Mineral field guide

How to identify staurolite

Staurolite is a brown to reddish-brown metamorphic mineral known for prismatic crystals and distinctive cross-shaped twins, with hardness near 7 to 7.5 and a pale streak.

mineralIron magnesium aluminum silicate hydroxide

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Reddish-brown cross-shaped twinned staurolite specimen displayed on a pale base
Cross-shaped twinned staurolite example; source image resized for web displayPhoto: 384 · CC BY-SA 4.0 · Wikimedia Commons
Classification

What is staurolite?

Staurolite is a complex iron-, magnesium-, and aluminum-bearing silicate hydroxide with variable substitutions. Its exact formula and composition can vary among specimens.

Appearance

What does staurolite look like?

Crystals are commonly stout prisms with rough surfaces and resinous to subvitreous luster. Penetration twins may form crosses intersecting near 60 or 90 degrees.

Untwinned crystals, broken grains, and matrix-bound porphyroblasts may lack the famous cross and resemble garnet, tourmaline, or dark metamorphic minerals.

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

Scratches glass and is not readily scratched by steel.

Habit

Stout prismatic crystals, commonly twinned

Cross twins are highly characteristic but not universal.

Cleavage

Poor

Broken surfaces are uneven rather than dominated by repeated cleavage.

Streak

White to grayish

Separates it from dark-streaking metallic minerals.

Comparison

Common lookalikes

Garnet

Usually equant with dodecahedral or rounded forms rather than prismatic cross twins.

Tourmaline

Commonly longer, strongly striated, and triangular in cross section.

Manufactured or carved cross

May show tool marks, unnatural symmetry, or lack a metamorphic matrix and crystal surfaces.

Geologic origin

How does it form?

Staurolite forms during medium-grade regional metamorphism of aluminum-rich sedimentary rocks.

It commonly occurs with mica, garnet, kyanite, quartz, and other index minerals used to interpret metamorphic conditions.

Where it occurs

Geologic setting and occurrence

Staurolite is characteristic of selected metamorphic belts and occurs in schist and gneiss across parts of the Appalachians, New England, the southern Rocky Mountains, and other regions.

A cross-shaped object should be evaluated for natural crystal faces and lawful provenance rather than assumed to be a natural twin.

Human use

Uses and significance

Staurolite is chiefly a collector mineral and metamorphic indicator. Cross twins are sold as “fairy stones,” but commercial pieces may be altered, mounted, or manufactured.

Safety and limits

Field notes

  • Do not pry crystals from outcrops or damage protected sites.
  • Cross shape is strong evidence only when natural crystal texture is present.
  • Avoid destructive testing of complete twins.

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.