
A model of the Earth’s magnetic field: radial magnetic field at the core-mantle boundary (red/blue) and magnetic field lines as observed at the surface.
During a reversal the magnetic field won't be zero, but will assume a weaker and more complex form. It may fall to 10% of the present-day strength and have magnetic poles at the equator or even the simultaneous existence of multiple "north" and "south" magnetic poles.
Geomagnetic reversals occur a few times every million years on average. However, the interval between reversals is very irregular and can range up to tens of millions of years.
There can also be temporary and incomplete reversals, known as events and excursions, in which the magnetic poles move away from the geographic poles - perhaps even crossing the equator - before returning back to their original locations. The last full reversal, the Brunhes-Matuyama, occurred around 780,000 years ago. A temporary reversal, the Laschamp event, occurred around 41,000 years ago. It lasted less than 1,000 years with the actual change of polarity lasting around 250 years.














Comment: It would be interesting to know how the scientists determined the cave has been used by the hammerheads for a million years...