F1-4 Volcanoes and Divergent Plate Boundaries

Volcanoes can also form when two plates move apart (diverge), and magma flows up between the two plates. This is what is occurring in the Mid-Atlantic Ridge as oceanic crust is being pulled apart (i.e., seafloor spreading). Much of this magma from sea floor spreading does not reach the surface and remains underwater. A rare spot where this is visible above water is in Iceland as the North American and Eurasian plates diverge.

Divergent oceanic crust has resulted in a string of volcanoes forming in Iceland along the plate boundaries.
A fissure zone in Thingvellir National Park in Iceland. On the right of the fissure, the North American plate is pulling westward away from the Eurasian plate on the left-hand side of the fissure. Thingvellir National Park is a UNESCO World Heritage Site. Thingvellir was the site of meetings for the Althing, Iceland’s open air parliament between 930 CE and 1798 CE.

Although most divergent plate motion is the result of oceanic crust moving apart, this process can also be seen above ground as continental crust is pulled apart. This is exactly what is happening in East Africa in the Great Rift Valley as two parts of the African plate are pulled apart. A string of volcanoes has formed in the valley produced by this divergent plate motion.