Rock Identifier
Tumbled quartz-rich pebble, likely quartzite or chert (Quartz (SiO₂), possibly quartzite; exact identification is uncertain from the image) — metamorphic
metamorphic

Tumbled quartz-rich pebble, likely quartzite or chert

Quartz (SiO₂), possibly quartzite; exact identification is uncertain from the image

AI-generated identification · may be incorrect

Hardness about 7 Mohs, tan to honey-brown, translucent in thin areas, with a waxy to dull luster and no obvious cleavage. Rounded edges and surface polish indicate tumbling; visible pale patches may be quartz or weathering zones.

Identified More metamorphic
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Physical properties

Hardness about 7 Mohs, tan to honey-brown, translucent in thin areas, with a waxy to dull luster and no obvious cleavage. Rounded edges and surface polish indicate tumbling; visible pale patches may be quartz or weathering zones.

Formation & geological history

Quartzite forms when quartz-rich sandstone recrystallizes under heat and pressure; chert forms by silica precipitation or replacement in sedimentary environments. The specimen’s geological age and precise origin cannot be determined visually.

Uses & applications

Used as a decorative tumbled stone, craft material, and collector specimen; quartzite is also used as aggregate and building stone. Typical value is modest unless unusually attractive or proven to be a rare variety.

Geological facts

Its strong resistance to scratching is characteristic of quartz-rich material. A steel file should not scratch it; glass-scratching ability would support a quartz identification.

Field identification & locations

Commonly found in stream gravels and metamorphic or sedimentary terrains worldwide. Distinguish it from calcite by hardness: calcite scratches easily with a knife and fizzes in dilute hydrochloric acid.