Hot Rocks: Magnetic “Poles” Once at The Equator

Earth-702653 It has been 780,000 years since the last reversal, so we may be long overdue one. But will lethal radiation from space bombard the Earth, as it drops its protective magnetic shield during the reversal? Italian scientists studying one of the most mysterious natural phenomena say that polarity reversals seem to occur in clusters, indicating some kind of "memory" of previous events.

Scientists now say that the  Earth's magnetic poles were once near the equator, which could explain puzzling changes in the magnetism of rocks millions of years ago.

 The Earth's magnetic poles are aligned along roughly the same axis as its rotational poles. Geologists have assumed this was also true in the past, so they use volcanic rocks, which when they formed took on an imprint of the direction and strength of the Earth's magnetic field, to deduce the rocks' original latitude and to trace continental motions over the past billion years, which has created a puzzle for rocks in North America and eastern Europe. In both regions, there appear to be rocks that were at the equator at some points between 550 and 600 million years ago and near the poles for other parts of this time period.

There appear to be rocks that moved from the poles to the equator several times in 50 million years, which implies that the ancient continents sped across the surface at more than 45 centimetres a year – twice as fast as the top speed of plate tectonics – and then reversed course at a similarly improbable speeed, which is also too fast to be explained by a phenomenon called true polar wander, in which the Earth's entire crust and mantle reorient, moving a different geographic region to the north pole.

Reserach conducted by Alexandra Abrajevitch at Kochi University in Japan and Rob Van der Voo of the University of Michigan in Ann Arbor suggested that  the magnetic pole itself shifted by 90 degrees, so that it lined up along the equator.

 The planet's magnetic field is generated by the motion of molten iron flowing around a superhot, solid iron core. Changes in the thickness, viscosity and conductivity of the outer core in the past could have led to convection patterns that caused the magnetic pole to tilt.


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