Rock Identifier
Orbicular jasper / brecciated jasper (Silica-rich microcrystalline quartz (chalcedony), commonly with iron oxides and altered volcanic fragments) — metamorphic
metamorphic

Orbicular jasper / brecciated jasper

Silica-rich microcrystalline quartz (chalcedony), commonly with iron oxides and altered volcanic fragments

AI-generated identification · may be incorrect

Typically hardness 6.5–7 Mohs, opaque, with black, tan, cream, and reddish-brown patches; dull to waxy luster and no visible cleavage. The specimen appears polished or naturally water-worn, with contrasting orbicular/brecciated textures.

Identified More metamorphic
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Physical properties

Typically hardness 6.5–7 Mohs, opaque, with black, tan, cream, and reddish-brown patches; dull to waxy luster and no visible cleavage. The specimen appears polished or naturally water-worn, with contrasting orbicular/brecciated textures.

Formation & geological history

Forms when silica-rich fluids replace or cement altered volcanic rock, producing jasper, breccia, and orb-like mineral patterns. Usually associated with ancient volcanic terrains, commonly Paleozoic to Mesozoic or older depending on locality.

Uses & applications

Used as ornamental stone, cabochons, carvings, polished slabs, and lapidary collectibles; too variable and fractured for most construction use.

Geological facts

The black areas may be magnetite, manganese oxides, or dark silica, while cream and brown zones commonly contain quartz, clay minerals, and iron oxides. Exact identification requires a fresh surface, hardness testing, and ideally petrographic or chemical analysis.

Field identification & locations

Look for opaque cryptocrystalline silica, conchoidal fracture, and a quartz-like hardness that resists a steel knife. Similar material occurs in volcanic regions worldwide, including Oregon, California, Mexico, Madagascar, and Australia.