Loading [MathJax]/jax/output/HTML-CSS/jax.js
Skip to main content
Library homepage
 

Text Color

Text Size

 

Margin Size

 

Font Type

Enable Dyslexic Font
Geosciences LibreTexts

16.57: Pyrite

( \newcommand{\kernel}{\mathrm{null}\,}\)

Pyrite
Chemical composition FeS2
Crystal system Cubic
Habit Cubic, faces may be striated, but also frequently octahedral and pyritohedron. Often inter-grown, massive, radiated, granular, globular and stalactitic.
Cleavage Indistinct on {001}; partings on {011} and {111}
Fracture Very uneven, sometimes conchoidal
Hardness 6–6.5
Refractive index a = 1.730; b = 1.758; y = 1.838
Specific gravity 4.8-4.9
Lustre Metallic

Figure 16.57.1: Victorian Pyrite-set Lizard Pins
Photo courtesy of Barbra Voltaire

Marcasite is a misnomer, referring to the mineral pyrite when it is faceted into small reflective stones and used in jewelry. Marcasite and pyrite are both iron disulfides but they are different minerals because they crystallize in different systems and form under different geologic conditions. Marcasite isn't suitable for use in jewelry because it is unstable and can decompose in the air, appearing to acquire a chalky coating. Pyrite is named after the Greek word for fire as it produces sparks when struck by iron.

File:Pyrite xls.jpg

Figure 16.57.2: Pyrite Crystals, Spain
Photo courtesy of Barbra Voltaire

Pyrite crystallizes in the cubic system and can form perfect cubes with shiny metallic gold faces.
Native Americans believed that pyrite "mirrors" allowed you to see inside the soul.


16.57: Pyrite is shared under a CC BY-NC-SA license and was authored, remixed, and/or curated by LibreTexts.

Support Center

How can we help?