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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Physical geography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (291 pages)
    Edition: 1st ed.
    ISBN: 9783319339405
    DDC: 551.468091638
    Language: English
    Note: Intro -- Contents -- Introduction to the Atlas -- Bedform Analysis and Main Physical Processes -- 1 Bedform Mapping: Multibeam Data Processing, Metadata and Spatial Data Services -- Abstract -- 1.1 Introduction: Multibeam Data Processing -- 1.2 Metadata -- 1.3 Spatial Data Services -- 1.4 The INSPIRE Directive -- 1.5 Conclusions -- References -- 2 Methods for Analysing Bedform Geometry and Dynamics -- Abstract -- 2.1 Introduction -- 2.2 Review of Methods -- 2.2.1 Bedform Orientation and Wavelength -- 2.2.2 Superimposed Bedforms and Identification of Crests and Troughs -- 2.2.3 Bedform Dynamics -- 2.3 Discussion -- 2.4 Conclusions -- Acknowledgments -- References -- 3 Principles of Physical Modelling of Bedforms Under Waves and Currents -- Abstract -- 3.1 Introduction -- 3.2 Physical Modelling in Three Steps -- 3.3 Two Simple Cases -- 3.4 Concluding Remarks -- Acknowledgments -- References -- 4 Modelling Bedforms on the Continental Shelf -- Abstract -- 4.1 Introduction -- 4.2 Tidal Sand Waves -- 4.3 Tidal Sand Banks -- 4.4 Long Bed Waves -- 4.5 Shoreface-Connected Sand Ridges -- 4.6 Future Perspectives -- Acknowledgements -- References -- 5 Internal Waves and Bedforms -- Abstract -- 5.1 Introduction -- 5.2 Internal Wave Impact on Sediment -- 5.3 Observational Setup -- 5.4 Discussion -- References -- 6 Turbidity Current Bedforms -- Abstract -- 6.1 Turbidity Current Bedforms -- 6.2 Bedform Stability Diagram for Turbidity Currents -- 6.3 Discussion -- References -- 7 Dense Shelf Water Cascading and Associated Bedforms -- Abstract -- 7.1 Introduction -- 7.2 Dense Shelf Water Cascading in the Western Mediterranean -- References -- 8 Currents in the Western Mediterranean Basin -- Abstract -- 8.1 Introduction -- 8.2 The Mediterranean Basin -- 8.3 Methods and Observations -- 8.4 Surface Circulation -- 8.5 Intermediate Circulation -- 8.6 Deep Circulation. , Acknowledgments -- References -- Bedforms in the Coastal Zone -- 9 Bedforms as Self-organized Patterns -- Abstract -- 9.1 Introduction -- 9.2 Forced or Self-organized Response? -- References -- 10 Beach Cusps -- Abstract -- 10.1 Introduction -- 10.2 Modelling Beach Cusp Formation -- Bibliography -- 11 Km-Scale Shoreline Sand Waves -- Abstract -- 11.1 Shoreline Undulations -- 11.2 Km-Scale Shoreline Sand Waves -- 11.3 Self-organized Origin and Evolution -- Acknowledgments -- References -- 12 KM-Scale Shoreline Sand Waves In The Western Mediterranean Sea -- Abstract -- 12.1 Introduction -- 12.2 Open Coasts -- 12.3 Deltas -- 12.4 Sheltered Shores -- Acknowledgments -- References -- 13 Nearshore Sand Bars -- Abstract -- 13.1 Motivation -- 13.2 Classification and Morphological Characteristics and Dynamics -- 13.2.1 Shore-Parallel Bars (Straight or Crescentic) -- 13.2.2 Transverse Bars -- 13.3 Physical Processes for Their Development and Dynamics -- 13.3.1 Shore-Parallel Straight Bars -- 13.3.2 Crescentic Bars and Transverse TBR Bars (Type 1) -- 13.3.3 Transverse Medium-Energy Finger Bars (Type 2) -- 13.3.4 Transverse Low-Energy and Large-Scale Finger Bars (Types 3 and 4) -- Acknowledgments -- References -- 14 Nearshore Sand Bars on Western Mediterranean Beaches -- Abstract -- 14.1 Introduction -- 14.2 Observations of Nearshore Sand Bars in the Western Gulf of Lions, France -- 14.3 Observations of Nearshore Sand Bars on Catalan Beaches, Spain -- 14.3.1 Ebro Delta -- 14.3.2 Llobregat Delta (Barcelona and Castelldefels) -- 14.4 Summary and Comparison with Nearshore Bars on Other Coasts -- Acknowledgments -- References -- 15 Contemporary Subaqueous Dune Field Development Over an Abandoned River Mouth (Ebro Delta) -- Abstract -- 15.1 Introduction -- 15.2 General Setting -- 15.3 Data Collection -- 15.4 Results and Discussion -- 15.5 Conclusions. , Acknowledgments -- References -- 16 Bedforms on the Lowermost Reach of the Tiber River (Rome, Italy): Preliminary Results from Integrated Geophysical Surveys and Samplings -- Abstract -- 16.1 Introduction -- 16.2 Methods -- 16.3 Results -- 16.4 Final Remarks -- Acknowledgments -- References -- Bedforms in Prodeltas and Sorted Bedforms -- 17 Holocene Muddy Bedforms on the Llobregat River Prodelta Wedge -- Abstract -- 17.1 Introduction-Study Area -- 17.2 Methods -- 17.3 Results-Discussion -- 17.4 Conclusions -- Acknowledgments -- References -- 18 Prodeltaic Undulations and Hyperpycnal Flows (I): Morphological Observations -- Abstract -- 18.1 Introduction -- 18.2 Sediment Supply of Short, Mountainous Rivers -- 18.3 Morphological Observations -- 18.4 Diagnostic Morphological Criteria Compatible with Hyperpycnal Flow Genesis -- Acknowledgments -- References -- 19 Prodeltaic Undulations and Hyperpycnal Flows (II): Evolutionary Trends -- Abstract -- 19.1 Introduction -- 19.2 Holocene Prodeltaic Wedges in the Mediterranean Sea -- 19.3 Evidence of Progressive Undulation Development -- 19.4 Evolutionary Trends Compatible with Sediment Flow Activity -- Acknowledgments -- References -- 20 Sorted Bedforms Along the Egadi Islands Continental Shelf (Southern Tyrrhenian) -- Abstract -- 20.1 Introduction-Study Area -- 20.2 Methods -- 20.3 Results-Discussion -- 20.4 Conclusions -- Acknowledgments -- References -- 21 Sorted Bedforms Developed on Sandy Deposits Derived from Small Ephemeral Streams (Catalan Continental Shelf) -- Abstract -- 21.1 Introduction -- 21.2 Methods -- 21.3 Results -- 21.4 Discussion and Conclusions -- Acknowledgments -- References -- 22 Dynamics of Sorted Bedforms on a Shallow Infralittoral Prograding Wedge Influenced by Dredging (El Masnou, NW Mediterranean) -- Abstract -- 22.1 Introduction -- 22.2 Methods -- 22.3 Results. , 22.3.1 Sorted Bedform Characteristics -- 22.3.2 Short-Term Bedform Evolution -- 22.4 Discussion and Conclusions -- Acknowledgments -- References -- 23 Sorted Bedforms Along the Continental Shelf of Western Sardinia -- Abstract -- 23.1 Introduction -- 23.2 Methods -- 23.3 Results -- 23.4 Discussion and Conclusions -- Acknowledgments -- References -- Bedforms in the Continental Shelf -- 24 Sedimentary Bedforms in the Menorca Channel Region, Balearic Islands (Western Mediterranean) -- Abstract -- 24.1 Study Area -- 24.2 Methods -- 24.3 Results and Discussion -- Acknowledgments -- References -- 25 Dome Dunes on the Inner to Middle Shelf Transition on a Temperate-Water Carbonate Sediment Shelf. Pitiusas Islands -- Abstract -- 25.1 Introduction -- 25.2 Methods -- 25.3 Results -- 25.4 Discussion and Conclusions -- Bibliography -- 26 Trawl Marks and Dredge Spoils as Examples of Seabed Anthropic Alteration on Sediments (Menorca Shelf) -- Abstract -- 26.1 Introduction -- 26.2 Methods -- 26.3 Results -- 26.3.1 Trawl Marks -- 26.3.2 Dumping of Dredged Sediment -- 26.4 Discussion and Conclusions -- Acknowledgments -- Bibliography -- 27 Sand Ridges on the Mid-Outer Valencia Continental Shelf -- Abstract -- 27.1 Introduction, Study Area and Methods -- 27.2 Results and Discussion -- 27.3 Conclusions -- Acknowledgments -- References -- 28 Subaqueous Dune Fields on the Marine Protected Area Around the Cabrera Archipelago (Balearic Islands) -- Abstract -- 28.1 Introduction -- 28.2 Methods -- 28.3 Results -- 28.3.1 The Northern Dune Field (Na Foradada Island) -- 28.3.2 The Eastern Dune Field (Sa Conills and Na Redona Islands) -- 28.3.3 The Southern Dune Field (Es Estells islands) -- 28.4 Discussion and Concluding Remarks -- Acknowledgments -- References -- 29 Subaqueous Dunes Over Sand Ridges on the Murcia Outer Shelf -- Abstract -- 29.1 Introduction -- 29.2 Methods. , 29.3 Results -- 29.3.1 Sand Ridges -- 29.3.2 Subaqueous Dunes -- 29.4 Discussion and Conclusions -- Acknowledgments -- References -- Bedforms and Benthos -- 30 Bedforms as Benthic Habitats: Living on the Edge, Chaos, Order and Complexity -- Abstract -- 30.1 Study Area -- 30.2 Methodology -- 30.3 Results -- Acknowledgments -- References -- 31 Benthic Communities on Shallow Sedimentary Bottoms in the Western Mediterranean -- Abstract -- 31.1 Introduction -- 31.2 Benthic Communities -- 31.2.1 Very Coarse Bottoms -- 31.2.2 Sandy Bottoms -- 31.2.3 Fine-Grained Bottoms -- 31.2.4 Meadows -- 31.2.5 Maërl Beds -- 31.3 Concluding Remarks -- References -- 32 Characterization of Benthic Communities in a Subaqueous Dune Field on the Continental Shelf (Mar Menor, Western Mediterranean) -- Abstract -- 32.1 Introduction -- 32.2 Methods -- 32.3 Results -- 32.3.1 Subaqueous Dunes -- 32.3.2 Habitat Types and Benthic Communities -- 32.3.2.1 The Maërl Community -- 32.3.2.2 The Transition Community -- 32.3.2.3 The Fine-Sediment Community -- 32.4 Concluding Remarks -- Acknowledgments -- References -- 33 Bio and Anthropogenic Disturbance of Maërl Communities Settled on Subaqueous Dunes on the Mar Menor Continental Shelf (Western Mediterranean) -- Abstract -- 33.1 Introduction -- 33.2 Maërl Beds -- 33.3 Biogenic Disturbance -- 33.4 Anthropogenic Disturbance -- 33.5 Concluding Remarks -- Acknowledgments -- References -- Beforms in Submarine Canyons -- 34 Bedforms in the Southern Submarine Canyons of the Balearic Islands (Western Mediterranean) Interpreted as Cyclic Steps -- Abstract -- 34.1 Introduction -- 34.2 Methods -- 34.3 Results-Discussion -- 34.4 Conclusions -- Acknowledgments -- References -- 35 Cyclic Steps at the Head of Channelized Features Along the Calabrian Margin (Southern Tyrrhenian Sea, Italy) -- Abstract -- 35.1 Introduction and Study Area -- 35.2 Methods. , 35.3 Results and Discussion.
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  • 2
    Type of Medium: Book
    Pages: 100 pages
    ISBN: 9789464206111
    Series Statement: European Marine Board Position Paper 26
    Language: English
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  • 3
    Type of Medium: Book
    Pages: 171 S. , Ill., graph. Darst.
    ISBN: 9789492043030
    Series Statement: European Marine Board Position Paper 21
    Language: English
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  • 4
    Publication Date: 2021-05-11
    Description: Highlights: - Analysis of a combined new high-resolution 2D seismic and bathymetric data set offshore Mt Etna - Extensional domains are mapped at the shallow subsurface of the continental margin - Compressional structures are mapped at the toe of the continental margin - A coupled volcano edifice / continental margin instability is proposed Mount Etna is the largest active volcano in Europe. Instability of its eastern flank is well documented onshore, and continuously monitored by geodetic and InSAR measurements. Little is known, however, about the offshore extension of the eastern volcano flank, defining a serious shortcoming in stability models. In order to better constrain the active tectonics of the continental margin offshore the eastern flank of the volcano, we acquired a new high-resolution 2D reflection seismic dataset. The data provide new insights into the heterogeneous geology and tectonics at the continental margin offshore Mt Etna. The submarine realm is characterized by different blocks, which are controlled by local- and regional tectonics. A compressional regime is found at the toe of the continental margin, which is bound to a complex basin system. Both, the clear link between on- and offshore tectonic structures as well as the compressional regime at the easternmost flank edge, indicate a continental margin gravitational collapse as well as spreading to be present at Mt Etna. Moreover, we find evidence for the offshore southern boundary of the moving flank, which is identified as a right lateral oblique fault north of Catania Canyon. Our findings suggest a coupled volcano edifice / continental margin instability at Mt Etna, demonstrating first order linkage between on- and offshore tectonic processes.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 5
    Publication Date: 2021-05-11
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 6
    Publication Date: 2015-12-17
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 7
    Publication Date: 2011-12-01
    Description: Multibeam bathymetry and high-resolution seismic profiles depict in detail the characteristics of submarine gullies present in the upper continental slope offshore of the mouths of the Tiber and Volturno Rivers in the Tyrrhenian Sea and the Simeto River in the Ionian Sea. Upper slope gullies are interpreted as depositional features, growing because of faster aggradation on intergully areas with respect to their axes. The dispersal of river-flood sediment through plunging of hyperpycnal flows has been interpreted to be the limiting factor in sedimentation in gully axes. However, the generation of hyperpycnal flows requires a sediment concentration of several tens of kilograms per cubic meter in the river flows to overcome the higher density of seawater. This threshold is difficult to reach in medium-sized rivers (i.e., catchment basin of 500–5000 km2), such as the Tiber and Volturno. Two alternative scenarios of enhanced sediment availability for these rivers have been proposed. The first scenario is related to sea-level fall and lowstand stages, when the climate conditions may have been different and a huge amount of unconsolidated, fine-grained sediment deposited during the previous highstand stage may have been eroded from the river valleys, coastal plain valleys and shelf delta, as suggested in pioneering work of one of the authors (Chiocci) and Bill Normark. This scenario might explain the formation of some of the gullies offshore of the Tiber River mouth, which developed during the last glacial maximum; however, it is unable to explain the gullies within deposits related to transgressive and highstand system tracts, such as offshore of the Simeto and Volturno River mouths. An alternative scenario is thus proposed on the basis of the relationship observed between the studied rivers and the presence of large volcanic edifices in their catchment basins. Explosive volcanic activity could have drastically modified their catchment basins and caused a sudden and large supply of loose tephras, increasing the sediment load in watercourses and consequently favoring the development of gully-forming hyperpycnal flows. The timing of volcanic activity on the three study areas matches, in fact, the presence or absence of gullies in upper slope depositional sequences.
    Electronic ISSN: 1553-040X
    Topics: Geosciences
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  • 8
    Publication Date: 2020-05-26
    Description: The analysis of multibeam bathymetry, seismic profiles, ROV dive and seafloor sampling, integrated with stratigraphic and geological data derived from subaerial field studies, provides information on the multi-stage formation and evolution of La Fossa Caldera at the active volcanic system of Vulcano (Aeolian Islands). The caldera is mostly subaerial and delimited by well-defined rims associated to three different collapse events occurred at about 80, 48–24, and 13–8 ka, respectively. The NE part of the caldera presently lies below the sea-level and is delimited by two partially degraded rim segments, encompassing a depressed and eroded area of approximately 2 km2. We present here further morphological and petrochemical evidence linking the subaerial caldera rims to its submarine counterparts. Particularly, one of the submarine rims can be directly correlated with the subaerial eastern caldera border related to the intermediate (48–24 ka) collapse event. The other submarine rim cannot be directly linked to any subaerial caldera rim, because of the emplacement of the Vulcanello lava platform during the last 2 millennia that interrupts the caldera border. However, morphological interpretation and the trachyte composition of dredged lavas allow us to associate this submarine rim with the younger (13–8 ka) caldera collapse event that truncated the trachyte-rhyolite Monte Lentia dome complex in the NW sector of Vulcano. The diachronicity of the different collapse events forming the La Fossa Caldera can also explain the morpho-structural mismatch of some hundreds of meters between the two submarine caldera rims. A small part of this offset could be also accounted by tectonic displacement along NE–SW trending lineaments breaching and dismantling the submarine portion of the caldera. A network of active erosive gullies, whose headwall arrive up to the coast, is in fact responsible of the marked marine retrogressive erosion affecting the NE part of the caldera, where remnants of intra-caldera volcanic activity are still evident. Submarine morphological features associated to the entrance of subaerial lava flow units into the sea are presented, particularly related to the construction of the La Fossa Cone and Vulcanello. More generally, this study demonstrates the utility of integrated marine and subaerial studies to unravel the volcano-tectonic evolution of active insular volcanoes.
    Description: Published
    Description: 479–492
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Keywords: 04.04. Geology ; 04.08. Volcanology ; 04.02. Exploration geophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2020-05-26
    Description: 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 retrogressive (landward) erosion, that also controlled the shape and the evolution of the coastline. The canyon heads are formed by minor slide scars. By coupling slide scar morphometry and simple numerical model we have been able to roughly estimate the potential tsunami wave amplitudes generated by related slope failures. Moreover, the retrogressive erosion of canyon heads can be claimed as a cause of the enhanced subsidence reported in the last few thousand years in the eastern part of Lipari, where the main villages are located. Based on these evidence, we propose a first assessment of the coastal hazard due to marine retrogressive activity in the largest and most densely populated island of the Aeolian Archipelago
    Description: Published
    Description: 989–999
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Description: JCR Journal
    Keywords: Submarine canyons Slope failure Tsunamigenic potential Coastal retreat Subsidence
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2022-03-07
    Description: Coastal dynamics are the result of several processes controlling the balance between sediment input and output over time. The beach system is not always able to maintain a neutral coastal balance due to natural and anthropogenic causes. We present an integrated marine geology, geomorphological and sea-level rise analysis in the coastal sector between Torre delle Ciavole and Capo Calavà (North-Eastern Sicily, Italy).This sector is characterized by high uplift rates and frequent seismicity (mainly generated by the very active Vulcano-Tindari Fault System), promoting the development of mass-wasting processes in the coastal and offshore sectors. A main erosive feature observed in the area is the head of the Gioiosa Marea submarine canyon, located at some meters of depth, few hundred meters far the coastline. The main morphological features of the canyon were reconstructed through the analysis of high-resolution multibeam data, indicating that the canyon is active, as also testified by the comparison of time-lapse aerial photos. Due to this active setting, the study area is exposed to multiple geohazards, among which we deal with: (1) retrogressive instability at the head of the Gioiosa Marea submarine canyon, (2) coastal erosion favored by the downlope funnelling of littoral drift at the canyon head, (3) flooding scenario at 2100 using the IPCC (Intergovernmental Panel on Climate Change) and Rahmstorf sea-level projections. The consequences associated with these geohazards are amplified by the strong anthropization pressures occurring along in this sector. Our results provide key insights regarding the future scenarios of this coastal sector, revealing the effects of the retrogressive activity associated with the canyon head on the coastal strip. We also present the first management tool for the application of forecasting studies by local administrations.
    Description: Published
    Description: 2
    Description: 3A. Geofisica marina e osservazioni multiparametriche a fondo mare
    Description: JCR Journal
    Keywords: Submarine canyon · Sicily continental margin · Uplift rate · Coastal erosion · Relative sea-level projections · Coastal flooding ; Geohazard assessment
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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