
metamorphic
Brecciated jasper (polished/cut rough specimen)
Silica-rich microcrystalline quartz aggregate, chiefly SiO₂, with iron-oxide pigments; brecciated jasper
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque, multicolored red, yellow, brown, cream, and gray; vitreous to dull/waxy luster. It consists of angular silica-rich fragments cemented by chalcedony or quartz, with irregular cavities and no prominent cleavage.
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Physical properties
Hardness about 6.5–7 Mohs; opaque, multicolored red, yellow, brown, cream, and gray; vitreous to dull/waxy luster. It consists of angular silica-rich fragments cemented by chalcedony or quartz, with irregular cavities and no prominent cleavage.
Formation & geological history
Forms when silica-rich rock or volcanic material is fractured and later cemented by silica-bearing fluids, commonly with hematite/goethite staining. Usually Cenozoic to older, depending on the deposit; precise age requires locality data.
Uses & applications
Used for cabochons, carvings, beads, ornamental slabs, and lapidary collections; occasionally as decorative stone. Its value is primarily aesthetic rather than industrial.
Geological facts
The striking colors commonly reflect iron oxides and hydroxides, while cream or translucent areas are chalcedony or quartz. Brecciation produces the angular “jigsaw” pattern characteristic of brecciated jasper.
Field identification & locations
Identify it by its opaque multicolor pattern, angular fragments, silica hardness, and lack of acid reaction; a steel file generally does not scratch it. Common sources include Oregon, Utah, Arizona, Mexico, Madagascar, and Australia.
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