Rock Identifier
Jasper-rich breccia (likely iron-stained jasper) (Silicified breccia composed mainly of microcrystalline quartz (SiO₂), with hematite/goethite and possibly iron-rich clay minerals) — sedimentary
sedimentary

Jasper-rich breccia (likely iron-stained jasper)

Silicified breccia composed mainly of microcrystalline quartz (SiO₂), with hematite/goethite and possibly iron-rich clay minerals

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; opaque red, orange, brown, gray, and black; generally dull to waxy luster. The angular fragments and contrasting iron-oxide matrix indicate brecciation, while quartz gives high hardness and no obvious cleavage.

Identified More sedimentary
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Physical properties

Hardness about 6.5–7 Mohs; opaque red, orange, brown, gray, and black; generally dull to waxy luster. The angular fragments and contrasting iron-oxide matrix indicate brecciation, while quartz gives high hardness and no obvious cleavage.

Formation & geological history

Likely formed when silica-rich rock fragments were fractured, cemented, and later stained or replaced by iron oxides during hydrothermal or groundwater circulation. Its precise age cannot be determined from the photograph; such material occurs in rocks ranging from Precambrian to much younger deposits.

Uses & applications

Used as lapidary material, cabochons, carvings, tumbled stone, and decorative aggregate; attractive pieces may be sold as jasper or brecciated jasper.

Geological facts

The vivid red coloration commonly comes from hematite, while yellow-brown areas may contain goethite or limonite. “Jasper” is a descriptive lapidary term rather than a single mineral species.

Field identification & locations

Identify by testing for glass-scratching hardness, examining angular fragments, and checking that it is opaque with iron-red coloration; common occurrences include hydrothermal veins and iron-rich volcanic or sedimentary terrains worldwide.