Magnetic North Pole

From Wikipedia, the free encyclopedia

The Earth's Magnetic North Pole (actually the south pole of the Earth's magnetic field) is the shifting point to which the "north" end of a dipole magnet points. It drifts from 10 to 40 kilometers per year; indeed, affected by charged particles from the sun, it drifts by the day [1], and is not located at Earth's North Terrestrial Pole. It is offset from the axis of Earth's rotation by about 11 degrees[citation needed].

Magnetic pole positions

North Magnetic Pole [1] (2001) 81.3° N 110.8° W (2004 est) 82.3° N 113.4° W (2005 est) 82.7° N 114.4° W
South Magnetic Pole [2] (1998) 64.6° S 138.5° E. (2004 est) 63.5° S 138.0° E


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