Rock Identifier
Tumbled yellow jasper or chert pebble (Microcrystalline quartz (SiO₂), likely jasper/chert with iron-oxide staining) — sedimentary
sedimentary

Tumbled yellow jasper or chert pebble

Microcrystalline quartz (SiO₂), likely jasper/chert with iron-oxide staining

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; opaque cream-yellow color with faint reddish-brown veining, dull to waxy luster, and conchoidal fracture hidden by tumbling. Quartz has a trigonal crystal structure but is present here as microcrystalline mass with no visible cleavage.

Identified More sedimentary
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Physical properties

Hardness about 6.5–7 Mohs; opaque cream-yellow color with faint reddish-brown veining, dull to waxy luster, and conchoidal fracture hidden by tumbling. Quartz has a trigonal crystal structure but is present here as microcrystalline mass with no visible cleavage.

Formation & geological history

Formed when silica-rich fluids replaced or cemented sediment, often incorporating iron oxides that produce the yellow coloration; likely Paleozoic or younger, though age cannot be determined from the photograph. The rounded shape indicates natural water abrasion and/or mechanical tumbling.

Uses & applications

Used as a decorative stone, lapidary material, cabochons, beads, carvings, and inexpensive polished specimens; not typically used as a major construction stone.

Geological facts

Jasper is an opaque variety of chalcedony or microcrystalline quartz, while chert is the broader geological term for similar silica-rich rock. Color alone cannot reliably distinguish jasper from stained quartzite or other silicified rock.

Field identification & locations

Look for high hardness, opacity, waxy texture, and inability to scratch with a steel knife; it should scratch glass but not be scratched by ordinary steel. Common in stream gravels and silica-rich formations worldwide.