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- Q348567 subject Q7446336.
- Q348567 subject Q7463183.
- Q348567 abstract "The geomagnetic poles are antipodal points where the axis of a best-fitting dipole intersects the Earth's surface. This dipole is equivalent to a powerful bar magnet at the center of the Earth, and it is this theoretical dipole that comes closer than any other to accounting for the magnetic field observed at the Earth's surface. In contrast, the actual Earth's magnetic poles are not antipodal—that is, they do not lie on a line passing through the center of the Earth.Owing to motion of fluid in the Earth's outer core, the actual magnetic poles are constantly moving. However, over thousands of years their direction averages to the Earth's rotation axis. On the order of once every half a million years, the poles reverse (north changes place with south).".
- Q348567 thumbnail Geomagnetisme.svg?width=300.
- Q348567 wikiPageExternalLink servers.shtml.
- Q348567 wikiPageWikiLink Q101949.
- Q348567 wikiPageWikiLink Q1043682.
- Q348567 wikiPageWikiLink Q104698.
- Q348567 wikiPageWikiLink Q1059740.
- Q348567 wikiPageWikiLink Q11421.
- Q348567 wikiPageWikiLink Q117987.
- Q348567 wikiPageWikiLink Q1269129.
- Q348567 wikiPageWikiLink Q146841.
- Q348567 wikiPageWikiLink Q162219.
- Q348567 wikiPageWikiLink Q16760598.
- Q348567 wikiPageWikiLink Q1810738.
- Q348567 wikiPageWikiLink Q1814982.
- Q348567 wikiPageWikiLink Q1976304.
- Q348567 wikiPageWikiLink Q2.
- Q348567 wikiPageWikiLink Q2076913.
- Q348567 wikiPageWikiLink Q215589.
- Q348567 wikiPageWikiLink Q244743.
- Q348567 wikiPageWikiLink Q34735.
- Q348567 wikiPageWikiLink Q3656071.
- Q348567 wikiPageWikiLink Q394352.
- Q348567 wikiPageWikiLink Q42278.
- Q348567 wikiPageWikiLink Q505356.
- Q348567 wikiPageWikiLink Q619254.
- Q348567 wikiPageWikiLink Q6500960.
- Q348567 wikiPageWikiLink Q7100757.
- Q348567 wikiPageWikiLink Q7446336.
- Q348567 wikiPageWikiLink Q7463183.
- Q348567 wikiPageWikiLink Q7950.
- Q348567 wikiPageWikiLink Q79833.
- Q348567 wikiPageWikiLink Q842763.
- Q348567 wikiPageWikiLink Q853422.
- Q348567 wikiPageWikiLink Q857867.
- Q348567 wikiPageWikiLink Q933.
- Q348567 wikiPageWikiLink Q934.
- Q348567 point "80.08 -72.21".
- Q348567 type SpatialThing.
- Q348567 comment "The geomagnetic poles are antipodal points where the axis of a best-fitting dipole intersects the Earth's surface. This dipole is equivalent to a powerful bar magnet at the center of the Earth, and it is this theoretical dipole that comes closer than any other to accounting for the magnetic field observed at the Earth's surface.".
- Q348567 label "Geomagnetic pole".
- Q348567 lat "80.08".
- Q348567 long "-72.21".
- Q348567 depiction Geomagnetisme.svg.