Rock Identifier
Red jasper (iron-rich chert), possibly brecciated (Jasper: microcrystalline quartz (SiO₂) colored mainly by hematite/goethite; likely chert/jasper with iron-oxide veining) — sedimentary
sedimentary

Red jasper (iron-rich chert), possibly brecciated

Jasper: microcrystalline quartz (SiO₂) colored mainly by hematite/goethite; likely chert/jasper with iron-oxide veining

AI-generated identification · may be incorrect

Typically Mohs hardness 6.5–7, opaque, red-orange to brown with darker brecciated zones, and a dull to waxy or glassy luster. Quartz has a cryptocrystalline structure with no visible cleavage; specific gravity is about 2.6.

Identified More sedimentary
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Physical properties

Typically Mohs hardness 6.5–7, opaque, red-orange to brown with darker brecciated zones, and a dull to waxy or glassy luster. Quartz has a cryptocrystalline structure with no visible cleavage; specific gravity is about 2.6.

Formation & geological history

Forms when silica-rich sediments or volcanic fluids become silicified, with iron oxides producing the red coloration; brecciation may reflect later fracturing and cementation. Ages vary widely, commonly Precambrian to younger.

Uses & applications

Used as lapidary rough, cabochons, carvings, beads, and decorative stone; attractive pieces are collectible but generally inexpensive.

Geological facts

Jasper is a variety of opaque, impure chert rather than a single mineral. The specimen’s strong orange-red color and dark angular banding are characteristic of iron-rich jasper.

Field identification & locations

Identify by its opaque red color, very fine texture, lack of cleavage, and inability to scratch it with a steel knife easily; a streak test is usually pale red-brown. Common sources include India, Brazil, Madagascar, Australia, South Africa, and the western United States.