Submarine volcanoes are common morphological features on certain zones of the ocean floor and seafloor imagery systems (ie: multibeam and backscattering data) are recently playing a key role in providing instrumental data for the correct interpretation of geomorphic processes involved in their genesis and development through time.. We present here a detailed geomorphological map of the Enarete seamount (Aeolian Arc-Tyrrhenian Sea), produced by the interpretation of a high resolution Digital Terrain Model (DTM) obtained by a multi-beam bathymetric survey. The bathymetry has been acquired during the M70 oceanographic cruise, carried out on board the R∖ V Meteor in 2006. The Enarete seamount is located in the westernmost sector of the Aeolian Arc, between other two seamounts: Sisifo (NW) and Eolo (SE). The submarine edifice covers an area of about 160 km2 and rises roughly 2000m from the …

A geomorphological map of the Enarete seamount

Ceramicola S;
2018

Abstract

Submarine volcanoes are common morphological features on certain zones of the ocean floor and seafloor imagery systems (ie: multibeam and backscattering data) are recently playing a key role in providing instrumental data for the correct interpretation of geomorphic processes involved in their genesis and development through time.. We present here a detailed geomorphological map of the Enarete seamount (Aeolian Arc-Tyrrhenian Sea), produced by the interpretation of a high resolution Digital Terrain Model (DTM) obtained by a multi-beam bathymetric survey. The bathymetry has been acquired during the M70 oceanographic cruise, carried out on board the R∖ V Meteor in 2006. The Enarete seamount is located in the westernmost sector of the Aeolian Arc, between other two seamounts: Sisifo (NW) and Eolo (SE). The submarine edifice covers an area of about 160 km2 and rises roughly 2000m from the …
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/20.500.14083/5948
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