
mineral
Pink Tourmaline (Rubellite)
Rb:Na(Li,Al)3Al6(BO3)3Si6O18(OH)4 (Elbaite variety)
AI-generated identification · may be incorrectHardness: 7-7.5 on Mohs scale; Color: Pink to deep reddish-pink; Luster: Vitreous (glassy); Crystal Structure: Trilateral (hexagonal); Cleavage: Indistinct; Specific Gravity: 3.0-3.3
- Hardness
- 7-7
- Color
- Pink to deep reddish-pink
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7-7.5 on Mohs scale; Color: Pink to deep reddish-pink; Luster: Vitreous (glassy); Crystal Structure: Trilateral (hexagonal); Cleavage: Indistinct; Specific Gravity: 3.0-3.3
Formation & geological history
Formed in granitic pegmatites through hydrothermal activity. Mineral-rich fluids crystallize in cavities over millions of years, often associated with the late stages of igneous cooling.
Uses & applications
Primarily used as a gemstone in high-end jewelry (faceting or cabochon); also highly valued as mineral specimens for collectors due to its vibrant color and crystal habits.
Geological facts
Tourmaline is unique for its pyroelectric and piezoelectric properties, meaning it can generate an electrical charge when heated or compressed. The deep pink variety called Rubellite is one of the most sought-after colors.
Field identification & locations
Identify by its characteristic vertical striations along the crystal faces and its 'three-sided' rounded triangular cross-section. Commonly found in Brazil, Madagascar, Afghanistan, and the United States (Maine/California).
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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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary