
mineral
Chevron Amethyst
Quartz (SiO2) with patterned Amethyst and White Quartz/Milky Quartz
Hardness: 7 on Mohs scale. Color: Distinctive bands of deep purple (amethyst) and white or clear (quartz). Luster: Vitreous (glassy). Crystal structure: Trigonal. Cleavage: None. Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous (glassy)
Identified More mineral →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 7 on Mohs scale. Color: Distinctive bands of deep purple (amethyst) and white or clear (quartz). Luster: Vitreous (glassy). Crystal structure: Trigonal. Cleavage: None. Specific Gravity: 2.65.
Formation & geological history
Chevron Amethyst is a variety of quartz, specifically a combination of Amethyst and White Quartz (sometimes referred to as Milky Quartz). It forms hydrothermally in cavities within igneous rocks. The characteristic 'chevron' or 'banded' pattern arises from different phases of quartz growth and mineral deposition as the crystals form, often due to changes in fluid composition or temperature during crystallization. Geological age varies depending on the specific deposit, but quartz formations are common throughout Earth's history, from Precambrian to Cenozoic eras.
Uses & applications
Primarily used as an ornamental stone and for metaphysical purposes. It's often carved into spheres, tumbled stones, jewelry, and decorative objects. Its attractive banding makes it popular in lapidary arts. In crystal healing practices, it is believed to combine the stress-relieving qualities of amethyst with the purifying properties of quartz.
Geological facts
Chevron Amethyst is sometimes called 'Dog Tooth Amethyst' due to the V-shaped patterns resembling dog teeth in some formations. The purple color in amethyst is due to irradiation of iron impurities (Fe3+) within the crystal lattice. Heat treatment can change amethyst's color to yellow (citrine) or green (prasiolite), but this generally does not affect the white quartz bands in Chevron Amethyst. The finest specimens often come from Brazil and India.
Field identification & locations
To identify Chevron Amethyst in the field (or as a finished product), look for its distinctive banding of purple and white quartz. The 'chevron' pattern is key – a V-shaped or zigzag arrangement of the color bands, rather than parallel bands as seen in plain banded amethyst or agates. Its hardness (scratches glass) also helps confirm it's quartz. It's commonly found in areas rich in amethyst and quartz deposits, particularly in Brazil, India, and parts of Africa. For collectors, look for well-defined, contrasting bands and vibrant purple hues. Avoid pieces with significant cracks or dull coloration unless they offer other unique features.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral
Epidote
Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)
mineral