How it works
This Earth's magnetic field diagram has two scenes. The upper one shows the planet as a magnet; the lower one, not to scale, shows what the solar wind does to the field in space.
Read the full guide
The Earth as a magnet
Moving molten iron in the outer core makes the field. Its lines loop out of the ground at the south magnetic pole and back in at the north magnetic pole. The magnetic axis leans away from the rotation axis, so the magnetic poles are not at the geographic poles.
The field in space
The solar wind presses the field in on the side facing the Sun and stretches it into a long magnetotail on the other. The region inside is the magnetosphere and its edge is the magnetopause. Close to Earth, trapped particles fill two radiation belts.
Questions and answers
Where does Earth's magnetic field come from?
From the outer core. NASA and the US Geological Survey describe molten iron moving there by convection, which drives electric currents, and those currents make the magnetic field.
What is the difference between the geographic and the magnetic poles?
The geographic poles are where the rotation axis meets the surface. The magnetic poles are where the field is vertical. They are near each other but not in the same place, and the magnetic poles move.
Why does a compass not point exactly north?
A compass needle lines up with the magnetic field, not with the rotation axis. The angle between its direction and geographic north is called declination, and it changes with place and time.
How do I label a diagram of Earth's magnetic field?
Start with the two axes and the four poles, then the field lines and the outer core. In space, label the solar wind, the magnetosphere, its edge the magnetopause, the magnetotail and the radiation belts.