Rock Identifier
Chevron Amethyst (Silicon Dioxide (SiO2) with iron impurities) — mineral
mineral

Chevron Amethyst

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 on Mohs scale; Color: V-shaped bands of purple and white; Luster: Vitreous; Crystal Structure: Hexagonal (Trigonal); Cleavage: None; Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
V-shaped bands of purple and white
Luster
Vitreous
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: V-shaped bands of purple and white; Luster: Vitreous; Crystal Structure: Hexagonal (Trigonal); Cleavage: None; Specific Gravity: 2.65

Formation & geological history

Formed in hydrothermal veins and cavities of volcanic rocks. The 'Chevron' pattern occurs when bands of amethyst and white quartz grow in alternating cycles. Most specimens date from the Cretaceous to Cenozoic eras.

Uses & applications

Used primarily in jewelry, lapidary arts for tumbled stones and carvings, and widely collected as a healing or decorative crystal.

Geological facts

Chevron Amethyst is one of the strongest 'Third Eye' stones in metaphysical belief. It is a combination of amethyst and white quartz, creating a distinct 'V' or 'zigzag' pattern.

Field identification & locations

Identify by the characteristic white 'V' shaped bands of quartz against a dark purple background. Common locations include Brazil, Bolivia, Africa, and India.