Solidified magma from the Mid-Atlantic Divide.
The North American and European continental plates are being pushed apart. The magma thrusting up between the two cools and turns to new rock. As the continents move further apart, more and more rock is formed in convey-belt fashion, creating a historical record
Frozen within the rock are magnetic particles oriented towards the pole. They are observed to point different directions, depending on the age of the rock.
So, pole reversals.
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