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| | Geomagnetism - Earth's magnetic field |
 | | The magnetic field is often visualized in terms of magnetic field lines, or lines of force, that leave one end of the magnet, called the north pole, arc through space, and re-enter the magnet at the other end, the south pole. |
 | | Mathematically, the Earth's magnetic field is normally described by a spherical harmonic expansion, a series of special spherical functions of latitude/longitude and their associated coefficients. |
 | | Charts of the magnetic declination and total intensity, the two most widely used magnetic field elements, are shown in the accompanying figures. |
| gsc.nrcan.gc.ca /geomag/field/index_e.php (357 words) |
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