
mineral
Polished orbicular jasper
Jasper, microcrystalline quartz (SiO₂), with iron-oxide and other mineral inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque, reddish-orange, cream, brown, and gray; waxy to vitreous luster when polished; cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The rounded form is human-shaped/polished.
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Physical properties
Hardness about 6.5–7 Mohs; opaque, reddish-orange, cream, brown, and gray; waxy to vitreous luster when polished; cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The rounded form is human-shaped/polished.
Formation & geological history
Jasper forms when silica-rich fluids silicify volcanic ash, sediments, or breccia, with iron oxides producing red-brown colors; it is commonly Precambrian to younger. Exact locality and geological age cannot be determined from the image.
Uses & applications
Used for cabochons, carvings, spheres, ornaments, and lapidary collections; rarely used as aggregate or decorative stone. Its value is mainly aesthetic and depends on pattern, polish, size, and locality.
Geological facts
The mottled patterns may be called orbicular, brecciated, or scenic jasper, though visual identification alone cannot confirm a precise trade name. It is commonly confused with rhyolite, agate, or dyed stone.
Field identification & locations
Identify by its opaque silica-rich body, hardness, lack of cleavage, and iron-stained pattern; a steel file should generally scratch it only with difficulty. Common sources include Madagascar, Indonesia, Mexico, Brazil, and the western United States.
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