Proactive disclosure Print version ![Print version Print version](/web/20061103074509im_/http://gsc.nrcan.gc.ca/esst_images/_printversion2.gif) ![ÿ](/web/20061103074509im_/http://gsc.nrcan.gc.ca/esst_images/_spacer.gif) | ![ÿ](/web/20061103074509im_/http://gsc.nrcan.gc.ca/esst_images/_spacer.gif) | ![Geological Survey of Canada Geological Survey of Canada](/web/20061103074509im_/http://gsc.nrcan.gc.ca/esst_images/gsc_e.jpeg) Natural Resources Canada > Earth Sciences Sector > Geological Survey of Canada > Geomagnetism
Geomagnetism North Magnetic Pole
The Earth's magnetic field is shaped approximately like that of a bar
magnet and, like a magnet, it has two magnetic poles, one in the Canadian
arctic, referred to as the North Magnetic Pole, and one off the coast
of Antarctica, south of Australia, referred to as the South Magnetic
Pole. At the North Magnetic Pole the Earth's magnetic field is directed
vertically downward relative to the Earth's surface. Consequently, magnetic
dip, or inclination is 90° . In addition, the North Magnetic Pole
is the eventual destination for a traveller who follows his or her compass
needle from anywhere on Earth.
The North Magnetic Pole is slowly drifting across the Canadian Arctic.
The Geological Survey of Canada keeps track of this motion by periodically
carrying out magnetic surveys to redetermine the Pole's location. The
most recent survey, completed in May, 2001, determined an updated position
for the Pole and established that it is moving approximately northwest
at 40 km per year. The observed position for 2001 and estimated positions
for 2002 to 2005 are given in the table.
Year |
Latitude ( °N) |
Longitude ( °W) |
2001 |
81.3 |
110.8 |
2002 |
81.6 |
111.6 |
2003 |
82.0 |
112.4 |
2004 |
82.3 |
113.4 |
2005 |
82.7 |
114.4 |
Explore the pages listed in the menu to learn more about the North Magnetic Pole.
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