From magnetic striping patterns, scientists can learn the following three things:
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The cause of magnetic pole reversals: Magnetic striping helps in understanding the history of the Earth's magnetic field and its reversals.
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The direction plates are moving relative to each other: The patterns in the magnetic striping correspond to the movements of tectonic plates and their directions.
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The speed of one plate as it subducts below another plate: By analyzing the magnetic strips, scientists can infer the rate at which tectonic plates are moving and interacting.
The other options regarding earthquake locations and the year of the next magnetic reversal are not determined by magnetic striping patterns.