
mineral
Green Tourmaline
Elbaite (Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)4)
AI-generated identification · may be incorrectHardness: 7-7.5 on Mohs scale; Color: Bottle green to olive green; Luster: Vitreous (glassy); Crystal Structure: Trigonal (often found as prismatic crystals with vertical striations); Cleavage: Indistinct; Specific Gravity: 3.0-3.3
- Hardness
- 7-7
- Color
- Bottle green to olive green
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7-7.5 on Mohs scale; Color: Bottle green to olive green; Luster: Vitreous (glassy); Crystal Structure: Trigonal (often found as prismatic crystals with vertical striations); Cleavage: Indistinct; Specific Gravity: 3.0-3.3
Formation & geological history
Formed in granitic pegmatites and metamorphic rocks through hydrothermal processes where boron-rich fluids are present. Generally formed during the late stages of magma crystallization.
Uses & applications
Used primarily as a gemstone in jewelry, as mineral specimens for collectors, and historically in some pressure-sensitive gauges due to its piezoelectric properties.
Geological facts
Tourmaline is unique because it is pyroelectric, meaning it can generate an electrical charge when heated. Large, gem-quality green tourmaline is often called 'Verdelite' in the jewelry trade.
Field identification & locations
Identify in the field by looking for triangular cross-sections and distinct vertical striations on crystal faces. Commonly found in Brazil, Afghanistan, Pakistan, and parts of Africa.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous