Pyrite, a complex sulfide mineral, holds a special place in nature for its unique properties and appearance. Its primary component is FeS, a compound of iron and sulfur. It has a light brass-colored appearance, often covered with a yellowish-brown hue, and shimmers with a metallic sheen. Its hardness ranges from 6 to 6.5, making it one of the most widely distributed sulfides in the Earth's crust.
Pyrite has an isometric crystal structure and a variety of morphologies, with cubes, octahedra, and pentagonal dodecahedrons being common. Three distinct sets of perpendicular striations are visible on the crystal faces, occasionally forming intersecting twins, adding to its unique beauty. Its aggregates often take the form of granules, dense blocks, spheres, or strawberry shapes, with a variety of shapes.
It is worth noting that pyrite is called "pyr" in Greek, meaning fire, due to the brilliant sparks it produces when struck, which can even be used to start fires. However, it also has a well-known nickname: "fool's gold." Despite having the word "gold" in its name, pyrite is very different from real gold in properties and value.