Changes in direction or orientation of the magnetic field of the Earth that have occurred from time to time. (Several hundred are known in the geological record.) Sometimes the north magnetic pole is near the geographic North Pole and sometimes near the South Pole in Antarctica.
Note: The causes of these reversals are not known in detail, but are thought to be related to the motion of fluids in the Earth’s core.
noun 1. . noun, Electricity. 1. that part of the magnetic induction that is determined at any point in space by the current density and displacement current at that point independently of the magnetic or other physical properties of the surrounding medium. Symbol: H. magnetic field strength A vector quantity indicating the ability of a […]
noun, Electricity. 1. the total magnetic induction crossing a surface, equal to the integral of the component of magnetic induction perpendicular to the surface over the surface: usually measured in webers or maxwells. noun 1. a measure of the strength of a magnetic field over a given area perpendicular to it, equal to the product […]
noun, Electronics. 1. (def 33).
noun, Physics. 1. hysteresis in a ferromagnetic material; the lag in the response of magnetic induction to changes of magnetic intensity.