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Earth’s magnetic field

Earth’s magnetic field

Earth’s magnetic field

As the earth rotates, its molten core generates electrical currents through a process called the dynamo effect. The electrical charges produce magnetic fields with a north and south magnetic pole, which are close to but not at the geographic poles. The magnetic poles move several kilometres a year. Many migratory birds seem to be able to detect the magnetic field, giving them a sense of northward or southward direction. They may also detect the angle of dip (the angle between the force field and the earth’s surface) and regional variation in the field’s strength, which would help them to form a magnetic map.

Source: Living Earth

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Te Ara - The Encyclopedia of New Zealand

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