Shield
Shield volcanoes are one of the four major types of volcanoes, distinguished from the three other major volcanic types, stratovolcanoes, lava domes, and cinder cones, by distinct differences in structure and composition. Stratovolcanoes are built up by the accumulation of thick, viscous lavas, cinder cones are constructed of tephra ejected in explosive eruptions, and lava domes are built from extremely thick lava which can't flow far from the vent. In comparison, shield volcanoes are usually built of low viscosity basaltic lavas that erupt in longer cycles than that of a stratovolcano.