Scientists can learn the following from magnetic striping patterns:
- The direction plates are moving relative to each other.
- The speed of one plate as it subducts below another plate.
- The location of ancient faults caused by seismic activity.
These magnetic striping patterns, which are created as magma solidifies at mid-ocean ridges and records the Earth's magnetic field at the time of solidification, provide valuable information about tectonic activity and plate movement.