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On top of that it will be either responsive or come with a mobile theme and will not be handled inside of numerous tables.
The main part of Earth's magnetic field is generated in the core, the site of a dynamo process that converts the kinetic energy of thermally and compositionally driven convection into electrical and magnetic field energy.
The field extends outwards from the core, through the mantle, and up to Earth's surface, where it is, approximately, a dipole. The poles of the dipole dating in worcester located close to Earth's geographic poles. At the equator of the magnetic field, the magnetic-field strength at the surface is 3. This causes secular variation of the main field and field reversals at irregular intervals averaging a few times every million years. The most recent reversal occurred approximatelyyears ago. The extent of Earth's magnetic field in space defines the magnetosphere.
Ions and electrons of the solar wind are deflected by the magnetosphere; solar wind pressure compresses the dayside of the magnetosphere, to about 10 Earth radii, and extends the nightside magnetosphere into a long tail.