Rock Identifier
Tumbled orbicular jasper (likely ocean jasper) (Silicified volcanic rock; mainly microcrystalline quartz (SiO₂) with iron oxides and other accessory minerals) — metamorphic
metamorphic

Tumbled orbicular jasper (likely ocean jasper)

Silicified volcanic rock; mainly microcrystalline quartz (SiO₂) with iron oxides and other accessory minerals

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; polished brown, orange, black, and gray patterning with opaque coloration and a waxy-to-glassy luster. It is cryptocrystalline, with no visible cleavage and typically conchoidal fracture.

Identified More metamorphic
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Physical properties

Hardness about 6.5–7 Mohs; polished brown, orange, black, and gray patterning with opaque coloration and a waxy-to-glassy luster. It is cryptocrystalline, with no visible cleavage and typically conchoidal fracture.

Formation & geological history

Jasper forms when silica-rich fluids replace or cement volcanic ash and rock, commonly with iron-oxide staining; ocean jasper formed in volcanic rocks of Madagascar, largely during the late Oligocene–Miocene. Exact identification requires locality or testing.

Uses & applications

Used for cabochons, beads, carvings, worry stones, and ornamental objects; it has modest lapidary value rather than gemstone-grade rarity.

Geological facts

Orbicular patterns result from concentric mineral growth or replacement around nuclei. The pictured elongated, polished specimen may also be another iron-rich jasper variety, since color alone cannot confirm ocean jasper.

Field identification & locations

Identify by its opaque multicolor silica-rich body, high polish, lack of cleavage, and ability to scratch glass; a steel file should not easily scratch it. Common sources include Madagascar, Australia, Brazil, India, and the western United States.