The positions of the magnetic poles can be defined in at least two ways: locally or globally. The local definition is the point where the magnetic field is vertical. This can be determined by measuring the inclination. The inclination of the Earth's field is 90° (downwards) at the North Magnetic Pole and –90° (upwards) at the South Magnetic Pole. The two poles wander independently of each other and are not directly opposite each other on the globe. Movements of up to per year have been observed for the North Magnetic Pole. Over the last 180 years, the North Magnetic Pole has been migrating northwestward, from Cape Adelaide in the Boothia Peninsula in 1831 to from Resolute Bay in 2001. The magnetic equator is the line where the inclination is zero (the magnetic field is horizontal).
the positions of the magnetic poles can be defined in at least two ways locally or globally the local definition is the point where the magnetic field is vertical this can be determined by measuring the inclination the inclination of the earth's field is 90° (downwards) at the north magnetic pole and –90° (upwards) at the south magnetic pole the two poles wander independently of each other and are not directly opposite each other on the globe movements of up to per year have been observed for the north magnetic pole over the last 180 years the north magnetic pole has been migrating northwestward from cape adelaide in the boothia peninsula in 1831 to from resolute bay in 2001 the magnetic equator is the line where the inclination is zero (the magnetic field is horizontal)