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The standard geologic time scale was devised according to relative time relationships observed in rocks across the world. Determining the actual ages of these time spans, and thus establishing the beginning and ending dates of geologic eons, eras, periods, and epochs, became possible with the discovery of radioactivity. Radioactive elements decay at known rates of speed. This radioactive decay begins after the elements are locked into crystalline mineral structures. Some elements have variations called isotopes , which are atoms that contain different numbers of neutrons in their nuclei.