Yes, it is true that along the Mid-Atlantic Ridge, the North American Plate and the Eurasian Plate are moving apart at a slow rate, typically around 2.5 centimeters (1 inch) per year. This divergent boundary allows magma to rise and create new oceanic crust, contributing to the growth of the Atlantic Ocean. While they are moving away from each other, they are not moving together; rather, they are separating as a result of tectonic activity.
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