Scientists can learn the following from magnetic striping patterns:
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The cause of magnetic pole reversals - Magnetic striping provides evidence of past geomagnetic reversals, which can help scientists understand the processes behind these events.
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The direction plates are moving relative to each other - The alternating patterns of magnetic stripes on either side of mid-ocean ridges indicate the movement of tectonic plates away from the ridge, revealing their directional movement.
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The speed of one plate as it subducts below another plate - The width of the magnetic stripes can give an estimate of the rate at which tectonic plates are moving, including during subduction.
The other options provided do not accurately reflect what scientists can derive from magnetic striping patterns.