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1 The Earth in Context
2 The Way the Earth Works: Plate Tectonics
3 Patterns in Nature: Minerals
4 Up From the Inferno: Magma and Igneous Rocks
5 A Surface Veneer: Sediments and Sedimentary Rocks
6 Change in the Solid State: Metamorphic Rocks
7 The Wrath of Vulcan: Volcanic Eruptions
8 A Violent Pulse: Earthquakes
9 Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building
10 Deep Time: How Old is Old?
11 A Biography of Earth
12 Riches in Rock: Energy and Mineral Resources
13 Unsafe Ground: Landslides and Other Mass Movements
14 Streams and Floods: The Geology of Running Water
15 Restless Realm: Oceans and Coasts
16 A Hidden Reserve: Groundwater
17 Dry Regions: The Geology of Deserts
18 Amazing Ice: Glaciers and Ice Ages
19 Global Change in the Earth System


The Rest of the Story: Earth's Rotation

by Stephen Marshak
Overview Image

Time-lapse foucault's pendulum

Credit: NASA

If you gaze at the night sky for a long time, you'll see that the stars move in a circular path around the North Star. This movement suggests either that the Earth spins on its axis (an imaginary line connecting the North and South Poles) with respect to the stars, or that the stars orbit the earth.

Curiously, it was not until the middle of the neneteenth century that Jean Bernard Léon Foucault (1819-1868), a French physicist, proved that the Earht spins on its axis. He made this discovery by settinga heavy pendulum, attached to a long string, in motion. As the pendulum continued to swing for many days, Foucault noted that the plane in which it oscillated (a plane perpendicular to the Earth's surface) appeared to rotate around a vertical axis (a line perpendicular to the Earth's surface.) If Newton's first law of motion—objects in motion remain in motion, objects at rest remain at rest—was correct, then the only exlanation for this phenomenon was that the Earth rotated under the pendulum while the pendulum continued to swing in the same plane (Fig. 1.4a, b). Foucalt displayed his discover beneath the great dome of the Pantheon in Paris, to much acclaim.

We now know that, in fact, the earth's spin axis is not fixed in orientation; rather, it wobbles. This wobble, known as precession corresponds to the wobble of a top as it spins. We'll see later in this book that the precession of the Earth's axis, which takes 26,500 years, may affect the planet's climate.


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