Rock Identifier
Polished jasper–quartzite river pebble (Silicified metasedimentary rock, chiefly microcrystalline quartz (SiO₂) with iron-oxide staining) — metamorphic
metamorphic

Polished jasper–quartzite river pebble

Silicified metasedimentary rock, chiefly microcrystalline quartz (SiO₂) with iron-oxide staining

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; tan, cream, gray, and rusty-brown banding; waxy to dull luster; massive, fine-grained texture with no obvious cleavage. The rounded, polished surface indicates water abrasion or intentional tumbling.

Identified More metamorphic
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Physical properties

Hardness about 6.5–7 Mohs; tan, cream, gray, and rusty-brown banding; waxy to dull luster; massive, fine-grained texture with no obvious cleavage. The rounded, polished surface indicates water abrasion or intentional tumbling.

Formation & geological history

Likely formed when silica-rich sedimentary material was lithified and later silicified or weakly metamorphosed, with hematite/goethite producing the brown coloration. Its precise geological age and locality cannot be determined from the image.

Uses & applications

Used as a lapidary stone for cabochons, carvings, decorative polished pieces, and collection specimens; not generally important as construction aggregate in this small form.

Geological facts

The pale bands are quartz-rich zones, while dark pits and rusty areas may represent iron oxides or weathered inclusions. It may be marketed informally as jasper, quartzite, or “picture jasper,” though laboratory testing is needed for a definitive name.

Field identification & locations

Identify by its silica hardness, inability to scratch with a steel knife, opaque banding, and lack of visible large crystals; common in gravel beds and silica-rich metamorphic terrains. Value is mainly aesthetic and depends on pattern and polish.