Simple scientific technique that geologists like Hutton, Steno, and Lyell use to draw fundamental geologic conclusions is Comparing ancient rocks/fossils to modern counterparts .
According to the uniformitarian concept, the past can be understood through the present. The science of geology has been greatly impacted by this idea.
James Hutton co-created the idea of uniformitarianism with Charles Lyell. He thought that progressive processes over a long period of time generated Earth's landforms, such as the mountains and oceans.
Grasp Earth's past requires an understanding of the uniformitarian principle. Lyell thought Hutton was right regarding the mechanisms gradually altering that shape the Earth's surface. In looking at rocks and sediments, he discovered his own examples of these processes.
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