
mineral
Dyed Crackle Quartz
Silicon Dioxide (SiO2) with synthetic dye
AI-generated identification · may be incorrectHardness: 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
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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.
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