Why are there Symmetrical Patterns of Magnetic Anomalies preserved on either side of mid-ocean Ridges

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Why are there symmetrical patterns of magnetic anomalies preserved on either side of mid-ocean ridges (i.e., divergent boundaries)? Volcanic island arcs form over the divergent boundary, producing the symmetrical pattern of magnetic anomalies. O Lava and magma solidify at the mid-ocean ridge, preserving a paleomagnetic record. The magnetic polarity of one plate reverses as the plates are pulled apart. The magnetic polarity of the other plate stays the same. Lava and magma solidify at the mid-ocean ridge, preserving a paleomagnetic record. That record is then split in half as one plate subducts under the other. Lava and magma solidify at the mid-ocean ridge, preserving a paleomagnetic record. That record is then split in half as the two plates pull away from each other.

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