Here we report a previously unrecognized deep-seated slump structure and associated surficial mass wasting phenomena which occur off Ischia south-western flank. Recently acquired hydrological and geophysical data lead to identify the morphological features and the internal organization of the failed sediments which spread along the continental slope. The extent of this deep-seated deformations and the deep structural levels involved lead to investigate on the influence played by volcanic processes on slope failure.

Large deep-seated slump structure off Ischia volcanic island, Eastern Tyrrhenian sea (Italy)

Violante C;De Alteriis G;Mazzola S
2012

Abstract

Here we report a previously unrecognized deep-seated slump structure and associated surficial mass wasting phenomena which occur off Ischia south-western flank. Recently acquired hydrological and geophysical data lead to identify the morphological features and the internal organization of the failed sediments which spread along the continental slope. The extent of this deep-seated deformations and the deep structural levels involved lead to investigate on the influence played by volcanic processes on slope failure.
2012
Istituto per l'Ambiente Marino Costiero - IAMC - Sede Napoli
Ischia Island
Slump
Vocanic spreading
Volcano-tectonic uplift
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/336410
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