Rock Identifier
Crackled Quartz (Blue Dyed) (Silicon Dioxide (SiO2) with anthropogenic dye) — mineral
mineral

Crackled Quartz (Blue Dyed)

Silicon Dioxide (SiO2) with anthropogenic dye

Hardness: 7 (Mohs scale); Color: Neon or electric blue (concentrated in cracks); Luster: Vitreous; Crystal Structure: Trigonal (often appears as internal fractures); Cleavage: None; Specific Gravity: 2.65.

Hardness
7 (Mohs scale)
Color
Neon or electric blue (concentrated in cracks)
Luster
Vitreous
Identified More mineral

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Physical properties

Hardness: 7 (Mohs scale); Color: Neon or electric blue (concentrated in cracks); Luster: Vitreous; Crystal Structure: Trigonal (often appears as internal fractures); Cleavage: None; Specific Gravity: 2.65.

Formation & geological history

Created by heating natural clear quartz and then quenching it in cold liquid (dye). This 'thermal shock' causes internal fracturing while keeping the specimen intact. The dye then seeps into these internal cracks.

Uses & applications

Used primarily in costume jewelry, decorative home accents, tumbled stones, and 'healing crystal' collections.

Geological facts

Naturally occurring blue quartz exists, but it is typically a dull, grayish-blue. The vibrant, neon color seen in this specimen is a sure sign of human-made color enhancement. The internal network of tiny cracks gives it the name 'crackle quartz.'

Field identification & locations

Identify by looking at color distribution; the blue pigment is concentrated in spider-web patterned veins rather than being uniform throughout the body of the crystal. Commonly sold in gift shops and crystal boutiques.