
sedimentary
Banded jasper (likely brecciated jasper)
Microcrystalline quartz/chalcedony, SiO₂, with iron-oxide and other mineral impurities
AI-generated identification · may be incorrectOpaque, rough to partly polished; gray, brown, cream, and red bands or breccia-like patches, with dull to waxy luster. Mohs hardness about 6.5–7; no prominent cleavage, conchoidal fracture, and specific gravity near 2.6.
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Physical properties
Opaque, rough to partly polished; gray, brown, cream, and red bands or breccia-like patches, with dull to waxy luster. Mohs hardness about 6.5–7; no prominent cleavage, conchoidal fracture, and specific gravity near 2.6.
Formation & geological history
Forms when silica-rich groundwater replaces or cements sediment, volcanic ash, or fractured rock; red coloration comes mainly from hematite. Jasper deposits range from Precambrian to much younger, depending on locality.
Uses & applications
Used for cabochons, carvings, ornaments, lapidary slabs, and decorative stone; dense varieties may serve as minor aggregate or building stone.
Geological facts
The specimen’s blocky internal fractures and contrasting red-gray colors are typical of brecciated or banded jasper rather than a single crystalline mineral.
Field identification & locations
Identify it by its opaque appearance, very hard quartz-like surface, lack of visible individual crystals, and resistance to scratching by a steel file; common sources include Oregon, Utah, Arizona, India, Madagascar, and South Africa.
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