Rock Identifier
Amethyst Elestial Quartz (Silicon Dioxide with inclusions (SiO2)) — mineral
mineral

Amethyst Elestial Quartz

Silicon Dioxide with inclusions (SiO2)

Hardness: 7 Mohs; Color: Pale to deep purple and white; Luster: Vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture.

Hardness
7 Mohs
Color
Pale to deep purple and white
Luster
Vitreous
Identified More mineral
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Physical properties

Hardness: 7 Mohs; Color: Pale to deep purple and white; Luster: Vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture.

Formation & geological history

Formed in hydrothermal veins or cavities (geodes) where silica-rich fluids crystallize. Elestial growth occurs when crystals grow rapidly under high-pressure conditions, often resulting in skeletal or stacked layers.

Uses & applications

Primarily used for metaphysical collecting, lapidary work, and crystal healing specimens. Smaller pieces are often used in jewelry or as pocket stones.

Geological facts

The purple color is caused by trace amounts of iron (Fe3+) that have been irradiated by natural gamma radiation from surrounding rock. Elestial Amethysts are also known as Jacare quartz due to their scale-like appearance.

Field identification & locations

Identified by its distinctive purple hue and the 'skeletal' or stepped crystal growth pattern. Common locations include Brazil, Uruguay, and Madagascar. Collectors look for clarity and deep color saturation.