Rock Identifier
Red jasper (likely tumbled or naturally worn) (Jasper, microcrystalline quartz/chalcedony (SiO₂), colored mainly by iron oxides) — mineral
mineral

Red jasper (likely tumbled or naturally worn)

Jasper, microcrystalline quartz/chalcedony (SiO₂), colored mainly by iron oxides

AI-generated identification · may be incorrect

Typically opaque brick-red to orange-red, earthy to dull vitreous luster, hardness about 6.5–7 Mohs, and no visible cleavage; dense, fine-grained cryptocrystalline quartz. The specimen appears rough and partially polished, with dark inclusions or surface pits.

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Physical properties

Typically opaque brick-red to orange-red, earthy to dull vitreous luster, hardness about 6.5–7 Mohs, and no visible cleavage; dense, fine-grained cryptocrystalline quartz. The specimen appears rough and partially polished, with dark inclusions or surface pits.

Formation & geological history

Forms when silica-rich fluids replace or cement volcanic ash, sediments, or cavities, with iron oxides producing the red color. Jasper deposits range from Precambrian to recent geological ages and occur in volcanic and sedimentary terrains.

Uses & applications

Used for beads, cabochons, carvings, ornaments, and lapidary pieces; historically used for tools and decorative stone. Common material has modest commercial value.

Geological facts

Jasper is a variety of chalcedony and may grade into chert, iron-rich silica, or brecciated jasper. Color intensity depends on hematite and other iron minerals.

Field identification & locations

Identify it by its opaque red color, fine texture, waxy-to-dull luster, and inability to scratch with a steel knife; quartz should scratch glass. Common sources include India, Madagascar, Brazil, Australia, and the western United States.