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The elevation of the rock. Decay rates are given by the decay constants of the nuclides.
The depth from which we take the sample. Chlorine nuclides are Cosmogeinc measured to date surface rocks. The production rate for a particular nuclide is a function of geomagnetic latitude, the amount of sky that can be seen from the point that is sampled, elevation, sample depth, and density of the material in which the sample is embedded. In practice, we are not going to be able to tell the difference between a rock which has reached