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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.
Pure titanium was first produced by Matthew A. Hunter, an American metallurgist, in 1910. Titanium is the ninth most abundant element in the earth's crust and is primarily found in the minerals rutile (TiO2), ilmenite (FeTiO3) and sphene (CaTiSiO5). Titanium makes up about 0.57% of the earth's crust. Titanium is a strong, light metal. It is as strong as steel and twice as strong as aluminum, but is 45% lighter than steel and only 60% heavier than aluminum.