F2-3 Shield Volcano
The structure of a shield volcano.

Scientists have grouped volcanoes into three general types based largely on their shape, and on the type of materials they erupt. These are: shield volcanoes, composite volcanoes, and cinder cone volcanoes.

Shield volcanoes are roughly oval shaped and have a broad base with gently sloping sides that have angles up to about 10°. Shield volcanoes are formed by repeated mafic lava flows that build up over time around a central vent. Shield volcanoes are composed primarily of basaltic rock since they are formed by mafic lava flows.

Shield volcanoes are among the largest volcanoes in the world since they are built up slowly over a fairly long period of time. The volcanoes of the Hawaiian Islands, the Galapagos Islands, and Iceland are all shield volcanoes. Mauna Loa, a shield volcano on the Big Island of Hawaii, is actually the world’s largest shield volcano with a diameter of over 80 kilometers (50 miles) at its base.