Shield volcano

A shield volcano is a type of volcano named for its low profile, resembling a warrior's shield lying on the ground. It is formed by the eruption of highly fluid (low viscosity) lava, which travels farther and forms thinner flows than the more viscous lava erupted from a stratovolcano. Repeated eruptions result in the steady accumulation of broad sheets of lava, building up the shield volcano's distinctive form.

Mauna Loa, a shield volcano in Hawaii
An Ancient Greek warrior's shield–its circular shape and gently sloping surface, with a central raised area, is a shape shared by many shield volcanoes.

Shield volcanoes are found wherever fluid low-silica lava reaches the surface of a rocky planet. However, they are most characteristic of ocean island volcanism associated with hot spots or with continental rift volcanism.[1] They include the largest volcanoes on earth, such as Tamu Massif and Mauna Loa.[2] Giant shield volcanoes are found on other planets of the Solar System, including Olympus Mons on Mars[3] and Sapas Mons on Venus.[4]

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