
mineral
Tourmalinated quartz
Quartz (SiO₂) with black tourmaline (schorl; NaFe²⁺₃Al₆(BO₃)₃Si₆O₁₈(OH)₄) inclusions
AI-generated identification · may be incorrectHardness: quartz 7, tourmaline 7–7.5 Mohs; transparent to translucent gray-brown quartz with vitreous luster and black, prismatic tourmaline crystals. Quartz is trigonal with no cleavage; tourmaline is trigonal and has poor cleavage.
- Hardness
- quartz 7, tourmaline 7–7
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Physical properties
Hardness: quartz 7, tourmaline 7–7.5 Mohs; transparent to translucent gray-brown quartz with vitreous luster and black, prismatic tourmaline crystals. Quartz is trigonal with no cleavage; tourmaline is trigonal and has poor cleavage.
Formation & geological history
Forms in hydrothermal quartz veins and granitic pegmatites when tourmaline grows inside quartz during late-stage cooling, commonly in the Mesozoic to Precambrian geologic record.
Uses & applications
Used as a decorative and lapidary material, especially in cabochons, polished slices, and collectible mineral specimens; transparent pieces may be set in jewelry.
Geological facts
The dark needles are typically schorl, the most common black tourmaline. Tourmaline is piezoelectric and can develop electrical charge when heated or compressed.
Field identification & locations
Identify it by glassy quartz enclosing sharply contrasting black, elongated tourmaline crystals; distinguish it from smoky quartz by the visible inclusions. Common sources include Brazil, Madagascar, Pakistan, Afghanistan, and the United States.
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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