Rock Identifier
Smoky quartz and clear/white quartz bead necklace (Quartz, silicon dioxide (SiO₂); smoky variety colored by irradiation-related defects) — gemstone
gemstone

Smoky quartz and clear/white quartz bead necklace

Quartz, silicon dioxide (SiO₂); smoky variety colored by irradiation-related defects

AI-generated identification · may be incorrect

Beads show translucent gray-brown smoky quartz alternating with colorless to milky quartz. Quartz has Mohs hardness 7, vitreous luster, trigonal crystal structure, no cleavage, and specific gravity about 2.65; surfaces are polished and drilled.

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Physical properties

Beads show translucent gray-brown smoky quartz alternating with colorless to milky quartz. Quartz has Mohs hardness 7, vitreous luster, trigonal crystal structure, no cleavage, and specific gravity about 2.65; surfaces are polished and drilled.

Formation & geological history

Quartz crystallizes from silica-rich hydrothermal fluids and igneous pegmatites; smoky coloration develops through natural irradiation of aluminum-related defects. Quartz ranges from Precambrian to modern geological ages and occurs worldwide.

Uses & applications

Used for inexpensive jewelry, ornament, and collecting. This is a human-processed geological specimen, not a single natural rock.

Geological facts

Smoky quartz is typically brown, gray, or nearly black; heating can remove its color, while irradiation can sometimes create it. The pale beads may also include milky quartz or another pale quartz variety.

Field identification & locations

Identify quartz by its glassy luster, lack of cleavage, hardness, and inability to scratch it with a steel nail easily; smoky quartz is distinguished by its smoky translucent color. Common sources include Brazil, Madagascar, Switzerland, and the United States.