When Nicolaus Steno discovered that the relative ages of rocks can be determined by examining the position of fossils in separate layers of soil, he coined a process called

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Nicolaus Steno's discovery led to the development of the field of stratigraphy, which involves studying the layers (or strata) of rocks to determine the relative ages of different deposits. By examining the position of fossils in these layers, scientists can determine the order in which different species lived and how they evolved over time. This technique is still used today to study the history of the Earth and the evolution of life on our planet.

When Nicolaus Steno Discovered That the Relative Ages of Rocks