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Mineral Species · Silicates

Schorl

黑电气石

NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄

Schorl (NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄) is the iron-rich end-member of the tourmaline group and by far the most abundant tourmaline species. Its jet-black trigonal prisms, often striated lengthwise, are common in granitic pegmatites and are the most familiar…

Crystal system

Trigonal

Hardness

7–7.5

Specific gravity

3.2

Schorl (NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄) is the iron-rich end-member of the tourmaline group and by far the most abundant tourmaline species. Its jet-black trigonal prisms, often striated lengthwise, are common in granitic pegmatites and are the most familiar collector form of tourmaline globally. While the colorful elbaite varieties (rubellite, indicolite, watermelon) capture gem markets, Schorl dominates specimen-grade tourmaline output by sheer volume.

Key Facts

  • Mohs hardness 7–7.5.
  • Trigonal symmetry; signature triangular cross-section visible at crystal terminations.
  • Strong vertical striations along the prism faces.
  • Black to brownish-black color from iron content.
  • Strongly piezoelectric and pyroelectric — develops electrical charge under pressure or heat.

Notable Localities

Erongo Mountains (Namibia) produce world-class Schorl on aquamarine. Pakistan and Brazil yield large prismatic specimens. China has minor presence in Xinjiang and Yunnan pegmatite zones.

Found at these Localities

Notable Localities

Where to find collector-grade Schorl.

Erongo Mountains

Namibia

Stak Nala

Pakistan

Minas Gerais

Brazil

Altai Mountains

Xinjiang

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