On average, it takes 250,000 years for Earth’s magnetic north to flip polarity.
As shown in rocks, magnetic pole reversals are one of the key gateways to recognizing the past.
On average, pole reversals occur every 200,000 to 300,000 years. We may be due for one soon.
What are magnetic field lines and pole reversals?
Earth’s magnetic field changes with time. It’s known to wander from place to place. And it doesn’t match with Earth’s geographic north and south poles.
In the past, magnetic poles have reversed and even changed direction. This means that the north pole becomes the south pole and vice versa.
There aren’t any patterns for magnetic pole reversals. They don’t reverse in regular intervals making them very unpredictable.
How do rocks show evidence of pole reversals?
Basaltic magma is rich with iron when it freezes. Because iron is magnetic, we use magnetometers to find the direction of the magnetic field.
When magma cools, the magnetic material aligns with Earth’s magnetic field. As it solidifies, it locks the magnetic field orientation like a tiny compass. Based on the rock’s magnetism, we can find the magnetic pole orientation.
So, within the first layer of basaltic lava, magnetite records the north pole direction. Then for the next layer, the south pole becomes the north pole.
How does our magnetic field protect Earth?
The magnetic field gives us a layer out in space called the magnetosphere high above in the atmosphere. It varies in distance but can extend up to 65,000 kilometers from Earth’s surface.
From space, the magnetosphere resembles a magnetic dipole. Field lines resonate in a circular pattern from magnetic north and south poles.
The magnetosphere allows life to exist on Earth’s surface. Without it, Earth would be exposed to cosmic and solar radiation from the sun.
During magnetic storms, trapped plasma flashes lights that are observable around the globe. This disturbance in the magnetosphere is what creates the Aurora Borealis or Northern Lights.
Summary: Earth’s Geomagnetic Reversal
Earth’s magnetic field changes every 200,000 years on average.
We know this by studying magnetic material in rocks.
But why do poles reverse?
We are still trying to find the cause for pole reversals and when the next one will occur.