Rock Identifier
Tumbled jasper (Microcrystalline quartz (chalcedony), SiO₂, colored by iron oxides) — mineral
mineral

Tumbled jasper

Microcrystalline quartz (chalcedony), SiO₂, colored by iron oxides

AI-generated identification · may be incorrect

Opaque, polished reddish-brown and cream stone with waxy-to-dull luster; Mohs hardness 6.5–7, no visible cleavage, conchoidal fracture, and microcrystalline quartz structure. The mottled pattern is typical of jasper, though exact variety cannot be confirmed from the image alone.

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Physical properties

Opaque, polished reddish-brown and cream stone with waxy-to-dull luster; Mohs hardness 6.5–7, no visible cleavage, conchoidal fracture, and microcrystalline quartz structure. The mottled pattern is typical of jasper, though exact variety cannot be confirmed from the image alone.

Formation & geological history

Forms when silica-rich groundwater fills cavities or replaces volcanic and sedimentary material, with iron producing red-brown coloration. Deposits occur from Precambrian to recent ages; this specimen has been cut or tumbled and polished.

Uses & applications

Used for cabochons, beads, carvings, ornaments, and lapidary pieces; occasionally as decorative aggregate. Common tumbled specimens generally have modest market value.

Geological facts

Jasper is a variety of opaque chalcedony rather than a single mineral species, and its colors reflect impurities and alteration history. Similar material may be sold as red jasper, picture jasper, or brecciated jasper.

Field identification & locations

Identify it by opacity, earthy iron-rich colors, smooth polish, and quartz-like hardness; it should scratch glass but resist a steel knife. Common sources include India, Madagascar, Brazil, the United States, and Australia.