Polymetallic nodules (manganese nodules) are metal-rich nodules found on the seabed of Earth's oceans. They are 5-10cm in diameter and found at depths of 4000-5000m. It is believed they are formed by the chemical precipitation of metals around small objects, such as the shells of marine organisms. These nodules contain around 30% manganese, with smaller amounts of iron, nickel, copper, cobalt and titanium.