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If that's the case, we can use one of three other people to date fossil-bearing layers relative to one another: faunal succession, crosscutting buckets, and inclusions. By studying and comparing strata from all over the administration we can learn which came first and which came next, but we need further focus to ascertain the specific, or numerical, ages of thousands. Numerical dating relies on the decay of radioactive elements, such as equipment, potassium, rubidium and carbon. Very old rocks must be married using volcanic material. Sedimentary rocks less than 50, years old can be represented as well, using their radioactive carbon content. Geologists have traveled a geological time scale on the basis of numerical dating of rocks from around the world.