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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
    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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  • 3
    Publication Date: 2023-02-28
    Description: The Sciara del Fuoco (SdF) collapse scar at Stromboli is an active volcanic area affected by rapid morphological changes due to explosive/effusive eruptions and mass-wasting processes. The aim of this paper is to demonstrate the importance of an integrated analysis of multi-temporal remote sensing (photogrammetry, COSMO-SkyMed Synthetic Aperture Radar amplitude image) and marine geophysical data (multibeam and side scan sonar data) to characterize the main morphological, textural, and volumetric changes that occurred along the SdF slope in the 2020–2021 period. The analysis showed the marked erosive potential of the 19 May 2021 pyroclastic density current generated by a crater rim collapse, which mobilized a minimum volume of 44,000 m^3 in the upper Sciara del Fuoco slope and eroded 350,000–400,000 m^3 of material just considering the shallow-water setting. The analysis allowed us also to constrain the main factors controlling the emplacement of different lava flows and overflows during the monitored period. Despite the morphological continuity between the subaerial and submarine slope, textural variations in the SdF primarily depend on different processes and characteristics of the subaerial slope, the coastal area, the nearshore, and “deeper” marine areas.
    Description: Published
    Description: 4605
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: JCR Journal
    Keywords: Stromboli ; hazard ; active volcano ; morphological changes ; UAV flight ; remote sensing ; multibeam bathymetry ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2023-03-02
    Description: This study analyses the morphological changes induced by eruptive activity at Stromboli volcano (Italy) during and after events occurring during July–August 2019. This period was characterized by intense eruptive activity (two paroxysmal explosions, a two-month-long lava emission, and more intense and frequent “ordinary” explosive activity) that produced significant changes within the region known as Sciara del Fuoco, located on the most unstable, north-western flank of the volcano. Since September 2019, the eruptive activity waned but remained intense, and erosive phenomena continued to contribute to the re-shaping of the Sciara del Fuoco. The morphological changes described here were documented by integrating topographic (PLÉIADES satellite tri-stereo Digital Elevation Models) and multibeam bathymetric data, acquired before, during, and after the paroxysmal events. This allowed the study of the cumulative effect of the different processes and the characterization of the different phases of accumulation/emplacement, erosion, remobilization and re-sedimentation of the volcaniclastic materials. Data acquired at several periods between September 2018 and April 2020, allowed a comparison of the subaerial and submarine effects of the 2019 events. We find evidence of localized, significant erosion following the two pyroclastic density currents triggered by the paroxysmal explosion of the 3 July 2019. We interpret this erosion as being caused by submarine and subaerial landslides triggered by the propagation of pyroclastic density currents down the Sciara del Fuoco slope. Immediately after the explosion, a lava field accumulated on the sub-aerial slope, produced by effusive activity which lasted about two months. Subsequently, the newly emplaced lava, and in particular its breccia, was eroded, with the transfer of material onto the submarine slope. This work demonstrates how repeated topo-bathymetric surveys allowed identification of the slope processes that were triggered in response to the rapid geomorphological variations due to the eruptive activity. The surveys also allowed distinction of whether estimated volumetric losses were the result of single mass-flows or gradual erosive processes, with implications on the related geohazard. Furthermore, this work highlights how submarine slope failures can be triggered by the entry into the water of pyroclastic density currents, even of modest size. These results are important for the development and improvement of an early warning system for tsunami-induced by mass flows, both in Stromboli and for island-based and coastal volcanoes elsewhere, where landslides and pyroclastic density currents can trigger significant, potentially destructive, tsunami waves.
    Description: Published
    Description: 108093
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: JCR Journal
    Keywords: Digital Elevation Models ; PLÉIADES ; Repeated bathymetric surveys ; Volcano geomorphology ; Submarine morphology ; Stromboli ; Active volcano ; Aeolian Archipelago ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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