Evidence of a Modern Deep-Water Magmatic Hydrothermal System in the Canary Basin (Eastern Central Atlantic Ocean)
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AuthorsMedialdea, T.; Somoza, L.; González, F.J.; Vázquez, J.T. (Juan Tomás); de Ignacio, C.; Sumino, H.; Sánchez-Guillamón, O. (Olga); Orihashi, Y.; León, R.; Palomino, D. (Desirée)
KeywordsDEEP SEA FLOOR
Submarine volcanic eruptions are frequent and important events, yet they are rarely observed. Here we relate bathymetric and hydroacoustic images from the 2011 to 2012 El Hierro eruption with surface observations and deposits imaged and sampled by ROV. As a result of the shallow submarine eruption, a new volcano named Tagoro grew from 375 to 89 m depth. The eruption consisted of two main phases of edifice construction intercalated with collapse events. Hydroacoustic images show that the eruptions ranged from explosive to effusive with variable plume types and resulting deposits, even over short time intervals. At the base of the edifice, ROV observations show large accumulations of lava balloons changing in size and type downslope, coinciding with the area where floating lava balloon fallout was observed. Peaks in eruption intensity during explosive phases generated vigorous bubbling at the surface, extensive ash, vesicular lapilli and formed high-density currents, which together ...