
Marco AnzideiNational Institute of Geophysics and Volcanology | INGV
Marco Anzidei
Geology, PhD
About
233
Publications
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6,337
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Citations since 2017
Introduction
Degree in Geology (University Sapienza, Italy); PhD in physics of the complex systems (University of Calabria, Italy). Senior Researcher at INGV. Teaching experience in national and foreign Universities. Board member of AIQUA, Earth Space Technology and RING network. Editor of scientific Journals. Author of about 170 publications. Research skills: i) GPS; ii) sea level; iii) topography.
Author of 3 videos on the Mediterranean.
Leader of the EU DG-ECHO Projects -SAVEMEDCOASTS and SAVEMEDCOASTS-2
Additional affiliations
October 2004 - September 2012
February 1987 - present
February 1987 - present
Education
July 1984
Publications
Publications (233)
Extreme events are becoming more frequent due to anthropogenic climate change, posing serious concerns on societal and economic impacts and asking for mitigating strategies, as for Venice. Here we proposed a dynamical diagnostic of Extreme Sea Level (ESL) events in the Venice lagoon by using two indicators based on combining extreme value theory an...
Unlabelled:
The coasts of the Mediterranean basin are exposed to the ongoing effects of climate change and anthropogenic pressure. Low elevated coastal plains, river deltas, lagoons and reclamation areas are experiencing beach retreat, coastal erosion and marine flooding. This makes them particularly vulnerable to sea level rise (SLR), which is ex...
Low-lying coastal zones are highly subject to coastal hazards as a result of sea-level rise enhanced by natural or anthropogenic land subsidence. A combined analysis using sea-level data and remote sensing techniques allows the estimation of the current rates of land subsidence and shoreline retreat, supporting the development of quantified relativ...
Lipari is the largest and most populated island in the Aeolian Archipelago, a UNESCO site, and a highly frequented touristic destination. As in many other insular settings, the low-lying coastal stretches in the E and NE sectors of Lipari are locally exposed to coastal erosion and flooding, enhanced by subsidence effects leading to local sea level...
Analysis of high-resolution seismic profiles integrated with archaeological data along the coast has allowed quantifying the last ∼10 ka BP displacements in the offshore part of the Campi Flegrei resurgent caldera, one of the world's highest-risk volcanic areas. Previous onland studies revealed that, following the Neapolitan Yellow Tuff (NYT) erupt...
Since 2012 the Geoswim programme has been investigating coastal landforms along the Mediterranean rocky shores and their lateral variations, through snorkelling and field surveys. The focus of Geoswim investigation is collecting physical/chemical and ecological data relevant to the evaluation of past to future sea level changes. In spring 2017 we e...
The island of Paros is undergoing to a continuous submergence, caused by the combination of land subsidence and sea level rise that are continuously shaping its coasts. From low elevation aerial photogrammetric surveys and climatic data from the IPCC, we attempted a sea level rise scenario for the bay of Paroikia for AD 2050 and 2100. Thanks to the...
The global sea-level rise (SLR) projections for the next few decades are the basis for
developing flooding maps that depict the expected hazard scenarios. However, the spatially variable land subsidence has generally not been considered in the current projections. In this study, we use geodetic data from global navigation satellite system (GNSS), s...
The RETRACE-3D project (centRal italy EarThquakes integRAted Crustal model) focused on the revision of all the available geological and geophysical data in the area interested by the 2016-2018 seismic sequence of central Italy, with the final aim to reconstruct a reliable and consistent 3D geological model of that area. It is based on a collaborati...
The coasts of the Mediterranean Sea are dynamic habitats in which human activities have been conducted for centuries and which feature micro-tidal environments with about 0.40 m of range. For this reason, human settlements are still concentrated along a narrow coastline strip, where any change in the sea level and coastal dynamics may impact anthro...
The dynamics of the sandy coast between Castellaneta and Taranto (Southern Italy) has been influenced by many natural and anthropogenic factors, resulting in significant changes in the coastal system over the last century. The interactions between vertical components of sea-level changes and horizontal components of the sedimentary budget, in combi...
Sea level rise is one of the main risk factors for the preservation of cultural heritage sites located along the coasts of the Mediterranean basin. Coastal retreat, erosion, and storm surges are posing serious threats to archaeological and historical structures built along the coastal zones of this region. In order to assess the coastal changes by...
In the engineering geology field increased attention has been posed in recent years to potential liquefaction mitigation interventions in susceptible sand formations. In silty sands this is a major challenge because, as the fines content increases, vibratory methods for densification become progressively less effective. An alternative mitigation te...
Sea level rise is one of the main factor of risk for the preservation of cultural heritage sites located along the coasts of the Mediterranean basin. Coastal retreat, erosion and storm surges are yet posing serious threats to archaeological and historical structures built along the coastal zones of this region. In order to assess the coastal change...
We present a geomorphological, stratigraphical and geochronological study reconstructing a suite of paleo-surfaces in a 200 km-long coastal sector of the central Tyrrhenian Sea between Argentario and Circeo promontories. Identification of the near-shore deposits associated with these paleo-surfaces allow us to define corresponding marine terraces a...
In this study, we analyze the impact of the sea level rise induced by climate change on the coastal cultural heritage site of Motya, the Phoenician colony (IV–III millennium B.P.) located in the San Pantaleo island, NW corner of Sicily (southern Italy). In particular, we assessed the effects of this phenomenon on the human settlement in the past 24...
We analyzed a set of geodetic data to investigate the contribution of local factors, namely the sea level natural variability (SLNV) and the vertical land motion (VLM), to the sea-level trend. The SLNV is analyzed through the Empirical Mode Decomposition (EMD) on tidal data (>60 years of recordings) and results are used to evaluate its effects on s...
The recent high-resolution multibeam bathymetry surveys around Lipari Island allowed to evidence several submarine canyons, whose head often cut back up to very shallow water and at a few tens of meters far from the coast. These canyons are mainly located in the eastern and southern side of the island and are characterized by an ongoing retrogressi...
We report detailed morphometric observations on several MIS 5.5 and a few older (MIS 11, 21, 25) fossil tidal notches shaped along carbonate coasts at 80 sites in the central Mediterranean Sea and at an additional six sites in the eastern and western Mediterranean. At each site, we performed precise measurements of the fossil tidal notch (FTN) widt...
Submerged caves represent potential archives of speleothems with continental and marine biogenic layers. In turn, these can be used to reconstruct relative sea-level changes. This study presents new data on the tectonic behaviour of the island of Malta during the Holocene. These data were obtained from a speleothem sampled, during an underwater sur...
Following the pioneering work of Schmiedt et al. (1972) on establishing the level of the Tyrrhenian Sea in Antiquity, a number of studies have examined this evidence from Roman Period fish tanks but with significantly different outcomes due primarily to different interpretations of the functional level of these pools at the time of their constructi...
The coastal area of southeastern Sicily (Italy) is undergoing weak
land subsidence, heavy coastal retreat, land flooding and exposed to severe
storms associated with high-waves, also in consequence of the global
sea level rise, which is expected to raise even more that 1 m by 2100
AD depending on different estimates. This value will be even larger...
The volcanic island of Lipari belongs to the Aeolian archipelago (Southern Tyrrhenian Sea, Italy), which is an active volcanic arc of the Mediterranean basin. This region has been inhabited since Neolithic and particularly the coasts of Lipari, which is the largest island of the archipelago, have been continuously settled from the Greek period unti...
The coastal areas of the central Mediterranean Sea are sensitive to climate change and the consequent relative sea level rise. Both phenomena may affect densely urbanized and populated areas, causing severe damages.
Our maps show the land-marine flooding projections as effects of the expected relative sea
level rise for four Italian coastal plains...
Soil liquefaction can result in significant settlement and reduction of load-bearing capacity. Moreover, the generation of pore pressure during an earthquake and its post-seismic dissipation can generate permanent deformations and settlements. The quantitative evaluation of post-liquefaction settlements is of extreme importance for engineering purp...
This article reviews and discusses key data, literature, debates and discussions focussed on relative sea-level change since the Last Interglacial (approximately last ~132,000 years) in the Mediterranean Basin. Special reference is given to the geomorphological (physical and environmental) and archaeological (human and cultural) aspects of central...
We investigate a large geodetic dataset of InSAR and GPS measurements to determine the source parameters for the three mainshocks of the 2016 Central Italy earthquake sequence on 24th August, 26th and 30th October (MW 6.1, 5.9 and 6.5, respectively). Our preferred model is consistent with the activation of four main coseismic asperities belonging t...
Central Mediterranean shelves show a large variability in morphology (width, slope, unevenness), stratigraphy (different thickness of depositional bodies resulting from the last climatic/eustatic cycle) and sedimentology (shelf-mud offshore of the main river mouths, bioclastic sediment in under-supplied areas) because of their geologically young ag...
We investigated archaeological sites located along the coasts of central Apulia (Italy) to estimate the relative sea level changes which have occurred in this region since the Bronze Age, and test the most recent model of predicted sea level for this region. Surveys focused on six sites located on both the Adriatic and Ionian coasts of Apulia at th...
The coast of the Mediterranean provide several remnants of ancient coastal quarries, which are now useful to study sea level change occurring during the last millennia. Millstones quarries were exploited with same quarrying techniques from rocks like beachrocks, sandstones or similar lithologies, were shaped to be suitable to grind olives, seeds an...
We present a full 3-D velocity field of the Earth’s surface in the Euro-Mediterranean
area obtained from a combination of three different velocity solutions
computed at the Centro Nazionale Terremoti (CNT) of the Istituto Nazionale
di Geofisica e Vulcanologia (INGV). All the publicly available GPS data since
1993, have been fully reprocessed by thr...
We present and discuss the genesis, age and evolution of indented landforms carved at sea level in correspondence of carbonatic headlands in three sites of the central Mediterranean coasts, between Marseille (France) and Balzi Rossi (Italy), the island of Tavolara (Sardinia, Italy) and the promontory of Tindari (Sicily, Italy). The shape of these a...
Abstract We depict the relative sea-level rise scenarios for the year 2100 from four areas of the Italian peninsula. Our estimates are based on the Rahmstorf (2007) and IPCC-AR5 reports 2013 for the RCP-8.5 scenarios (www.ipcc.ch) of climate change, adjusted for the rates of vertical land movements (isostasy and tectonics). These latter are inferre...
On August 24, 2016, a ML 6.0 earthquake struck the Central Apennines between the towns of Amatrice and Norcia, causing extensive damage to the town of Amatrice and several surroundings villages, and killing 297 inhabitants. The main shock nucleated at a depth of about 7-8 km and was followed by a vigorous aftershock sequence southeast and northwest...
We used continuous Global Positioning System (GPS) measurements to infer the fault geometry and the amount of coseismic slip associated to the August 24, 2016 Mw 6 Amatrice earthquake. We realized a three dimensional coseismic displacement field by combining different geodetic solutions generated by three independent analyses of the raw GPS observa...
Archaeological and instrumental data indicate that the southern sector of the volcanic island of Lipari has been subsiding for the last 2100 years due to isostatic and tectonic factors, at variable rates of up to ~11 mm/yr. Based on this data, a detailed marine flooding scenario for 2100 A.D. is provided for the bay of Marina Lunga in the eastern p...
We present and discuss data from petrographic observation at the optical microscope, electron microprobe analyses on selected glass shards, and trace-element analyses on 14 mortar aggregates collected at the ancient harbors and other maritime structures of Latium and Campania, spanning the third century BCE through the second CE, aimed at identify...
The availability of very high resolution Digital Elevation Models (DEM), represent a main tool for hazards analysis and landscape morphology evolution. During the past years DEMs have been traditionally generated by aerial photogrammetric surveys from aircrafts, providing accurate results by at high costs. The recent developments of ultra-light Unm...
We present and discuss the genesis, age and evolution of indented landforms carved at sea level in correspondence of carbonatic headlands in three sites of the central Mediterranean coasts, between Marseille (France) and Balzi Rossi (Italy), the island of Tavolara (Sardinia, Italy) and the promontory of Tindari (Sicily, Italy). These landforms can...
The availability of very high resolution Digital Elevation Models (DEM), represent a main tool for hazards analysis and landscape morphology evolution. During the past years DEMs have been traditionally generated by aerial photogrammetric surveys from aircrafts, providing accurate results by at high costs. The recent developments of ultra-light Unm...
Recently acquired geochronological and stratigraphic data provide new information on the sedimentary successions deposited by the Paleo-Tiber River in the coastal and near-coastal area of Rome in consequence of the glacio-eustatic changes, allowing to better define their inner geometry and palaeogeographic spatial distribution. In the present work...
Geomorphological survey along the coasts of Crete revealed widespread evidence of uplifted and submerged tidal notches, different phases of beachrock formation, and many relics of ancient coastal constructions. About 1.6 ka BP, when the sea level was at −1.25 ± 0.05 m, the western tectonic block of the island uplifted by 9.15 ± 0.20 m in its wester...
The Structure-from-Motion photogrammetry (SfM) allows a fast and easy data acquisition and a highly automated data processing, leading to accurate photorealistic point clouds. The results of a SfM-based modeling of the coastal zone of Monterosso a Mare (Eastern Liguria, Italy) are shown here. Four photogrammetric surveys of the area were carried ou...
The Mediterranean basin is an important area of the Earth for studying the interplay between geodynamic processes and landscape evolution affected by tectonic, glacio-hydro-isostatic and eustatic factors. We focus on determining vertical deformations and relative sea-level change of the coastal zone utilizing geological, archaeological, historical...
The maritime archaeological indicators play a crucial role for the reconstruction of past relative sea levels in the Mediterranean basin, filling the gap between geology and modern instrumental data. During the last decades several studies have presented different estimates of the relative sea level change in same locations using these indicators....
Since the early 1970s, geodetic networks became a most important tool to monitor the present day deformations of the volcanic arc of the Aeolian Islands. The first benchmarks were installed in this region at Lipari and Vulcano Islands and the number of GPS benchmarks increased in time since the early '90s. These networks were periodically surveyed...