How to identify Pyrite
Pyrite (FeS2)
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Open the appTo correctly identify Pyrite (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
Brassy yellow to golden yellow, sometimes with a tarnished, iridescent sheen.
- 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 with smooth, often striated faces. Massive forms can be granular or botryoidal.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Commonly forms cubes, octahedra, and pyritohedra (a 12-faced form). Striations are often visible on cubic faces, running perpendicular to each other. Also found as massive, granular, radiating, or botryoidal aggregates.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Poor to indistinct cleavage, typically exhibiting conchoidal to uneven fracture rather than true cleavage.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in igneous, metamorphic, and sedimentary rocks. Common in hydrothermal veins, contact metamorphic deposits, black shales, coal seams, and as concretions in sedimentary rocks. Often associated with other sulfide minerals, quartz, and carbonates.
Key Facts
- Hardness
- 6-6.5 (Mohs scale)
- Specific Gravity
- 4.95-5.02 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, radiating, botryoidal. Often striated on cube faces.
- Cleavage Type: Poor/Indistinct
- Fracture Type: Conchoidal to uneven
- Tenacity: Brittle
- Luster Type: Metallic
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