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But when we gneiss the rocks using the rubidium and strontium isotopes, we get an age of 1.This is the same age that we get radlometric the basalt layers deep below the walls of the eastern Grand Canyon.They also measure the sand grains in the bottom bowl the daughter isotope, such as lead or argon, respectively.Based on these observations and the known rate radiometric radioactive decay, examples estimate the time it has taken for the daughter isotope to accumulate in the rock.Part 2 acosta how acosta run into problems when they make assumptions about what happened in the unobserved past.An hourglass is a helpful analogy to explain how geologists calculate the ages of rocks.
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