Rock Identifier
Chalcedony (Common Opal or Agate variant) (Silicon Dioxide (SiO₂)) — mineral
mineral

Chalcedony (Common Opal or Agate variant)

Silicon Dioxide (SiO₂)

Hardness: 6.5-7 on Mohs scale; Color: Pinkish-purple, lavender, or bluish-grey with translucent waxy luster; Crystal structure: Microcrystalline/cryptocrystalline (trigonal); Cleavage: None; Fracture: Conchoidal (shell-like curves).

Hardness
6
Identified More mineral

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Physical properties

Hardness: 6.5-7 on Mohs scale; Color: Pinkish-purple, lavender, or bluish-grey with translucent waxy luster; Crystal structure: Microcrystalline/cryptocrystalline (trigonal); Cleavage: None; Fracture: Conchoidal (shell-like curves).

Formation & geological history

Formed by the precipitation of silica from groundwater in cavities of igneous rocks or sedimentary layers. Often associated with volcanic environments where hydrothermal fluids cool over thousands of years.

Uses & applications

Used primarily in lapidary arts for cabochons, carvings, and beads. Also valued as a metaphysical stone and by mineral collectors for its smooth texture and color palette.

Geological facts

Chalcedony was highly prized in the ancient world, particularly by the Greeks and Romans for seals and signet rings because hot wax does not stick to it. This specific specimen shows the characteristic waxy 'skin' of raw chalcedony nodules.

Field identification & locations

Identify in the field by its smooth, waxy surface and the absence of visible crystals. It is much harder than glass (it will scratch glass). Commonly found in the Western United States (Oregon, Arizona), Brazil, and Madagascar.