Rock Identifier
Polished jasper or jasper-rich breccia (Microcrystalline quartz (SiO₂), commonly with iron oxides and other silicates) — metamorphic
metamorphic

Polished jasper or jasper-rich breccia

Microcrystalline quartz (SiO₂), commonly with iron oxides and other silicates

AI-generated identification · may be incorrect

Opaque, polished, dark brown-black with rusty orange and blue-green patches; vitreous to waxy luster, cryptocrystalline structure, no visible cleavage, Mohs hardness about 6.5–7, specific gravity roughly 2.5–2.7.

Identified More metamorphic
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Physical properties

Opaque, polished, dark brown-black with rusty orange and blue-green patches; vitreous to waxy luster, cryptocrystalline structure, no visible cleavage, Mohs hardness about 6.5–7, specific gravity roughly 2.5–2.7.

Formation & geological history

Jasper forms when silica-rich groundwater replaces or cements volcanic ash, sediments, or brecciated rock; iron and copper-bearing impurities create the vivid colors. Its exact geological age cannot be determined from the photograph and depends on its locality.

Uses & applications

Commonly cut and tumbled for jewelry, cabochons, ornaments, and collectibles; occasionally used as decorative stone. Small polished pieces generally have modest commercial value.

Geological facts

The blue-green areas may indicate chrysocolla, chlorite, or other mineral inclusions, so a precise variety cannot be confirmed visually. The specimen appears human-polished rather than naturally weathered.

Field identification & locations

Identify by its opaque fine-grained texture, strong polish, hardness, and irregular multicolor pattern; it will not show transparent quartz crystals. Common sources include India, Madagascar, Australia, Brazil, and the western United States.