Rock Identifier
Mixed river gravel, prominently iron-stained chert/jasper (Microcrystalline quartz (SiO₂), chiefly chert/jasper with iron-oxide staining; mixed clasts may include quartzite and other silicates) — sedimentary
sedimentary

Mixed river gravel, prominently iron-stained chert/jasper

Microcrystalline quartz (SiO₂), chiefly chert/jasper with iron-oxide staining; mixed clasts may include quartzite and other silicates

AI-generated identification · may be incorrect

Typically Mohs hardness 6.5–7, dull to waxy or vitreous luster, opaque brown/red/yellow coloration, and no visible cleavage; the rounded surfaces indicate water abrasion. The white piece with brown circular marks appears to be a polished or weathered siliceous pebble, possibly chert or quartzite.

Identified More sedimentary
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Physical properties

Typically Mohs hardness 6.5–7, dull to waxy or vitreous luster, opaque brown/red/yellow coloration, and no visible cleavage; the rounded surfaces indicate water abrasion. The white piece with brown circular marks appears to be a polished or weathered siliceous pebble, possibly chert or quartzite.

Formation & geological history

These are water-rounded cobbles and pebbles eroded from older bedrock and deposited in a stream or gravel bar. Chert forms by silica replacement in sedimentary rocks, commonly during the Paleozoic–Cenozoic, while iron oxides create the red, orange, and brown colors.

Uses & applications

Used as decorative landscaping gravel, aggregate, lapidary material, and occasionally for cabochons or carvings. Attractive jasper and patterned chert have modest collector appeal.

Geological facts

Iron minerals such as hematite and goethite produce the rusty colors; banding, brecciation, or orbicular patterns can increase interest. The assortment is not a single uniform rock species.

Field identification & locations

Identify chert/jasper by its very fine grain, hardness, waxy fracture, and conchoidal edges; it should scratch glass but not be scratched by a steel knife. Common in stream gravels worldwide, including glacial and desert deposits.