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The age of the earth has been arrived at, slowly and step by step, as scientists refine existing methods and discover new ones.

Charles Lyell is probably the pioneer who first proved that the Earth is millions of years old. Early in the nineteenth century, he examined the great volcano of Etna on Sicily and studied the historical records of frequent eruptions. He noticed that each time it erupted, a new layer of lava would be added, causing the mountain to grow at a measurable rate. By knowing the height of the volcano, its approximate rate of growth and the frequency of eruptions, Lyall determined that the volcano must be several hundred thousand years old. At the edge of the volcano, under the first lava flows, he found fossil shells that were virtually identical to the shells of molluscs still found in the Mediterranean Sea. From this, he deduced that the fossils were geologically recent, that a hundred thousand years was geologically short and that the age of the earth must be immense.

A further important step took place in 1862, when Lord Kelvin, Professor of Natural Philosophy at Glasgow University and regarded by his contemporaries as the greatest physicist of his day, announced that he had calculated the time it would take the world to cool down from its molten state. He calculated that this was between 20 and 400 million years. Later, Kelvin refined his calculations to within the range 20 to 100 million years and, later still, to some 20 to 40 million years. With the discovery of radioactivity, it was soon realised that the uranium present in the earth prolongs its cooling almost indefinitely. So. Kelvin's method only gives a minimum age, but by no means a true estimate.

Samuel Haughton, an Irish geologist, calculated that sediments were deposited on the ocean floor at the rate of "one foot in 8,616 years". He then calculated a minimum duration of around 2000 million years. Unwilling to accept such a long period, he scaled it back, by a factor of 10, to just 200 million years. This may not be an important dating method today, but it does lend confirmation to other dating methods.

These early estimates fell far short of the Earth's real age of more than 4.5 billion years, a figure more recently established by nuclear physicists, but they did show that it was no longer possible to consider the earth to be only a few thousand years old.

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