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- Apparent_polar_wander abstract "Apparent polar wander (APW) is the perceived movement of the Earth's paleo-magnetic poles relative to a continent while regarding the continent being studied as fixed in position. It is frequently displayed on the present latitude-longitude map as a path connecting the locations of geomagnetic poles, inferred at distinct times using paleomagnetic techniques.In reality, the relative polar movement can either be polar wandering or continental drift (or a combination of both). Data from around the globe is needed in order to isolate or distinguish between the two. Nevertheless, the magnetic poles rarely stray far from the geographic poles of the planet. Therefore, the concept of apparent polar wander is very useful in plate tectonics, since it can retrace the relative motion of continents, as well as the formation and break-up of supercontinents.".
- Apparent_polar_wander wikiPageID "26240231".
- Apparent_polar_wander wikiPageLength "7971".
- Apparent_polar_wander wikiPageOutDegree "8".
- Apparent_polar_wander wikiPageRevisionID "665688503".
- Apparent_polar_wander wikiPageWikiLink Category:Plate_tectonics.
- Apparent_polar_wander wikiPageWikiLink Closure_temperature.
- Apparent_polar_wander wikiPageWikiLink Continent.
- Apparent_polar_wander wikiPageWikiLink Earth.
- Apparent_polar_wander wikiPageWikiLink Eulers_rotation_theorem.
- Apparent_polar_wander wikiPageWikiLink Paleomagnetism.
- Apparent_polar_wander wikiPageWikiLink Poles_of_astronomical_bodies.
- Apparent_polar_wander wikiPageWikiLinkText "Apparent polar wander".
- Apparent_polar_wander wikiPageWikiLinkText "apparent polar wander".
- Apparent_polar_wander hasPhotoCollection Apparent_polar_wander.
- Apparent_polar_wander wikiPageUsesTemplate Template:Books-inline.
- Apparent_polar_wander wikiPageUsesTemplate Template:Reflist.
- Apparent_polar_wander subject Category:Plate_tectonics.
- Apparent_polar_wander hypernym Movement.
- Apparent_polar_wander type Organisation.
- Apparent_polar_wander comment "Apparent polar wander (APW) is the perceived movement of the Earth's paleo-magnetic poles relative to a continent while regarding the continent being studied as fixed in position. It is frequently displayed on the present latitude-longitude map as a path connecting the locations of geomagnetic poles, inferred at distinct times using paleomagnetic techniques.In reality, the relative polar movement can either be polar wandering or continental drift (or a combination of both).".
- Apparent_polar_wander label "Apparent polar wander".
- Apparent_polar_wander sameAs m.0b75r65.
- Apparent_polar_wander sameAs Q4780930.
- Apparent_polar_wander sameAs Q4780930.
- Apparent_polar_wander wasDerivedFrom Apparent_polar_wander?oldid=665688503.
- Apparent_polar_wander isPrimaryTopicOf Apparent_polar_wander.