Rock Identifier
Pink opal and dendritic agate bead bracelet/necklace (Common opal (hydrated amorphous silica, SiO₂·nH₂O) with dendritic agate/chalcedony (microcrystalline quartz, SiO₂)) — gemstone
gemstone

Pink opal and dendritic agate bead bracelet/necklace

Common opal (hydrated amorphous silica, SiO₂·nH₂O) with dendritic agate/chalcedony (microcrystalline quartz, SiO₂)

AI-generated identification · may be incorrect

Polished spherical beads, mostly pale pink opaque opal with gray-white chalcedony beads containing black manganese-oxide dendrites. Opal hardness is about 5.5–6.5 Mohs; chalcedony is 6.5–7, with vitreous-to-waxy luster and no cleavage.

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Physical properties

Polished spherical beads, mostly pale pink opaque opal with gray-white chalcedony beads containing black manganese-oxide dendrites. Opal hardness is about 5.5–6.5 Mohs; chalcedony is 6.5–7, with vitreous-to-waxy luster and no cleavage.

Formation & geological history

Opal forms when silica-rich groundwater deposits hydrated silica in cavities and fractures; chalcedony forms from microcrystalline silica, while dendrites develop from mineral-rich fluids. These are generally young, commonly Cenozoic deposits, often from Peru, Mexico, Madagascar, or Indonesia.

Uses & applications

Used primarily in jewelry and ornamental beads; pink opal is valued for its pastel color, while dendritic agate is prized for natural patterning.

Geological facts

The black branching markings are mineral dendrites, not fossils or biological inclusions. Opal may dehydrate, craze, or scratch more readily than quartz.

Field identification & locations

Identify by low-to-moderate hardness, opaque pastel pink color, waxy luster, and branching inclusions in the gray beads; avoid prolonged heat, chemicals, and ultrasonic cleaning.