Rock Identifier
Orbicular jasper (Silicified volcanic or sedimentary rock, primarily microcrystalline quartz (SiO₂) with iron-oxide minerals) — sedimentary
sedimentary

Orbicular jasper

Silicified volcanic or sedimentary rock, primarily microcrystalline quartz (SiO₂) with iron-oxide minerals

AI-generated identification · may be incorrect

Typically tan, cream, red, and brown orbicular patterns; opaque, earthy to dull/waxy luster, massive structure, no cleavage, and Mohs hardness about 6.5–7. The rounded specimen appears naturally weathered or roughly tumbled.

Identified More sedimentary
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Physical properties

Typically tan, cream, red, and brown orbicular patterns; opaque, earthy to dull/waxy luster, massive structure, no cleavage, and Mohs hardness about 6.5–7. The rounded specimen appears naturally weathered or roughly tumbled.

Formation & geological history

Forms when silica-rich fluids replace or cement volcanic ash, sediment, or preexisting rock, producing concentric mineral growths and iron staining. Exact age cannot be determined from the image; deposits range from Precambrian to much younger.

Uses & applications

Used for cabochons, beads, carvings, decorative stones, and lapidary collectibles; too small and patterned for construction use.

Geological facts

Orbicular jasper is valued for its distinctive eye-like or floral spheres, though similar material may be sold as ocean jasper, leopard jasper, or rhyolite depending on locality and composition.

Field identification & locations

Identify by its opaque concentric orb patterns, silica hardness, lack of visible cleavage, and inability to scratch with a steel coin easily; common sources include Madagascar, Mexico, Australia, and the western United States. A locality label or testing is needed for precise identification.