
mineral
Black Tourmaline
Schorl (Sodium Iron Aluminum Borosilicate Hydroxide), NaFe3Al6(BO3)3Si6O18(OH)4
Hardness: 7-7.5 on Mohs scale; Color: Jet black; Luster: Vitreous to sub-metallic; Crystal Structure: Trigonal (often long, striated columnar crystals); Cleavage: Indistinct; Specific Gravity: 3.0-3.2
- Hardness
- 7-7
- Color
- Jet black
- Luster
- Vitreous to sub-metallic
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Physical properties
Hardness: 7-7.5 on Mohs scale; Color: Jet black; Luster: Vitreous to sub-metallic; Crystal Structure: Trigonal (often long, striated columnar crystals); Cleavage: Indistinct; Specific Gravity: 3.0-3.2
Formation & geological history
Formed in granitic pegmatites, hydrothermal veins, and metamorphic rocks such as schists. They are common in late-stage igneous environments where boron is concentrated. Found in geological formations ranging from Precambrian to recent periods.
Uses & applications
Extensively used in jewelry (tumbled or faceted), metaphysical or 'healing' crystals, and industrial applications due to its piezoelectric properties (used in pressure gauges and optical instruments).
Geological facts
Black tourmaline is piezoelectric, meaning it can generate an electrical charge when mechanically stressed. It is the most common member of the tourmaline group, accounting for 95% of all tourmaline in nature. In Victorian times, it was frequently used as mourning jewelry.
Field identification & locations
Identify in the field by its deep black color, high hardness (cannot be scratched by steel), and characteristic longitudinal striations (parallel lines) along the crystal faces. Common locations include Brazil, Namibia, Madagascar, and San Diego County, USA.
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