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The oldest nuclear fission reactor on Earth formed naturally in West Africa about two billion years ago, where groundwater enabled atoms in uranium deposits to split, releasing energy.

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In modern nuclear power plants, water acts as a moderator that slows down high-energy neutrons released by uranium, allowing them to collide with other uranium atoms, inducing further splitting and a sustained release of energy.
Scientists hypothesize that there were more than a dozen natural nuclear fission reactors in a mine near Oklo, Gabon, identified by comparing the concentrations of radioactive uranium isotopes in underground deposits at the site with those found elsewhere on Earth.
The Oklo reactors are thought to have naturally operated in cycles lasting from hours to months, in which groundwater seeping into uranium deposits facilitated the reactions until it boiled away due to the energy produced, with the largest able to power a car's engine.
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