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In addition to the stable isotopes, there have been 21 radioactive isotopes of titanium identified. The most stable of these is 44 Ti, with a half life of 60 years. 45 Ti, 51 Ti and 52 Ti are the only other isotopes with a half life of longer than a minute.
Titanium is the fourth most abundant metallic element in the earth's crust. It occurs chiefly as an oxide ore. The commercially important forms are rutile (titanium dioxide) and ilmeite (titanium-iron oxide), the former being richest in titanium content. Metallic titanium was first isolated in impure form in 1887 and with higher purity in 1910.