
mineral
Polished red jasper and carnelian specimens
Jasper: microcrystalline quartz (SiO₂) colored by iron oxides; carnelian: orange-red chalcedony, also SiO₂
AI-generated identification · may be incorrectOpaque to translucent red-orange, waxy to vitreous luster, commonly polished; quartz hardness 6.5–7 Mohs, no cleavage, cryptocrystalline structure, specific gravity about 2.6.
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Physical properties
Opaque to translucent red-orange, waxy to vitreous luster, commonly polished; quartz hardness 6.5–7 Mohs, no cleavage, cryptocrystalline structure, specific gravity about 2.6.
Formation & geological history
Formed when silica-rich groundwater fills cavities or replaces volcanic and sedimentary rock, with iron producing the red color; deposits range from Precambrian to younger geological ages.
Uses & applications
Used for cabochons, beads, carvings, ornaments, and lapidary collections; jasper is also used decoratively in tiles and architectural stone.
Geological facts
The dark red center is likely jasper, while the brighter orange-red pieces may be carnelian or iron-rich jasper; exact identification requires translucency and locality information.
Field identification & locations
Identify by hardness, waxy polish, absence of cleavage, and red/orange iron staining; common sources include Brazil, India, Madagascar, Uruguay, Australia, and the western United States.
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