Rock Identifier
Tumbled jasper (likely brecciated or iron-rich jasper) (Microcrystalline quartz/chalcedony, SiO₂, colored by iron oxides and possibly other silicates) — mineral
mineral

Tumbled jasper (likely brecciated or iron-rich jasper)

Microcrystalline quartz/chalcedony, SiO₂, colored by iron oxides and possibly other silicates

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; opaque brown, reddish-brown, and dark gray with a smooth tumbled surface and waxy to dull luster. It has cryptocrystalline quartz structure, no visible cleavage, and typical specific gravity near 2.6.

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Physical properties

Hardness about 6.5–7 Mohs; opaque brown, reddish-brown, and dark gray with a smooth tumbled surface and waxy to dull luster. It has cryptocrystalline quartz structure, no visible cleavage, and typical specific gravity near 2.6.

Formation & geological history

Jasper forms when silica-rich fluids replace or cement volcanic, sedimentary, or hydrothermal material, with iron producing the brown-red coloration; ages vary widely, commonly Precambrian to younger. This specimen has been human-polished.

Uses & applications

Used for cabochons, beads, carvings, worry stones, and ornamental objects; it is inexpensive but attractive as a lapidary material.

Geological facts

Jasper is a variety of opaque chalcedony and can show brecciation, banding, orbicular patterns, or dendritic markings. Exact identification requires a fresh surface or laboratory testing because many brown stones look similar.

Field identification & locations

Identify it by its opaque appearance, fine texture, glassy/waxy polish, and resistance to scratching with a steel knife; quartz should scratch glass. Common sources include the western United States, Madagascar, Brazil, India, and Australia.