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Colorado River near Nankoweap Creek. Grand Canyon National Park, Arizona.

The Present is the Key to the Past

Many geologists consider James Hutton (1726-1797) to be the father of historical geology. Hutton observed such processes as wave action, erosion by running water, and sediment transport and concluded that given enough time these processes could account for the geologic features in his native Scotland. He thought that "the past history of our globe must be explained by what can be seen to be happening now." This assumption that present-day processes have operated throughout geologic time was the basis for the principle of uniformitarianism.

Before Hutton, no one had effectively demonstrated that geologic processes occurred over long periods of time. Hutton persuasively argued that seemingly weak, slow-acting processes could, over long spans of time, produce effects that were just as great as those resulting from sudden catastrophic events. And, unlike his predecessors, Hutton cited verifiable observations to support his ideas.

Although Hutton developed a comprehensive theory of uniformitarian geology, Charles Lyell (1797-1875) became its principal advocate. Lyell was successful in interpreting and publicizing uniformitarianism for society at large. Hutton's idea of uniformitarianism (and his cumbersome and difficult literary style) had simply failed to capture the imagination of his generation, so geologists often credit Lyell with advancing the basic principles of modern geology. Lyell's Principles of Geology is a landmark text in the history of science and as important to modern world views as the works of Charles Darwin. In 1990 the University of Chicago Press republished his works. In the first of three volumes, Charles Lyell sets forth the uniformitarian argument: processes now visibly acting in the natural world are essentially the same as those that have acted throughout the history of the Earth, and are sufficient to account for all geologic phenomena.

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Many geologists consider James Hutton (1726-1797) to be the father of historical geology. Hutton observed such processes as wave action, erosion by running water, and sediment transport and concluded that given enough time these processes could account for the geologic features in his native Scotland.

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Relative vs. absolute dating SUPER MINI review

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Relative vs. absolute dating SUPER MINI review

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Easily create beautiful interactive video lessons for your students you can integrate right into your LMS. Track students' progress with hassle-free analytics as you flip your classroom!

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Radioactive dating goes hand in hand with absolute dating.

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Easily create beautiful interactive video lessons for your students you can integrate right into your LMS. Track students' progress with hassle-free analytics as you flip your classroom!

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Radioactive dating and absolute dating go hand in hand. Watch this video to find out why.

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Easily create beautiful interactive video lessons for your students you can integrate right into your LMS. Track students' progress with hassle-free analytics as you flip your classroom!

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This is reading about the processes used to determine the age of fossils. 
->uniformitarianism introduced
->relative rock layers
   - law of superposition
-> Geologic columns
-> Absolute age of rocks
   - radioactive decay
   -  half-life
-> Radiometric dating
-> index fossils

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Studying the Age of Fossils introduction

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Studying the Age of Fossils introduction

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This is reading about the processes used to determine the age of fossils.
->uniformitarianism introduced
->relative rock layers
- law of superposition
-> Geologic columns
-> Absolute age of rocks
- radioactive decay
-  half-life
-> Radiometric dating
-> index fossils