Mineral field guide

How to identify tourmaline

Tourmaline is a diverse borosilicate mineral group commonly recognized by hard, strongly lengthwise-striated prismatic crystals with triangular to rounded-triangular cross sections.

mineralComplex borosilicate mineral group

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Dark prismatic tourmaline specimen about eight centimeters tall from Minas Gerais, Brazil
Dark prismatic tourmaline specimenPhoto: Mike Davis · CC0 1.0 · Wikimedia Commons
Classification

What is tourmaline?

Tourmaline is a chemically complex mineral group containing boron with varying sodium, calcium, lithium, magnesium, iron, aluminum, and other elements. Species such as schorl, elbaite, and dravite cannot be assigned reliably from color alone.

Appearance

What does tourmaline look like?

Tourmaline commonly forms elongated prisms with deep parallel grooves. Cross sections are often three-sided or six-sided in a way that reflects trigonal symmetry, and crystal ends may differ from one another.

Black schorl is widespread; gem tourmalines may be transparent and color-zoned. Massive, radiating, acicular, or fibrous aggregates also occur.

Field tests

Identification tests

Begin with observation and use the least destructive test first. Results can change with weathering, mixtures, coatings, and grain size. Review the step-by-step field-test methods before altering an unfamiliar specimen.

Hardness

About 7 to 7.5

Typically scratches glass and resists a steel point.

Cleavage

Poor or indistinct

Breaks irregularly rather than into repeated flat cleavage fragments.

Habit

Strongly striated trigonal prisms

The combination of grooves and triangular cross section is highly useful.

Streak

White

Not usually diagnostic.

Comparison

Common lookalikes

Hornblende

Softer, has two good cleavage directions near 60 and 120 degrees, and commonly forms splintery amphibole prisms.

Beryl

Forms true hexagonal prisms, often with flatter faces and a hexagonal rather than triangular cross section.

Garnet

Commonly equant with dodecahedral forms rather than long striated prisms.

Geologic origin

How does it form?

Tourmaline crystallizes in granitic pegmatites, hydrothermal veins, and metamorphic rocks and can survive weathering into sediment.

Its composition records aspects of the fluids and rocks in which it grew, but chemical analysis is needed for precise species and provenance.

Where it occurs

Geologic setting and occurrence

Tourmaline is widespread in pegmatites and metamorphic rocks and can occur as accessory grains in granite, schist, and stream sediment.

Black prismatic material in pegmatite is often schorl, but species assignment and gem identification require more than color and setting.

Human use

Uses and significance

Transparent colored tourmaline is used as a gemstone; black and opaque material is chiefly collected or studied. Tourmaline also has scientific value as a durable recorder of geologic fluids and conditions.

Safety and limits

Field notes

  • Inspect cross section and striations before using color.
  • Do not break a crystal merely to test cleavage or interior color.
  • Gem quality, treatment, and species require professional testing.

This guide supports preliminary field identification, not a laboratory determination, appraisal, hazard assessment, or statement of ownership or collecting permission. Verify land status and local rules before handling or collecting material.

Source basis

Authoritative sources

LithoMap wrote this guide in original language using the scientific concepts and physical-property standards supported by these sources.

Editorial review: September 17, 2026.