How to identify Pyrite
Pyrite (Iron sulfide)
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Open the appTo correctly identify Pyrite (Pyrite (Iron sulfide)), 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
Brass-yellow to pale brass-yellow, sometimes with a slight greenish tint. Can tarnish to a duller, darker brassy color.
- 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 euhedral to subhedral crystals, granular aggregates, or massive forms. Crystal faces are often striated.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Commonly cubic, pyritohedral (12-faced pentagonal dodecahedron), or octahedral. Also found as massive, granular, reniform, or stalactitic aggregates. Penetration twins are common.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Poor to indistinct on {001}. Typically fractures rather than cleaves.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in igneous, metamorphic, and sedimentary rocks. Common in hydrothermal veins, disseminated in igneous intrusions, in black shales, coal seams, and as concretions in sedimentary rocks. Also found in massive sulfide deposits.
Key Facts
- Hardness
- 6-6.5 (Mohs scale)
- Specific Gravity
- 4.95-5.10 g/cm³
- Crystal System
- Isometric (Cubic)
- Color
- Pale brass-yellow to golden-yellow
- Luster
- Metallic
- Transparency
- Opaque
- Fracture
- Conchoidal to uneven
- Cleavage
- Poor to indistinct on {001}
- Composition
- Iron sulfide (FeS₂)
Physical characteristics
- Crystal Habit: Cubic, pyritohedral, octahedral, massive, granular, reniform, stalactitic. Striations often present on crystal faces.
- Cleavage Type: Poor/Indistinct
- Fracture Type: Conchoidal to uneven
- Tenacity: Brittle
- Luster Type: Metallic
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