Titlebook: Nisyros Volcano; The Kos - Yali - Nis Volker Jörg Dietrich,Evangelos Lagios Book 2018 Springer International Publishing AG 2018 Dodecanese

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Geography, Nature and Habitation of Nisyros Volcano,, conical shaped and caldera bearing stratovolcano. Nisyros is located between the islands of Kos and Tilos within a prehistoric volcanic field that generated the largest volcanic eruption in the eastern Mediterranean (Kos Plateau Tuff), which devastated the entire Dodecanese area 161,000 years ago.

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Geodynamics and Volcanism in the Kos-Yali-Nisyros Volcanic Field,nce between the African plate and the Anatolian and Aegean microplates. Southeast-ward subduction of oceanic lithosphere and crust of a remnant Thethys ocean beneath the microplates are responsible for the generation of magmatism and volcanism during the past 5 million years. This formed the South A

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The Hydrothermal System and Geothermal Activity,g structures. Hydrothermal explosions in the caldera floor of unknown age until recently created a complex set of intersecting crater structures with evident structural controls. Low-temperature thermal springs and fumaroles occur along known and inferred fracture systems and their crossing points,

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Seismicity and Tomographic Imaging of the Broader Nisyros Region (Greece),kes have been reported in the study area. Nevertheless, seismic activity during the last decades is moderate to low, consisting of both shallow and intermediate depth earthquakes. The main regions of the broader area with observed spatiotemporally clustered seismicity are between Nisyros and Karpath