Rock Identifier
Polished chrysoprase (likely) (Chalcedony, microcrystalline quartz (SiO₂), colored by nickel-bearing minerals) — mineral
mineral

Polished chrysoprase (likely)

Chalcedony, microcrystalline quartz (SiO₂), colored by nickel-bearing minerals

AI-generated identification · may be incorrect

A polished, blue-green to gray-green, waxy/lustrous cryptocrystalline quartz with dark brown-black dendritic or matrix-like inclusions; Mohs hardness 6.5–7, no visible cleavage, conchoidal fracture, and specific gravity about 2.6.…

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Physical properties

A polished, blue-green to gray-green, waxy/lustrous cryptocrystalline quartz with dark brown-black dendritic or matrix-like inclusions; Mohs hardness 6.5–7, no visible cleavage, conchoidal fracture, and specific gravity about 2.6. The blue-green coloration may also indicate chrysocolla-bearing chalcedony or turquoise matrix, so exact identification requires testing.

Formation & geological history

Forms when silica-rich fluids fill cavities and fractures, with nickel or copper minerals producing green-blue color; commonly associated with volcanic rocks and weathered ultramafic zones, generally formed during relatively recent hydrothermal or weathering episodes.

Uses & applications

Used for cabochons, beads, carvings, and ornamental polished stones; lower-grade material is primarily decorative or collectible.

Geological facts

Chrysoprase is the best-known green chalcedony variety, while blue-green material is often sold under trade names such as “chrysocolla chalcedony.” Color can fade with prolonged heat or sunlight.

Field identification & locations

Common sources include Australia, Brazil, Poland, Tanzania, and the United States. A glassy waxy luster, hardness near quartz, and lack of cleavage help distinguish it from softer turquoise or dyed stone; laboratory Raman/XRF testing is recommended.