Rock Identifier
Rutilated quartz beads (Quartz (SiO₂) with rutile (TiO₂) inclusions) — mineral
mineral

Rutilated quartz beads

Quartz (SiO₂) with rutile (TiO₂) inclusions

AI-generated identification · may be incorrect

Quartz has Mohs hardness 7, vitreous luster, and a trigonal crystal structure; the beads are transparent to translucent with dark needle-like inclusions. Bead cutting and reflections make precise identification of the inclusions uncertain.

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Physical properties

Quartz has Mohs hardness 7, vitreous luster, and a trigonal crystal structure; the beads are transparent to translucent with dark needle-like inclusions. Bead cutting and reflections make precise identification of the inclusions uncertain.

Formation & geological history

Quartz crystallized from silica-rich fluids or pegmatitic environments, with rutile needles trapped during growth; the specimens’ geological age and source cannot be determined from the image.

Uses & applications

Cut and polished as jewelry beads and collected as decorative quartz.

Geological facts

Rutile inclusions can form striking needle-like patterns, sometimes called “Venus hair” quartz.

Field identification & locations

Look for internal acicular inclusions rather than surface scratches; similar dark inclusions can be other minerals. Rutilated quartz occurs in places including Brazil, Madagascar, and India.