Abstract
ABSTRACT In this paper, we describe the geohazard-related elements of the Eastern Tyrrhenian Sea continental margin, situated between the 40° and 41° North latitude. These features were recognised principally through morphological analysis. The investigation utilized medium – and high-resolution digital models of the submarine landscape, produced within the framework of the Magic project (Marine Geohazard along Italian Coasts), and primarily focusing on the bathymetric range of 50–700 meters. The surveyed area encompasses a recently formed continental margin, which connects the internal segments of the Apennine fold-and-thrust belt, verging NE, to the Tyrrhenian Sea bathyal plain, a 3000-m-deep back-arc basin that has developed since the Middle-Late Miocene. Several classes of hazard-related elements have been identified offshore, primarily associated with high-gradient slopes and a large number of volcanic edifices and banks. These include canyon systems, erosive scarps, landslide complexes, fault – and volcanic-related features, such as the products of the volcanic edifices instability, which claim to varying degrees of geo-hazard. Additionally, bedforms, fluid seepages and creeping phenomena in the prodelta slopes suggest high morpho-tectonic and environmental dynamics. Highlights This article reports on the thematic maps developed along the Lazio – Campania offshore (Central-eastern Tyrrhenian Sea, Italy) within the framework of the Magic Project, based on geomorphological analysis of the HR Digital Elevation Model of the seafloor. Several classes of hazard-related elements have been identified offshore, mainly associated with high-gradient slopes, volcanic activity and intense morphodynamic processes. The entire suite of maps created in the context of the Magic Project serves as a valuable base of knowledge, extending to the national scale and benchmarks for future monitoring of critical sites and geo-hazard-related features, as well as for maritime spatial planning actions.
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