The Hydrothermal Vent Field at the Eastern Edge of the Hellenic Volcanic Arc: The Avyssos Caldera (Nisyros)
Almost three-quarters of known volcanic activity on Earth occurs in underwater locations. The presence of active hydrothermal vent fields in such environments is a potential natural hazard for the environment, society, and economy. Despite its importance for risk assessment and risk mitigation, the...
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doaj-7e6fc08dd46e4a90a39acf6c55cc51b52021-07-23T13:42:16ZengMDPI AGGeosciences2076-32632021-07-011129029010.3390/geosciences11070290The Hydrothermal Vent Field at the Eastern Edge of the Hellenic Volcanic Arc: The Avyssos Caldera (Nisyros)Ana Dura0Theo J. Mertzimekis1Paraskevi Nomikou2Andreas Gondikas3Martín Manuel Gómez Míguez4Evangelos Bakalis5Francesco Zerbetto6Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Zografou Campus, GR-15784 Athens, GreeceDepartment of Physics, National and Kapodistrian University of Athens, Zografou Campus, GR-15784 Athens, GreeceDepartment of Geology and Geoenvironment, National and Kapodistrian University of Athens, Zografou Campus, GR-15784 Athens, GreeceDepartment of Geology and Geoenvironment, National and Kapodistrian University of Athens, Zografou Campus, GR-15784 Athens, GreeceDepartment of Physics, National and Kapodistrian University of Athens, Zografou Campus, GR-15784 Athens, GreeceDipartimento di Chimica “G. Ciamician”, Università di Bologna, 40126 Bologna, ItalyDipartimento di Chimica “G. Ciamician”, Università di Bologna, 40126 Bologna, ItalyAlmost three-quarters of known volcanic activity on Earth occurs in underwater locations. The presence of active hydrothermal vent fields in such environments is a potential natural hazard for the environment, society, and economy. Despite its importance for risk assessment and risk mitigation, the monitoring of volcanic activity is impeded by the remoteness and the extreme conditions of many underwater volcanoes. The morphology and the activity of the submarine caldera, Avyssos, at the northern part of Nisyros volcano in the South Aegean Sea (Greece), were studied using a remotely operated underwater vehicle. The recorded time series of temperature and conductivity over the submarine volcano have been analyzed in terms of the Generalized Moments Method. This type of analysis can be used as an indicator for the state of activity of a submarine volcano. Here, we expand the work conducted for the first time in 2018. We present the findings of the geological exploration and the mathematical analysis, obtained from the data collected in October 2010. The temperature and conductivity time series show minor fluctuations in a rather stable environment. Based on these results, the impact of developing appropriate mechanisms and policies to avoid the associated natural hazard is expected to be important.https://www.mdpi.com/2076-3263/11/7/290hydrothermal ventNisyrosGeneralized Moments Method |
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DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Ana Dura Theo J. Mertzimekis Paraskevi Nomikou Andreas Gondikas Martín Manuel Gómez Míguez Evangelos Bakalis Francesco Zerbetto |
spellingShingle |
Ana Dura Theo J. Mertzimekis Paraskevi Nomikou Andreas Gondikas Martín Manuel Gómez Míguez Evangelos Bakalis Francesco Zerbetto The Hydrothermal Vent Field at the Eastern Edge of the Hellenic Volcanic Arc: The Avyssos Caldera (Nisyros) Geosciences hydrothermal vent Nisyros Generalized Moments Method |
author_facet |
Ana Dura Theo J. Mertzimekis Paraskevi Nomikou Andreas Gondikas Martín Manuel Gómez Míguez Evangelos Bakalis Francesco Zerbetto |
author_sort |
Ana Dura |
title |
The Hydrothermal Vent Field at the Eastern Edge of the Hellenic Volcanic Arc: The Avyssos Caldera (Nisyros) |
title_short |
The Hydrothermal Vent Field at the Eastern Edge of the Hellenic Volcanic Arc: The Avyssos Caldera (Nisyros) |
title_full |
The Hydrothermal Vent Field at the Eastern Edge of the Hellenic Volcanic Arc: The Avyssos Caldera (Nisyros) |
title_fullStr |
The Hydrothermal Vent Field at the Eastern Edge of the Hellenic Volcanic Arc: The Avyssos Caldera (Nisyros) |
title_full_unstemmed |
The Hydrothermal Vent Field at the Eastern Edge of the Hellenic Volcanic Arc: The Avyssos Caldera (Nisyros) |
title_sort |
hydrothermal vent field at the eastern edge of the hellenic volcanic arc: the avyssos caldera (nisyros) |
publisher |
MDPI AG |
series |
Geosciences |
issn |
2076-3263 |
publishDate |
2021-07-01 |
description |
Almost three-quarters of known volcanic activity on Earth occurs in underwater locations. The presence of active hydrothermal vent fields in such environments is a potential natural hazard for the environment, society, and economy. Despite its importance for risk assessment and risk mitigation, the monitoring of volcanic activity is impeded by the remoteness and the extreme conditions of many underwater volcanoes. The morphology and the activity of the submarine caldera, Avyssos, at the northern part of Nisyros volcano in the South Aegean Sea (Greece), were studied using a remotely operated underwater vehicle. The recorded time series of temperature and conductivity over the submarine volcano have been analyzed in terms of the Generalized Moments Method. This type of analysis can be used as an indicator for the state of activity of a submarine volcano. Here, we expand the work conducted for the first time in 2018. We present the findings of the geological exploration and the mathematical analysis, obtained from the data collected in October 2010. The temperature and conductivity time series show minor fluctuations in a rather stable environment. Based on these results, the impact of developing appropriate mechanisms and policies to avoid the associated natural hazard is expected to be important. |
topic |
hydrothermal vent Nisyros Generalized Moments Method |
url |
https://www.mdpi.com/2076-3263/11/7/290 |
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