We present a seafloor map of the summit of Palinuro Seamount, an E-W elongated volcanic ridge located in the Eastern Tyrrhenian Sea. The seafloor was mapped using multibeam backscatter and seafloor samples collected between 80 and 1000 m below the sea level. The high resolution imaging of the Palinuro seafloor was obtained by merging a Digital Terrain Model with a 2.5 m sized grid and a backscatter mosaic with 2.5 m pixel. The resulting 1:20.000 scale map includes six main facies recognized on the basis of their backscatter properties. These six facies reflect different lithologies. The Palinuro seafloor map represents a useful tool for morphological and geological studies of the Palinuro volcanic ridge.

Seafloor mapping using high-resolution multibeam backscatter: the Palinuro Seamount (Eastern Tyrrhenian Sea)

Sara Innangi;Salvatore Passaro;Renato Tonielli;Stella Tamburrino
2015

Abstract

We present a seafloor map of the summit of Palinuro Seamount, an E-W elongated volcanic ridge located in the Eastern Tyrrhenian Sea. The seafloor was mapped using multibeam backscatter and seafloor samples collected between 80 and 1000 m below the sea level. The high resolution imaging of the Palinuro seafloor was obtained by merging a Digital Terrain Model with a 2.5 m sized grid and a backscatter mosaic with 2.5 m pixel. The resulting 1:20.000 scale map includes six main facies recognized on the basis of their backscatter properties. These six facies reflect different lithologies. The Palinuro seafloor map represents a useful tool for morphological and geological studies of the Palinuro volcanic ridge.
2015
Istituto di Scienze Marine - ISMAR
Seafloor mapping; multibeam backscatter; volcanic seamount; Palinuro volcano
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/291488
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