The Earth's magnetic field lines appear to emanate perpendicularly from the poles and go round along the Earth from the South Pole to the North Pole. Therefore, the Earth's magnetic field is generally not parallel to the ground at every location. It is parallel to the earth at the equator near the earth's surface.
The Earth's magnetic field, also known as the geomagnetic field, is a magnetic field that extends from the Earth's interior into space, where it interacts with the solar wind, a stream of charged particles emanating from the Sun.
The magnetic field varies in strength over the earth's surface. It is strongest at the poles and weakest at the equator.
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