Rock Identifier
Polished brecciated iron-rich rock, possibly jasper or chert (Brecciated silica-rich rock; likely microcrystalline quartz (SiO₂) with iron-oxide minerals) — sedimentary
sedimentary

Polished brecciated iron-rich rock, possibly jasper or chert

Brecciated silica-rich rock; likely microcrystalline quartz (SiO₂) with iron-oxide minerals

AI-generated identification · may be incorrect

Typically hardness about 6.5–7 Mohs, earthy brown, gray, black, and rusty-red colors, and a dull to waxy or glassy luster. The irregular fragments and iron-stained matrix suggest brecciation; individual crystals are mostly microscopic, with no obvious cleavage.

Identified More sedimentary
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Physical properties

Typically hardness about 6.5–7 Mohs, earthy brown, gray, black, and rusty-red colors, and a dull to waxy or glassy luster. The irregular fragments and iron-stained matrix suggest brecciation; individual crystals are mostly microscopic, with no obvious cleavage.

Formation & geological history

Likely formed when silica-rich sediment or volcanic material fractured and was cemented by quartz and iron oxides, then later weathered and rounded. Its exact geological age and locality cannot be determined from the photograph alone.

Uses & applications

Used as a decorative stone, tumbled specimen, lapidary material, and occasionally in cabochons or small carvings; not generally important as a construction stone.

Geological facts

The metallic-looking dark areas may be hematite or magnetite, while orange-brown patches are likely limonite/goethite. A streak, hardness, magnetism, and acid tests would substantially improve identification.

Field identification & locations

Look for a very hard surface that scratches glass, a white-to-reddish streak, and possible weak magnetism; jasper/chert commonly occurs in sedimentary beds, volcanic terrains, and gravel deposits worldwide.