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The answer lies in ocean basalts. As the sea floor slowly spreads, the igneous rock of which it is comprised cools and congeals, recording earth's current magnetic pole alignment. It turns out there are numerous parallel stripes encoded within ocean bedrock, indicating the strength and polarity of earth's magnetic field over the course of many millions of years. One trouble with this record is that once the sea floor reaches a continental plate margin it is subducted beneath the crustal rock and destroyed, so the record is only about a hundred million years old at most.

However, there is excellent agreement between the sea floor rock and volcanic rock deposited on earth's surface. We can date isotopes within that rock to compare the sea floor record with the record on land, and confirm the accuracy of the dating techniques. One fascinating find is known as the Jaramillo Creek event, a pole reversal from about 900,000 years ago.

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Examination of the mid-Atlantic ridge and the lave deposits left on the ocean floor has indicated that every few million years, the Earth's magnetic polarity seems to reverse.

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Q: How do scientists know that the earths magnetic poles have reversed themselves many times during earths history?
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What do earths magnetic stripes indicate about ocean crust?

reversed itself in the pastThe alternating magnetic orientation is caused by polar shifts or reversal, (not end of the world kinda stuff). When the rock is new and molten the grains are free to align themselves with the prevailing magnetic field, as the rock cools, the grains are frozen in time. As the sea floor expands outward (in the Atlantic), it is regularly striped with rock oriented in different directions. This indicates that the magnetic poles have reversed many times throughout the Earth's history.


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