Science & technology

James Hutton presents his Theory of the Earth

1788

In 1785 the Scottish farmer-geologist James Hutton read a paper to the Royal Society of Edinburgh and published his Theory of the Earth in 1788, arguing that the planet's rocks are formed by slow processes still in operation today: erosion, deposition, burial, heat and uplift. At Siccar Point on the Scottish coast in 1788 he, with John Playfair and James Hall, saw tilted layers of older rock capped by flat younger ones, showing endless cycles. He saw 'no vestige of a beginning, no prospect of an end'. The idea of deep time prepared the ground for Lyell and Darwin.

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This moment belongs to the Industrial era (1760 CE to 1914 CE), steam, factories and revolutions. You can also browse everything in the 18th century.