
Deep beneath our feet lies Earth's molten heart. It is almost entirely made of iron. This metal generates the planet's magnetic field, shielding us from deadly cosmic radiation. Without iron at the core, life on Earth would never have survived.
But iron matters far beyond geology. Every red blood cell carries hemoglobin — a protein built around iron atoms. It grabs oxygen in your lungs and delivers it to every cell. Each breath you take works because of iron. And from this same metal we make steel — the backbone of modern civilization.
Humans have used iron for over 3,000 years. The Iron Age transformed warfare, farming, and construction. Today, iron alloys account for about 90% of all metal produced worldwide. Steel and cast iron are everywhere: in skyscrapers, bridges, ships, and cars.
The world produces over 1.8 billion tons of steel each year. China, India, and Japan lead production. Iron ore reserves are massive — Australia, Brazil, and Ukraine hold some of the largest deposits on the planet.
Metallic iron is safe to touch and non-toxic. However, fine iron dust is flammable and can explode in enclosed spaces. Rust (iron oxide) itself is harmless, but rusty surfaces often harbor bacteria, including the tetanus pathogen. Excess iron in the body (hemochromatosis) can damage the liver and heart. The recommended daily intake for adults is 8–18 mg.
Earth's core is about 85% iron. It forms a molten ball 2,440 km across — nearly the size of Mars.
An adult body contains 3–4 grams of iron. Enough for one small nail. But without it, blood could not carry oxygen.
Iron is the last element forged inside living stars. To create anything heavier, a star must explode as a supernova.
Ancient Egyptians called iron 'metal from the sky.' The earliest iron tools were hammered from meteorites, long before smelting was invented.
Only three metals can be permanently magnetized: iron, cobalt, and nickel. That's why magnets stick to your fridge door.
The world produces over 1.8 billion tons of steel every year. That's more than 90% of all metal made by humans.
| Isotope | Mass (u) | Abundance | Half-life | Decay |
|---|---|---|---|---|
54Fe | 53.939611 | 5.84% | stable | — |
56Fe | 55.934937 | 91.75% | stable | — |
57Fe | 56.935394 | 2.12% | stable | — |
58Fe | 57.933276 | 0.28% | stable | — |
Known since antiquity