3D numerical deformation model of the intrusive event forerunning the 2001 Etna eruption
نویسندگان
چکیده
منابع مشابه
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We report the direct observation of a peculiar lava channel that was formed near the base of a parasitic cone during the 2001 eruption on Mount Etna. Erosive processes by flowing lava are commonly attributed to thermal erosion. However, field evidence strongly suggests that models of thermal erosion cannot explain the formation of this channel. Here, we put forward the idea that the essential e...
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Most flank eruptions within a central stratovolcano are triggered by lateral draining of magma from its central conduit, and only few eruptions appear to be independent of the central conduit. In order to better highlight the dynamics of flank eruptions in a central stratovolcano, we review the eruptive history of Etna over the last 100 years. In particular, we take into consideration the Mount...
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ژورنال
عنوان ژورنال: Physics of the Earth and Planetary Interiors
سال: 2008
ISSN: 0031-9201
DOI: 10.1016/j.pepi.2008.05.004