Rock Identifier
Reddish-brown fine-grained rock (likely jasper or iron-stained chert) (Microcrystalline quartz, SiO₂, with iron-oxide staining; exact identification is uncertain from the photo) — sedimentary
sedimentary

Reddish-brown fine-grained rock (likely jasper or iron-stained chert)

Microcrystalline quartz, SiO₂, with iron-oxide staining; exact identification is uncertain from the photo

AI-generated identification · may be incorrect

Opaque, reddish-brown with pale veins or weathered patches and a dull to slightly waxy surface. Quartz has Mohs hardness 7 and trigonal crystal structure; the specimen shows no visible cleavage and likely breaks with irregular or conchoidal fracture.

Identified More sedimentary →
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Physical properties

Opaque, reddish-brown with pale veins or weathered patches and a dull to slightly waxy surface. Quartz has Mohs hardness 7 and trigonal crystal structure; the specimen shows no visible cleavage and likely breaks with irregular or conchoidal fracture.

Formation & geological history

If jasper or chert, it formed as silica-rich sediment or replacement in sedimentary rocks, with iron oxides supplying the color. Such material forms across many geological ages and settings.

Uses & applications

Similar material is used for carvings, beads, cabochons, and decorative stone; this small rough piece has little apparent commercial value.

Geological facts

Jasper is an opaque variety of chalcedony, while chert is a broader term for fine-grained silica rock; color alone cannot distinguish them reliably.

Field identification & locations

Look for hardness near 7, lack of cleavage, and a conchoidal fracture; a scratch or streak test can help, but the photo is insufficient for a firm ID. Chert and jasper occur worldwide in sedimentary settings.