
mineral
Tourmalinated Quartz
Silicon dioxide (SiO2) with inclusions of Schorl (NaFe2+3Al6(Si6O18)(BO3)3(OH)3OH)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Clear to milky white with black needle-like inclusions; Luster: Vitreous; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Clear to milky white with black needle-like inclusions
- Luster
- Vitreous
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Physical properties
Hardness: 7 (Mohs scale); Color: Clear to milky white with black needle-like inclusions; Luster: Vitreous; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins and pegmatites when quartz and liquid tourmaline crystallize simultaneously or when tourmaline needles are enveloped by growing quartz crystals.
Uses & applications
Used primarily in lapidary arts, jewelry (cabochons and beads), and as a decorative display specimen for metaphysical enthusiasts.
Geological facts
The black needles are specifically the mineral Schorl, which is the most common form of tourmaline. While quartz is a silicate, tourmaline is a complex boro-silicate.
Field identification & locations
Identify by looking for distinct, needle-like black crystals trapped inside transparent or translucent quartz. Common sources include Brazil, Madagascar, 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