MadSci Network: Earth Sciences |
The Earth's magnetic field behaves as a dipole (in fact, more than 90% of the field can be explained by a dipolar field) in all the regions, not only at the poles. That's why we can use a compass to obtain the north direction (if we consider the magnetic declination of the point where we are measuring, of course). But the Earth's field is not so strong that you could see a bar magnet stick on the ground! If you get a magnetized needle, you can notice that near the magnetic poles (that don't coincide with the geographic poles) the needle remains in the vertical position, and in the magnetic equator (that is not the geographic equator as well), the needle will stand on the horizontal. In the other places, the needle will dip a certain angle, that we call magnetic inclination, that varies from place to place in the Earth. Among other things, the Earth's magnetic field makes a barrier against the particles provenient from Sun in all regions, except at the magnetic poles, where the particles can enter, originating the auroras. Best regards Eder C. Molina eder@iag.usp.br Dept. of Geophysics IAG-USP
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