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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


Generating Earth's Magnetic Field

by Stephen Marshak
Overview Image

Magnetic lines of force in space

Credit: W. W. Norton

Explantatons for how the Earth generates a magnetic field rely on the theory of electronmagnetism: an electric current generates magnetism, and the movement of an electrical conductro (such as metal wire) in a magentic field produces electricty. Because iron allow is a good electrical conductor (electrons flow through it easily), the flow of iron alloy makes the Earth's outer core into an electromagnet.

To better understand the generation of Earth's magnetic field, consider an electric power plant. In a power plant, water or wind power spins a wire coil (an electrical conductor) around an iron bar (a permanent magnet). This apparatus is a dynamo. The motion of the wire in the bar's magnetic field generates an electric current in the wire, which in turn generates more magnetism. Similarly, in the Earth, convection and the Earth's rotation cause liquid iron alloy (an electrical conductor) to flow in Earth's magnetic field (see figure). This flow generates an electric current, which in turn generates more magnetism.

The Earth differs from an electric power plant in that there is no permanent magnet in the center of the Earth; at the very high temperatures of the core, permanent magnets can't exist, because thermal energy makes atoms vibrate and tumble so fast that their tiny magnetic dipoles can't lock into alignment. Instead, the Earth is a "self-exciting dynamo," meaning that the magnetism produced by elecric currents in the outer core is the magnetism that led to the generation of an electric current in the flowing iron alloy in the first place—this system perpetuates itself.


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