
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 incorrectHardness 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.
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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.
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