Rock Identifier
Likely polished leopard-skin jasper or brecciated jasper (Jasper, an opaque microcrystalline variety of quartz (SiO₂), with iron-oxide and other mineral inclusions; exact variety cannot be confirmed from the image alone) — sedimentary
sedimentary

Likely polished leopard-skin jasper or brecciated jasper

Jasper, an opaque microcrystalline variety of quartz (SiO₂), with iron-oxide and other mineral inclusions; exact variety cannot be confirmed from the image alone

AI-generated identification · may be incorrect

The specimen appears to be a polished, opaque, patterned siliceous stone with dark brown to black areas, tan-gray mottling, fine vein-like boundaries, and scattered reddish inclusions. Jasper is mainly cryptocrystalline quartz, typically hardness about 6.5–7 Mohs, vitreous to dull/waxy luster when polished, no visible…

Identified More sedimentary
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Physical properties

The specimen appears to be a polished, opaque, patterned siliceous stone with dark brown to black areas, tan-gray mottling, fine vein-like boundaries, and scattered reddish inclusions. Jasper is mainly cryptocrystalline quartz, typically hardness about 6.5–7 Mohs, vitreous to dull/waxy luster when polished, no visible cleavage, conchoidal fracture, and specific gravity around 2.5–2.9. The orange piece near the center may be a separate fragment or surface inclusion, so the image may show a polished slab or tabletop rather than a loose specimen.

Formation & geological history

Jasper forms when silica-rich groundwater replaces or cements volcanic ash, sediments, or preexisting rocks. Iron and manganese oxides produce red, brown, yellow, and black colors. Varieties marketed as leopard-skin, spotted, or brecciated jasper commonly formed in volcanic or sedimentary environments. Jasper has no single geological age; deposits range from ancient Precambrian rocks to younger volcanic and sedimentary formations.

Uses & applications

Used for ornamental slabs, cabochons, beads, carvings, bookends, tabletops, and decorative objects. It is popular with mineral collectors and lapidaries, though most commercial jasper is relatively inexpensive.

Geological facts

Jasper is an opaque form of chalcedony or microcrystalline quartz. Its patterns are caused by contrasting silica-rich zones, iron oxides, volcanic fragments, and brecciation. Trade names such as leopard-skin jasper are often descriptive rather than formally mineralogical and may be applied inconsistently.

Field identification & locations

In the field, jasper is usually opaque, dense, nonmetallic, and harder than ordinary glass or steel knife blades. A polished surface commonly shows a smooth waxy-to-glassy luster and may take a high polish. It generally does not fizz with dilute hydrochloric acid. The exact identification is uncertain because the photograph is a close-up with no scale, and similar patterns can occur in agate, rhyolite, orbicular jasper, or polished manufactured stone. Common sources include Oregon, California, Idaho, Utah, Arizona, Mexico, Madagascar, India, Brazil, and Australia.