
sedimentary
Polished brecciated jasper tower
Jasper, an opaque microcrystalline quartz (SiO₂), with iron-oxide-rich red breccia and possible chalcedony
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque multicolored red, gray, brown, and cream pattern; vitreous to waxy luster when polished; cryptocrystalline quartz with no visible cleavage, conchoidal fracture, and typical specific gravity near 2.6.
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Physical properties
Hardness about 6.5–7 Mohs; opaque multicolored red, gray, brown, and cream pattern; vitreous to waxy luster when polished; cryptocrystalline quartz with no visible cleavage, conchoidal fracture, and typical specific gravity near 2.6.
Formation & geological history
Formed when silica-rich fluids replaced or cemented volcanic or sedimentary material, commonly preserving angular breccia fragments colored by hematite or other iron oxides. Its exact geological age and locality cannot be determined from the photograph.
Uses & applications
Used for cabochons, carvings, ornamental towers, beads, and polished slabs; valued mainly as a decorative lapidary material rather than a gemstone of high rarity.
Geological facts
The angular, sharply contrasting fragments and red iron staining are characteristic of brecciated jasper. Jasper is a variety of chert and is composed primarily of quartz despite its earthy appearance.
Field identification & locations
Identify it by its opaque, strongly patterned appearance, glassy polish, and ability to scratch glass; a steel knife generally will not scratch it. Common sources include Oregon, Utah, Idaho, Arizona, Mexico, Madagascar, and Australia.
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