Daniele Casalbore

Datos Biográficos

ID2738193
NOMBREDaniele Casalbore
NOMBRESDaniele
APELLIDOCasalbore
FIRMACASALBORE D
AFILIACIONESInstitute of Environmental Geology and Geoengineering
ORCID0000-0002-0151-6901
VERIFICADOSí
TOTAL DE OBRAS15
TOTAL DE CITAS0
OBRAS COMO AUTOR15
OBRAS COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN2013
AÑO MÁS RECIENTE DE PUBLICACIÓN2026
ÍNDICE H0

  • Years of land subsidence at Lipari Island (Italy)

    Open AccessMarco Anzidei, Alessandro Bosman et al.ARTICLEQuaternary International2026

  • Geohazard features of the Eastern Sicily

    Open AccessFrancesco Latino Chiocci, Andrea Argnani et al.ARTICLEJournal of Maps2025

    Eastern Sicily is characterised by fast tectonic uplift, intricate GPS-derived velocity fields, and significant seismic activity. Mount Etna, the largest subaerial active volcano in Europe, dominates the landscape, influencing the development of large-scale instability processes on the facing continental margin. South of Etna, the Malta Escarpment discloses crustal thinning, with active tectonics, extensional faults, and half grabens. Indications…

  • Geohazard features of the north-western Sicily and Pantelleria

    Open AccessAttilio Sulli, Marilena Calarco et al.ARTICLEJournal of Maps2024

    We present maps of geohazard features identified across north-western Sicily and Pantelleria in the framework of the Magic project (MArine Geohazard along Italian Coasts), which involved Italian marine geological researchers in 2007-2013. These seafloor features were recognized using high-resolution bathymetry data and rely on the morphological expression of the seafloor and shallow sub-surface processes. The north-western Sicily is a complex con…

  • Geohazard features of the Gulf of Taranto

    Open AccessSilvia Ceramicola, Maria Rosaria Senatore et al.ARTICLEJournal of Maps2024

    Here, we explore the complex seabed morphologies of the Gulf of Taranto in southern Italy including their connection to the geodynamic evolution of the region that began during the Neogene period when the Adria plate started subducting beneath the retreating Calabrian arc. We compiled the first Maps of the Geohazard Features of the Gulf of Taranto through comprehensive and collaborative high-resolution seabed surveys, integrating regional high-re…

  • Geohazard features of the Gulf of Naples and Pontine Islands (Eastern Tyrrhenian Sea)

    Open AccessFrancesca Budillon, E Martorelli et al.ARTICLEJournal of Maps2024

    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 t…

  • Geohazard features of the Tyrrhenian Calabria

    Open AccessDaniele Casalbore, Alessandro Conforti et al.ARTICLEJournal of Maps2024

    This paper accompanies the Maps of Geohazard features of the Cilento and the Calabro-Tyrrhenian continental margin in the southern Tyrrhenian Sea (Italy). The main geohazard-related features were derived from extensive seafloor mapping through the collection of high-resolution multibeam data acquired during several oceanographic cruises. They encompass many fluids seepage features, fault scarps, landslides scars, gullies, channels, and canyons. H…

  • Geohazard features of the Aeolian Island slopes and the North-Eastern Sicily offshore

    Open AccessFabiano Gamberi, Daniele Casalbore et al.ARTICLEJournal of Maps2024

    The MaGIC project (Marine Geohazard along the Italian Coasts) had the aim of mapping the geohazard in the Italian seas and resulted in the production of numerous maps covering parts of the Italian Seas. In this paper, we present the maps: ‘The submerged portions of the Aeolian volcanic islands and the north-eastern Sicilian margin’, located in the south-eastern Tyrrhenian Sea. Both areas are affected by active geological processes, which represen…

  • Morphology of the submerged Ferdinandea Island, the ‘Neverland’ of the Sicily Channel (central Mediterranean Sea)

    Open AccessDaniele Spatola, Attilio Sulli et al.ARTICLEJournal of Maps2023

    We present the bathy-morphological map at a scale of 1: 50,000 of the area around the submerged Ferdinandea Island, the ‘Neverland’ of the Sicily Channel (central Mediterranean Sea). We investigate an area of 100 km2, between 10 and 350 m, which is part of a triangular morphological high, 360 km2 wide, representing the SE-wards prolongation of the Adventure Bank. The study is based on the morphometric analysis based on high resolution multibeam, …

  • Seafloor characterisation of the offshore sector around Scoglio d’Affrica islet (Tuscan Archipelago, northern Tyrrhenian sea)

    Open AccessDaniele Spatola, Daniele Casalbore et al.ARTICLEJournal of Maps2023

    We present a very high-resolution bathy-morphological map of the offshore sector around the Scoglio d’Affrica islet (northern Tyrrhenian Sea, Italy). The study area covers a sector of 45 km2, between 3 and 85 m depth. Its central part, i.e. the apex of the Ridge, is characterised by a flat or gently sloping seafloor, where three mud volcanoes, and 250 pockmarks are recognised. Differently, the western and eastern Ridge flanks are steeper and char…

  • The key role of canyons in funnelling litter to the deep sea

    Open AccessMartina Pierdomenico, Daniele Casalbore et al.ARTICLEAnthropocene2020Referencias: 60

  • Quaternary coastal and marine studies in Central Mediterranean

    Open AccessFabrizio Antonioli, Marco Anzidei et al.ARTICLEQuaternary International2017

  • Morphology of Salina offshore (Southern Tyrrhenian Sea)

    Open AccessDaniele Casalbore, Alessandro Bosman et al.ARTICLEJournal of Maps2016

    In this paper, we present the first complete morphological map of the Salina offshore at a scale of 1:100,000. The submarine flanks of the Salina edifice extend down to −650 to −1300 m, are steep and characterized by an uneven morphology due to the presence of volcanic and erosive-depositional features. The volcanic features cover ∼30% of the submarine portion and include volcanic cones and bedrock outcrops. The remaining ∼70% is affected by a wi…

  • Morphology of Lipari offshore (Southern Tyrrhenian Sea)

    Open AccessDaniele Casalbore, Alessandro Bosman et al.ARTICLEJournal of Maps2016

    High-resolution multibeam bathymetry was recently collected around Lipari, the largest and most densely populated island of the Aeolian Archipelago (Southern Tyrrhenian Sea). The data were acquired within the context of marine geological studies performed in the area over the last 10 years. We present the first detailed morphological map of the Lipari offshore at 1:100,000 scale (Main Map). A rugged morphology characterizes the submarine portions…

  • New insights on the subsidence of Lipari island (Aeolian islands, southern Italy) from the submerged Roman age pier at Marina Lunga

    Open AccessMarco Anzidei, Alessandro Bosman et al.ARTICLEQuaternary International2016

  • Bathy-morphological setting of Terceira Island (Azores) after the Faivi cruise

    Open AccessFrancesco Latino Chiocci, Claudia Romagnoli et al.ARTICLEJournal of Maps2013

    High-resolution morpho-bathymetric data at 1:200,000 scale obtained during the FAIVI cruise (2011) and the resulting geomorphologic map of the Terceira island offshore area (central Azores, Portugal) are presented for the first time. The uneven morphology around Terceira is primarily related to volcanic features, such as linear and cone-shaped eruptive centres and lava flows. Such features are mostly concentrated on volcanic ridges and are aligne…