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Frequent eruptions along divergent plate boundaries such as the Mid-Atlantic Ridge form new ocean bottom in a process known as seafloor spreading. This process occurs slowly (1-15 centimeters per year) yet relentlessly, moving the platesâand the ocean floor and continents above themâfurther apart.olcanoes are common occurrences along the boundaries of Earthâs tectonic plates. These boundaries allow super-heated molten rock called magma, along with ash and gases, to rise through Earthâs crust and emerge on the surface, often dramatically.
Youngest rock on the ocean floor can be seen in divergent plate boundaries and hot spots. Tectonic plates are moving continuously. When two plates diverge to each other volcanic material erupt in the boundry. This liquid magma cools down and become solid magmatic rock. Such areas are called divergent boundary. If these two boundries are beneath an ocean than cooling process become faster. Such areas are called seafloor spreading. Atlantic mid oceanic ridge is the longest divergent boundary. Iceland is formed because of this process! Hot spots are also host the youngest rocks on Earth. Hawaii Islands are the well known examples of hot spots.