How to identify Pyrite
Iron Pyrite (FeS2)
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Open the appTo correctly identify Pyrite (Iron Pyrite (FeS2)), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Pale brass-yellow to golden-yellow, often with a tarnished or iridescent surface.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Distinctive metallic luster, very bright and reflective.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically forms well-defined crystals; granular or massive aggregates are also common.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Cubes, octahedra, and pyritohedra are characteristic. Cube faces often show striations perpendicular to adjacent faces. Can also be massive, reniform, globular, or stalactitic.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Poor to indistinct cleavage on {100}. Typically fractures conchoidally or unevenly.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in igneous rocks (as an accessory mineral), metamorphic rocks (e.g., schists, gneisses), and sedimentary rocks (especially black shales, coal seams, and limestones). Common in hydrothermal veins, contact metamorphic deposits, and as concretions.
Key Facts
- Hardness
- 6-6.5 (Mohs scale)
- Specific Gravity
- 4.95-5.10 g/cm³
- Crystal System
- Isometric (Cubic)
- Color
- Pale brass-yellow, golden-yellow
- Luster
- Metallic
- Transparency
- Opaque
- Fracture
- Conchoidal to uneven
- Cleavage
- Poor to indistinct on {100}
- Composition
- Iron sulfide (FeS2)
Physical characteristics
- Crystal Habit: Cubic, octahedral, pyritohedral, massive, granular, reniform, globular, stalactitic. Cube faces often striated.
- Cleavage Type: Poor/Indistinct
- Fracture Type: Conchoidal to uneven
- Tenacity: Brittle
- Luster Type: Metallic
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