Mineral field guide

How to identify pyrite

Pyrite is a brassy iron sulfide commonly called fool’s gold; it is harder and more brittle than gold, produces a dark streak, and often forms striated cubes.

mineralSulfide mineral · FeS₂

Download LithoMapPut U.S. geology in your pocket.Choose Google Play or the App Store.

Brassy metallic pyrite crystal specimen
Pyrite crystal specimen; source image resized and re-encoded for web displayPhoto: Didier Descouens · CC BY-SA 4.0 · Wikimedia Commons
Classification

What is pyrite?

Pyrite is iron disulfide. Trace elements can occur, but bright color does not establish precious-metal content.

Appearance

What does pyrite look like?

Fresh pyrite is bright metallic and pale brass-yellow. Tarnish may darken surfaces or produce iridescent films, while weathering can create rusty iron oxides and acidic sulfate products.

Crystals often form cubes with fine parallel striations on adjacent faces oriented in different directions. It also occurs as nodules, disseminated grains, or massive material.

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

6 to 6.5

Scratches glass and cannot be cut or flattened like native gold.

Streak

Greenish-black to brownish-black

Strongly different from gold’s yellow streak.

Tenacity

Brittle

Breaks or powders instead of bending or flattening.

Magnetism

Not strongly magnetic

Separates it from magnetite, though mixed samples complicate the test.

Comparison

Common lookalikes

Gold

Gold is much denser, malleable, softer, and leaves a yellow streak.

Chalcopyrite

Usually deeper yellow, softer, and commonly tarnishes iridescently without pyrite’s typical striated cubes.

Mica

Reflective flakes are nonmetallic, flexible, and much softer.

Geologic origin

How does it form?

Pyrite forms in hydrothermal veins, igneous and metamorphic rocks, and oxygen-poor sedimentary environments where iron and sulfur combine.

It can replace fossils or occur in coal and shale. Exposure to air and water promotes oxidation, which may generate acidity and iron staining.

Where it occurs

Geologic setting and occurrence

Pyrite is widespread in many rock types and ore deposits. Its presence is not proof of gold, silver, or an economic deposit.

Oxidized pyrite may be absent at the surface even where it remains below, leaving rusty gossan or sulfate minerals.

Human use

Uses and significance

Pyrite has historically supplied sulfur and sulfuric acid and remains important as an indicator mineral and source of environmental acidity in disturbed rock.

Safety and limits

Field notes

  • Wash hands after handling sulfide-rich material.
  • Do not heat or conduct chemical tests on pyrite outside a laboratory.
  • Mine waste can generate acidic drainage and contain hazardous metals; avoid disturbing it.

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.