Cerro Azul (Spanish: Blue Hill) is a shield volcano on the south western part of Isabela Island in the Galápagos Islands. At a height of it is the second highest peak in the Galapagos and due to its topographic prominence of over it is categorised as an ultra. The volcano is one of the most active in the Galapagos, with the last eruption between May and June 2008. Geology The Galapagos Islands are believed to be formed from a mantle plume which creates a hotspot of volcanic activity away from plate boundaries where islands then form above it, similar to process that has created the Hawaiian islands. Cerro Azul is at the edge of the upwelling with steep drop offs in the ocean to the West, while the sea is shallower to the east of Isabela Island. Cerro Azul is one of six coalescing volcanoes on Isabela Island: Ecuador, Wolf, Darwin, Alcedo, and Sierra Negra. Cerro Azul is shaped like a large upturned soup bowl and like the other volcanoes on Isabela Island has a large caldera its one at 4x5 km across is one of the smallest. The caldera shows evidence of collapse following eruptive episodes and reaches a depth of 450 m to 650 m below the rim of the caldera, only Wolf Volcano in the Galapagos is as deep. The volcano is 34 by 22 km at maximum and has a volume of 172 km3. It has steep upper slopes of between 12 and 30 degrees. The shape of the volcano is affected by the sharp ocean drop off to the west where this flank of the volcano slopes steeply to the ocean. Historical eruptions date back to 1932, but the volcano has had a number of active periods since then in 1940, 1943,1949, 1951, 1959, 1968, 1979, 1998 and most recently in 2008. It is estimated that the surface of the volcano is young, less than 5000 years old and it is estimated that the volcano is about 350,000 years old. The age of Cerro Azul is similar to Sierra Negra and Alcedo and their positioning is not believed to be related to plate movement over the magma plume but instead an interaction between the plume and the lithosphere. The 2008 eruption began in May and included a fissure eruption on the southeast flank of the volcano; the eruption in 1998 had also included fissure eruptions