
mineral
Green Tourmaline
Verdelite (Silicate mineral); Na(Li,Al)3Al6(BO3)3Si6O18(OH)4
Hardness: 7-7.5 on the Mohs scale. Color: Pale green to forest green. Luster: Vitreous (glassy). Crystal structure: Trigonal/Hexagonal elongated prisms with vertical striations. Cleavage: Indistinct. Specific gravity: 3.06.
- Hardness
- 7-7
- Color
- Pale green to forest green
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7-7.5 on the Mohs scale. Color: Pale green to forest green. Luster: Vitreous (glassy). Crystal structure: Trigonal/Hexagonal elongated prisms with vertical striations. Cleavage: Indistinct. Specific gravity: 3.06.
Formation & geological history
Formed in granitic pegmatites and metamorphic rocks like schist and marble through hydrothermal processes. Most specimens date from the Phanerozoic eon down to recent geological eras, depending on the host rock formation.
Uses & applications
Used primarily in high-end jewelry as a gemstone, as a specimen for mineral collectors, and historically in scientific instruments due to its piezoelectric properties.
Geological facts
Green tourmaline is often called 'Verdelite'. It is unique because it is pleochroic, meaning it can show different shades of color when viewed from different angles. It also possesses pyroelectricity, becoming electrically charged when heated.
Field identification & locations
Identify in the field by its long, columnar crystal habit and the presence of fine parallel ridges (striations) along the length of the crystal. Commonly found in Brazil, Afghanistan, Pakistan, and Maine/California in the USA.
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