Titlebook: El Hierro Island; Pablo J. González Book 2023 The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature

MOAN

Geomorphology of Tagoro Volcano Along Eruptive and Posteruptive Phasese eruption of the Tagoro volcano and later evolution. The major geomorphological features were achieved fundamentally by the use of Multibeam EM710 echosounder data. Eruption was characterized by two main phases, the first one alternate stages of vertical growth and denudation by development of basa

calorie

Ten Years of Intense Physical–Chemical, Geological and Biological Monitoring Over the Tagoro Submariprocesses in specific scientific fields as physical and chemical oceanography or marine geology but also its interactions over the marine biology in one of the richest marine ecosystems in Europe. This chapter aims to summarize the most relevant physical–chemical, geological and biological changes t

緯度

Tagoro Submarine Volcano as a Natural Source of Significant Dissolved Inorganic Nutrientsn intensely monitored during both the eruptive stage (October 2011–March 2012) and the post-eruptive hydrothermal stage (March 2012—ongoing). The obtained seven-years dataset comprises over 3300 water samples analysed for concentrations of silicate (Si(OH).), phosphate (PO.), nitrate?+?nitrate(NO.?+

嬉耍

Microbial Communities Surrounding an Underwater Volcano Near the Island of El Hierro (Canary Islandsrganisms that can be found inhabiting hydrothermal plumes, metalliferous sediments, or forming dense microbial biofilms or mats on the surrounding of the vents. Most of the current knowledge on the microbiology associated with underwater volcanic activity comes from the study of deep-sea hydrotherma

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Identification and Management of Indirect Volcanic Risks: Citizens’ Rockfall Observatory on the Islat plans. However, SVH may cause more damage than primary volcanic hazards (PVH). The magmatic unrest on El Hierro Island in 2011–2012 is a perfect example of how SVH can be one of the leading causes of damage during magmatic unrest. Rockfalls are common on the island of El Hierro, mainly controlled

ANTH

Tagoro, the Youngest Submarine Volcano in the Spanish Geoheritage Inventory: Scientific Value, Geocoo island and ended in early March 2012. This eruption produced a volcanic cone, hornitos, a thick pyroclastic apron that prograded towards the base of the volcanic edifice and volcanic products that emerged from the sea floor over sea level, such as lava balloons and low-density vesicular pyroclasts

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https://doi.org/10.1007/978-3-658-01332-5m depth during a continuous eruptive pulse; (ii) a similar magmatic evolution and residence times at depth between previous and 2011–2012 eruptions on the island; (iii) an insignificant interaction of external fluids with the magma at depth or within the ascent conduit; (iv) a present-day magnetomet