
metamorphic
Polished jasper–quartzite river pebble
Silicified metasedimentary rock, chiefly microcrystalline quartz (SiO₂) with iron-oxide staining
AI-generated identification · may be incorrectHardness 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.
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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.
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