Magnesium is the eighth most abundant element in the Earth's crust and is extracted from seawater, dolomite, and magnesite ore. It has a melting point of 650°C and boiling point of 1107°C. Traditionally, magnesium is produced through electrochemical processes where dolomite or magnesite ore is crushed, roasted, and reacted with seawater or magnesium chloride to produce molten magnesium chloride, which is then electrolyzed to separate magnesium metal. Magnesium is also extracted from salt brines through drying and electrolysis.