Rock Identifier
Dyed Crackle Quartz (Silicon Dioxide (SiO2) with synthetic dye) — mineral
mineral

Dyed Crackle Quartz

Silicon Dioxide (SiO2) with synthetic dye

Hardness: 7 (Mohs scale); Color: Hot pink/magenta (artificial); Luster: Vitreous/Glassy; Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Characterized by a 'shattered' interior appearance with dye concentrated in the fissures.

Hardness
7 (Mohs scale)
Color
Hot pink/magenta (artificial)
Luster
Vitreous/Glassy
Identified More mineral

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Physical properties

Hardness: 7 (Mohs scale); Color: Hot pink/magenta (artificial); Luster: Vitreous/Glassy; Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Characterized by a 'shattered' interior appearance with dye concentrated in the fissures.

Formation & geological history

Formed through 'quench-crackling': natural clear quartz is heated to high temperatures and then rapidly cooled in a cold liquid dye solution. The thermal shock causes the mineral to fracture internally, allowing the dye to penetrate the cracks.

Uses & applications

Used primarily for decorative purposes, low-cost jewelry (beads, pendants), chakras/metaphysical healing practices, and as 'pocket stones' for children or amateur collectors.

Geological facts

Natural quartz of this specific neon magenta color does not exist in nature; any quartz with this level of internal fracturing and intense, uniform pink saturation along crack lines is man-made. It is often mislabeled as 'Pink Amethyst' or 'Rose Quartz' by unscrupulous sellers.

Field identification & locations

Identify in the field/market by looking for 'spider-web' fracture patterns where the color is darker in the cracks than in the solid parts of the stone. Natural rose quartz is usually cloudy and uniform, whereas this is transparent with internal crazing. Found in gift shops worldwide.