
mineral
Polished red jasper
Jasper, an opaque microcrystalline variety of quartz (SiO₂), commonly colored by iron oxides
AI-generated identification · may be incorrectTypically Mohs 6.5–7; brick-red to brown with black or gray inclusions, vitreous to waxy luster, cryptocrystalline quartz structure, and no visible cleavage. The smooth rounded surface indicates tumbling or polishing.
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Physical properties
Typically Mohs 6.5–7; brick-red to brown with black or gray inclusions, vitreous to waxy luster, cryptocrystalline quartz structure, and no visible cleavage. The smooth rounded surface indicates tumbling or polishing.
Formation & geological history
Forms when silica-rich fluids replace or cement sediments, volcanic ash, or cavities, with iron oxides producing the red color; specimens range from Precambrian to relatively young geological settings. Common sources include India, Madagascar, Brazil, South Africa, and the western United States.
Uses & applications
Used for beads, cabochons, carvings, ornaments, and lapidary objects; historically used for tools and decorative stone. It is durable but less valuable than transparent quartz gemstones.
Geological facts
Jasper is technically a rock rather than a single mineral, although quartz is its dominant component. Patterns and inclusions vary widely, making individual pieces attractive to collectors.
Field identification & locations
Identify it by its opaque red color, fine-grained texture, iron-oxide speckling, lack of cleavage, and ability to scratch glass; it will not show crystal faces or strong translucence. Common field varieties include red, picture, ocean, and brecciated jasper.
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Sandstone (with potential mineral staining/concretions)
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Epidote
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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