Magnetite is a mineral and one of the main iron ores, with the chemical formula Fe2+Fe3+2O4. It is one of the oxides of iron, and is ferrimagnetic; it is attracted to a magnet and can be magnetized to become a permanent magnet itself. With the exception of extremely rare native iron deposits, it is the most magnetic of all the naturally occurring minerals on Earth. Naturally magnetized pieces of magnetite, called lodestone, will attract small pieces of iron, which is how ancient peoples first discovered the property of magnetism.
Magnetite is one of the very few minerals that is ferrimagnetic; it is attracted by a magnet as shown here
Magnetite and other heavy minerals (dark) in a quartz beach sand (Chennai, India).
Octahedral crystals of magnetite up to 1.8 cm across, on cream colored feldspar crystals, locality: Cerro Huañaquino, Potosí Department, Bolivia
Telluric iron, also called native iron, is iron that originated on Earth, and is found in a metallic form rather than as an ore. Telluric iron is extremely rare, with only one known major deposit in the world, located in Greenland.
Sawed slab of basalt with bright, metallic native-iron inclusions from Uivfaq, Disko Island (specimen size: 7.8 cm × 3.5 cm × 0.6 cm (3.07 in × 1.38 in × 0.24 in))
Hand-sized sample of native iron from Disko Island, Greenland
Native iron from basalt quarry at Bühl, Weimar, district of Kassel, Germany (size: 6.6 × 5.9 × 1.8 cm)