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The solution is: where is the half-life of the element, is the time expired since the sample contained the initial number atoms of the nuclide, and is the remaining amount of the nuclide.We can measure directly, for example by using a radiation detector, and obtain a good estimate of by analyzing the chemical composition of the sample.Even though the decay of 40 K is somewhat complex with the decay to 40 Ca and three pathways to 40 Ar, Dalrymple and Lanphere point out that potassium-argon dating was being used to address significant geological problems by the mid 's. The foreign material itself could date over 1 billion years old!Many pieces of glass ejecta had been found on Haiti, which is over a thousand miles from the impact point currently.As the K in the rock decays into Ar, the gas is trapped in the rock.

Catastrophism in the Pacific Northwest: Is the prevalent view held by the majority of scientists the only plausible way of approaching the problems of time?Chicxulub was not so obvious as a candidate because much of the evidence for it was under the sea.The details are best pursued in a dedicated text like Mc Dougall and Harrison.Doing simple calculations it is easy to see that if the experiment was done again, but with only 2 atmospheres of Argon, that normal amounts of Argon would be forced into the rock. Research in Hawaii shows that the lava flows on the surface of the ground are able to loose essentially all of the Argon.Although the time at which any individual atom will decay cannot be forecast, the time in which any given percentage of a sample will decay can be calculated to varying degrees of accuracy.

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