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Present is the Key to the Past

The present is the key to the past

The present is the key to the past

  • Exhibition Text

    • This is a statement of the uniformitarian principle. Deceptively simple but enormously powerful, it means that the processes of occurring today have operated throughout most of the Earth’s history. For example, an ancient sandstone formed exactly as a beach forms today- by the gradual buildup, over many years, of water-transported sands. The principle is one of the guiding rules for understanding rocks and landforms, reconstructing their histories, and estimating the time it took for them to form.

      First insights from layered rocks
      Two of the most fundamental geological principles were outlined by a Danish physician, Nicolaus Steno (1638-1686). Hiking the mountains of Tuscany, in Italy, Steno realized that sedimentary rocks must have initially been deposited in horizontal layers, and that younger beds lie atop older ones. A century later, James Hutton came to another important realization: veins are dikes, both bodies of one rock inside another, must be younger than the rocks they invaded. 

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  • For Educators

    • Topic: Earth Science

      Subtopic: Earth Formation/Evolution

      Keywords: Dikes (Geology), Earth (Planet)--History, Earth sciences--History, Geology, Hutton, James, 1726-1797, Landforms, Rocks, Sedimentary rocks, Steno, Nicolaus, 1638-1686, Stratiographic--Proterozoic

      Audience: General

In This Section

Dike in a granite

Dike in a granite

This rock is a granite that solidified between 350 and 320 million years ago.

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