Rock Identifier
Tumbled chalcedony or quartzite pebble (Microcrystalline quartz, SiO₂ (likely chalcedony; exact identification requires testing)) — mineral
mineral

Tumbled chalcedony or quartzite pebble

Microcrystalline quartz, SiO₂ (likely chalcedony; exact identification requires testing)

AI-generated identification · may be incorrect

Pale lavender-gray to cream, opaque to slightly translucent, with a smooth water-worn/tumbled surface and dull-to-waxy luster. Quartz hardness is about 7 Mohs; no visible cleavage, conchoidal fracture, and specific gravity near 2.6.

Identified More mineral
Explore Tumbled chalcedony or quartzite pebble in the encyclopedia →

Identify your own rocks.

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

Physical properties

Pale lavender-gray to cream, opaque to slightly translucent, with a smooth water-worn/tumbled surface and dull-to-waxy luster. Quartz hardness is about 7 Mohs; no visible cleavage, conchoidal fracture, and specific gravity near 2.6.

Formation & geological history

Likely formed as silica-rich material in a volcanic or sedimentary environment, then rounded naturally or by tumbling; its precise geological age and source cannot be determined from the image.

Uses & applications

Used for lapidary cabochons, beads, carvings, and decorative stones; common pieces have limited jewelry value.

Geological facts

The lavender tint may reflect trace iron, manganese, or other impurities, but color alone cannot confirm amethyst. A steel blade should not scratch quartz, while quartz should scratch ordinary glass.

Field identification & locations

Common as rounded stream, beach, or landscaping pebbles worldwide, especially in quartz-rich terrains. Confirm with hardness, a glass-scratch test, translucency, and specific-gravity testing; acid testing is generally uninformative.