
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 incorrectTypically 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.
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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.
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