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- W2337087995 abstract "Recently, we made a study of the mechanical interaction between several active central volcanoes in the central part of Iceland. Here we extend this study to a wider part of the Neovolcanic Zone of Iceland, defined as the part of Iceland containing rocks belonging to the Bruhnes magnetic epoch (<0.8Ma). We believe that for assessing volcanic hazards and associated risks in an active area, it must be known if its volcanoes interact mechanically. If volcanoes interact mechanically then, in our definition, an unrest in one volcano may trigger unrest in one or more nearby volcanoes. The Neovolcanic Zone consists of three subzones: the North Volcanic Zone (NVZ), the West Volcanic Zone (NVZ), and the East Volcanic Zone (EVZ). The main geological features of the Neovolcanic Zone are the so-called volcanic systems. Of a total of 30, some 19 volcanic systems contain 23 central volcanoes, meaning that some systems contain more than one central volcano. A central volcano, by definition, has a shallow crustal magma chamber in addition to the deep-seated reservoir that underlies most of the associated volcanic system. The presence of a central volcano within a volcanic system indicates its level of maturity; the Vestmannaeyjar Volcanic System (the southernmost system in Iceland), for instance, has not as yet developed a central volcano and is therefore considered a young volcanic system. All the central volcanoes studied here belong to the EVZ. We modelled the central volcanoes as circular holes or inclusions in an elastic crust, under a tensile stress of 5MPa in a direction parallel with the spreading vector. The modelling shows two main results. The first main result is that the central volcanoes of the EVZ form two clusters. One cluster is at the northern end of the EVZ, under the" @default.
- W2337087995 created "2016-06-24" @default.
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- W2337087995 date "2008-01-01" @default.
- W2337087995 modified "2023-09-27" @default.
- W2337087995 title "Interaction between active volcanoes in Iceland" @default.
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