Discover, February 1, 1994
Swear not by magnetic north–it drifts, takes long excursions, and sometimes even heads south. Earth’s patchy core may be to blame.
Although it has long served as a fixed reference for navigators, Earth’s magnetic field is anything but static. Over the course of decades and centuries, in what is called secular variation, the pattern of the field drifts randomly, such that at a given geographic location the direction a compass needle points may change by tens of degrees. Every 30,000 years or so things get more extreme: the magnetic poles suddenly begin shifting toward the equator, only to snap back into place.