone, or lapidary material; quartzite is also used as aggregate and dimension stone. This individual piece has little commercial value unless it displays unusual color or texture.

Geological facts

Quartz-rich rocks commonly resist weathering, allowing them to survive transport as rounded cobbles. A glass-scratch test can help confirm quartz hardness, though it may damage the specimen.

Field identification & locations

Common in streambeds, beaches, glacial deposits, and quartzite-bearing terrains worldwide; inspect for interlocking quartz grains and test whether it scratches glass. Value is typically $1–$10 for a common collected pebble, or $10–$30 if polished or unusually attractive.