Divergent boundaries at the Mid-Atlantic Ridge lead to the widening of the Atlantic Ocean. This occurs through the creation of new oceanic crust in a process called seafloor spreading at a divergent plate boundary.
Divergent boundaries at the Mid-Atlantic Ridge cause the widening of the Atlantic Ocean by about 2.5 centimeters each year. As plates move apart, new oceanic crust is created, leading to seafloor spreading. The Mid-Atlantic Ridge is a prime example of a divergent plate boundary, where molten rock material emerges as the North American and Eurasian plates slowly drift apart.