Earth’s magnetic field (and the surface magnetic field) is approximately a magnetic dipole, with the magnetic field S pole near the Earth’s geographic north pole (see Magnetic North Pole) and the other magnetic field N pole near the Earth’s geographic south pole (see Magnetic South Pole).
The earth behaves as a magnetic dipole inclined at small angle to the earth’s axis of rotation with its south pole pointing geographic north. The idea of earth having magnetism is supported by following facts. A freely suspended magnet always comes to rest in N-S direction.
Explanation:
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Earth’s magnetic field (and the surface magnetic field) is approximately a magnetic dipole, with the magnetic field S pole near the Earth’s geographic north pole (see Magnetic North Pole) and the other magnetic field N pole near the Earth’s geographic south pole (see Magnetic South Pole).
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Answer:
The earth behaves as a magnetic dipole inclined at small angle to the earth’s axis of rotation with its south pole pointing geographic north. The idea of earth having magnetism is supported by following facts. A freely suspended magnet always comes to rest in N-S direction.
Explanation:
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