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  • 1
    Online Resource
    Online Resource
    Oxford :Taylor & Francis Group,
    Keywords: Volcanism-Research. ; Electronic books.
    Description / Table of Contents: Originally published in 1995, Monitoring Active Volcanoes is a comprehensive text which addresses the importance of volcano surveillance in the context of forecasting eruptive activity and mitigating its effects.
    Type of Medium: Online Resource
    Pages: 1 online resource (436 pages)
    Edition: 1st ed.
    ISBN: 9781000726565
    Series Statement: Routledge Revivals Series
    DDC: 551.210287
    Language: English
    Note: Cover -- Half Title -- Title -- Copyright -- Original Title -- Original Copyright -- Contents -- Preface -- Dedication -- List of contributors -- 1 Monitoring active volcanoes - an introduction -- 1.1 Why monitor volcanoes? -- 1.2 Recent advances in ground-based volcano surveillance -- 1.3 Airborne and satellite monitoring -- 1.4 Monitoring strategies -- 1.5 Predicting volcanic eruptions -- 1.6 Monitoring and volcanic hazard mitigation -- 1.7 Safe surveillance of active volcanoes -- References -- 2 Data acquisition and telemetry -- 2.1 Introduction -- 2.2 Principles of data acquisition and transmission -- 2.3 Examples of acquisition and transmission systems -- 2.4 Conclusions -- Acknowledgements -- References -- 3 Seismic monitoring at active volcanoes -- 3.1 Introduction -- 3.2 Locating seismic events: some constraints -- 3.3 The seismic source -- 3.4 The role of instrumentation: past, present and future -- Acknowledgements -- References -- 4 Real-time ground deformation monitoring -- 4.1 Introduction -- 4.2 Real-time tiltmeter monitoring at active volcanoes -- 4.3 Tiltmeter and aedm monitoring at Piton de la Fournaise -- Acknowledgements -- References -- 5 Ground deformation surveying of active volcanoes -- 5.1 Introduction -- 5.2 Measuring horizontal deformation -- 5.3 Measuring vertical deformation -- 5.4 Dry tilt -- 5.5 Benchmarks -- 5.6 Designing a deformation network -- 5.7 Analysis -- 5.8 Conclusions -- References -- 6 GPS - monitoring volcanic deformation from space -- 6.1 Introduction -- 6.2 Some basic concepts -- 6.3 Biases and errors -- 6.4 GPS operating equipment and survey design -- 6.5 Data processing -- 6.6 Use of continuous gps measurements for ground deformation monitoring -- 6.7 Case study: GPS surveys at Mount Etna -- 6.8 Concluding remarks -- References -- 7 Infrared thermal monitoring -- 7.1 Introduction. , 7.2 What can thermal measurements tell us about a volcano? -- 7.3 What is remote sensing? -- 7.4 Satellite data -- 7.5 The physics of thermal remote sensing -- 7.6 Case studies of remote sensing of high-temperature thermal anomalies -- 7.7 Case studies of remote sensing of low-temperature thermal anomalies -- 7.8 Ground-based infrared measurements of hot phenomena -- 7.9 Satellite data: where to get them, what to ask for, and what they cost -- 7.10 Conclusions -- Acknowledgements -- References -- Appendix: list of acronyms and related terms -- 8 Microgravity monitoring -- 8.1 Introduction -- 8.2 Background -- 8.3 Technique -- 8.4 Interpretation -- 8.5 Applications -- 8.6 Summary and conclusions -- Acknowledgements -- References -- 9 Geoelectrical methods in volcano monitoring -- 9.1 Introduction -- 9.2 Direct-current resistivity methods -- 9.3 Electromagnetic methods -- 9.4 Self-potential methods -- 9.5 Conclusion -- Acknowledgements -- References -- 10 Geomagnetic surveying methods -- 10.1 Introduction -- 10.2 Magnetic fields -- 10.3 Method -- 10.4 Case studies -- 10.5 Conclusion -- References -- 11 Remote sensing spectroscopy of volcanic plumes and clouds -- 11.1 Introduction -- 11.2 COSPEC -- 11.3 Activity and SO2 emission -- 11.4 Improvements in COSPEC methodology -- 11.5 Remote sensing of other gases -- 11.6 Satellite methods -- References -- 12 Monitoring fluids and gases at active volcanoes -- 12.1 Introduction -- 12.2 Sampling and analytical techniques -- 12.3 Interpretation of chemical and isotope data at Campi Flegrei caldera -- 12.4 Geochemical monitoring at Vulcano (Aeolian Islands) -- 12.5 Thermal waters -- 12.6 Soil gases -- 12.7 Conclusion -- References -- 13 Forecasting the behaviour of lava flows -- 13.1 Introduction -- 13.2 Basic features -- 13.3 Flow surfaces -- 13.4 Emplacement regimes -- 13.5 Aa flow emplacement. , 13.6 Comparison of lengthening models -- 13.7 Hazard assessment and future requirements -- Acknowledgements -- References -- 14 The role of monitoring in forecasting volcanic events -- 14.1 Introduction and historical perspective -- 14.2 Volcano monitoring and forecasts -- 14.3 Selected case studies -- 14.4 Lessons for the future -- Acknowledgements -- References -- 15 Prospects for volcano surveillance -- 15.1 An approach for the 21st century -- 15.2 Future technological developments -- 15.3 Conclusion -- References -- APPENDIX Safety measures for volcanologists -- Index.
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  • 2
    Online Resource
    Online Resource
    Oxford :Taylor & Francis Group,
    Keywords: Lava. ; Electronic books.
    Description / Table of Contents: Originally published in 1993, Active Lavas looks at the practical aspects of monitoring uncontrolled streams of molten rock and how field data can be applied for theoretical modelling and forecasting the growth of lava flows.
    Type of Medium: Online Resource
    Pages: 1 online resource (389 pages)
    Edition: 1st ed.
    ISBN: 9781000770698
    Series Statement: Routledge Revivals Series
    DDC: 552/.22
    Language: English
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  • 3
    Book
    Book
    London : UCL Press
    Keywords: Geology and Palaeontology ; volcanism ; Lava
    Type of Medium: Book
    Pages: X, 374 S. , Ill., graph. Darst.
    Edition: 1. publ.
    ISBN: 1857280075
    DDC: 551.2
    RVK:
    RVK:
    Language: English
    Note: Literaturangaben
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  • 4
    Keywords: Volcanism ; Calderas ; Aufsatzsammlung ; Vulkanismus ; Risikoanalyse ; Eruption ; Caldera ; Caldera
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (VIII, 198 Seiten)
    ISBN: 1862392110 , 9781862392113
    Series Statement: Geological Society special publication 269
    DDC: 551.21
    Language: English
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  • 5
    Publication Date: 2020-01-02
    Description: Large calderas are among the Earth's major volcanic features. They are associated with large magma reservoirs and elevated geothermal gradients. Caldera-forming eruptions result from the withdrawal and collapse of the magma chambers and produce large-volume pyroclastic deposits and later-stage deformation related to post-caldera resurgence and volcanism. Unrest episodes are not always followed by an eruption; however, every eruption is preceded by unrest. The Campi Flegrei caldera (CFc), located along the eastern Tyrrhenian coastline in southern Italy, is close to the densely populated area of Naples. It is one of the most dangerous volcanoes on Earth and represents a key example of an active, resurgent caldera. It has been traditionally interpreted as a nested caldera formed by collapses during the 100–200 km3 Campanian Ignimbrite (CI) eruption at ∼39 ka and the 40 km3 eruption of the Neapolitan Yellow Tuff (NYT) at ∼15 ka. Recent studies have suggested that the CI may instead have been fed by a fissure eruption from the Campanian Plain, north of Campi Flegrei. A MagellanPlus workshop was held in Naples, Italy, on 25–28 February 2017 to explore the potential of the CFc as target for an amphibious drilling project within the International Ocean Discovery Program (IODP) and the International Continental Drilling Program (ICDP). It was agreed that Campi Flegrei is an ideal site to investigate the mechanisms of caldera formation and associated post-caldera dynamics and to analyze the still poorly understood interplay between hydrothermal and magmatic processes. A coordinated onshore–offshore drilling strategy has been developed to reconstruct the structure and evolution of Campi Flegrei and to investigate volcanic precursors by examining (a) the succession of volcanic and hydrothermal products and related processes, (b) the inner structure of the caldera resurgence, (c) the physical, chemical, and biological characteristics of the hydrothermal system and offshore sediments, and (d) the geological expression of the phreatic and hydromagmatic eruptions, hydrothermal degassing, sedimentary structures, and other records of these phenomena. The deployment of a multiparametric in situ monitoring system at depth will enable near-real-time tracking of changes in the magma reservoir and hydrothermal system.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    Publication Date: 2021-01-25
    Description: Large calderas are among the Earth's major volcanic features. They are associated with large magma reservoirs and elevated geothermal gradients. Caldera-forming eruptions result from the withdrawal and collapse of the magma chambers and produce large-volume pyroclastic deposits and later-stage deformation related to post-caldera resurgence and volcanism. Unrest episodes are not always followed by an eruption; however, every eruption is preceded by unrest. The Campi Flegrei caldera (CFc), located along the eastern Tyrrhenian coastline in southern Italy, is close to the densely populated area of Naples. It is one of the most dangerous volcanoes on Earth and represents a key example of an active, resurgent caldera. It has been traditionally interpreted as a nested caldera formed by collapses during the 100–200 km3 Campanian Ignimbrite (CI) eruption at ∼39 ka and the 40 km3 eruption of the Neapolitan Yellow Tuff (NYT) at ∼15 ka. Recent studies have suggested that the CI may instead have been fed by a fissure eruption from the Campanian Plain, north of Campi Flegrei. A MagellanPlus workshop was held in Naples, Italy, on 25–28 February 2017 to explore the potential of the CFc as target for an amphibious drilling project within the International Ocean Discovery Program (IODP) and the International Continental Drilling Program (ICDP). It was agreed that Campi Flegrei is an ideal site to investigate the mechanisms of caldera formation and associated post-caldera dynamics and to analyze the still poorly understood interplay between hydrothermal and magmatic processes. A coordinated onshore–offshore drilling strategy has been developed to reconstruct the structure and evolution of Campi Flegrei and to investigate volcanic precursors by examining (a) the succession of volcanic and hydrothermal products and related processes, (b) the inner structure of the caldera resurgence, (c) the physical, chemical, and biological characteristics of the hydrothermal system and offshore sediments, and (d) the geological expression of the phreatic and hydromagmatic eruptions, hydrothermal degassing, sedimentary structures, and other records of these phenomena. The deployment of a multiparametric in situ monitoring system at depth will enable near-real-time tracking of changes in the magma reservoir and hydrothermal system.
    Description: Published
    Description: 29-46
    Description: 3A. Geofisica marina e osservazioni multiparametriche a fondo mare
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 7
    Publication Date: 2020-06-03
    Description: Naples and its hinterland in Southern Italy are one of the most urbanized areas in the worldunder threat from volcanic activity. The region lies within range of three active volcanic centers: Vesuvius,Campi Flegrei, and Ischia. The Campi Flegrei caldera, in particular, has been in unrest for six decades. Theunrest followed four centuries of quiescence and has heightened concern about an increased potential foreruption. Innovative modeling and scientific drilling are being used to investigate Campi Flegrei, and theresults highlight key directions for better understanding the mechanisms of caldera formation and the rolesof magma intrusion and geothermal activity in determining the volcano’s behavior. They also provide aframework for evaluating and mitigating the risk from this caldera and other large ones worldwide
    Description: Published
    Description: 2004– 2008
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2018-05-02
    Description: Unrest at large calderas rarely ends in eruption, encouraging vulnerable communities to perceive emergency warnings of volcanic activity as false alarms. A classic example is the Campi Flegrei caldera in southern Italy, where three episodes of major uplift since 1950 have raised its central district by about 3 m without an eruption. Individual episodes have conventionally been treated as independent events, so that only data from an ongoing episode are considered pertinent to evaluating eruptive potential. An implicit assumption is that the crust relaxes accumulated stress after each episode. Here we apply a new model of elastic-brittle failure to test the alternative view that successive episodes promote a long-term accumulation of stress in the crust. The results provide the first quantitative evidence that Campi Flegrei is evolving towards conditions more favourable to eruption and identify field tests for predictions on how the caldera will behave during future unrest.
    Description: Published
    Description: 15312
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2023-06-19
    Description: Volcanoes reawakening after long repose must rupture the crust before magma can erupt. Rupture is preceded by repeatable variations in the rate of seismicity with ground movement, which trace the amount of applied stress that is released by local earthquakes. A rupturing sequence has been developing across four episodes of ground uplift at Italy’s Campi Flegrei caldera: in 1950-1952, 1969-1972, 1982-1984 and since 2004. We predicted in 2016 that the approach to rupture would continue after an additional uplift of 30-40 cm at the location of largest movement. We have updated our analysis with new data on changes in the numbers of local earthquakes with amounts of ground movement. Here we show that subsequent events have confirmed our prediction and that the unrest has been changing the structure of Campi Flegrei’s crust. The results provide new constraints for evaluating the volcano’s potential to erupt or to subside without eruption.
    Description: Published
    Description: 190
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2024-01-18
    Description: Changes in seismicity with time and location are diagnostic signals for understanding the dynamics of volcanic unrest. We used these signals at the Campi Flegrei caldera, in southern Italy, to investigate how structural changes have determined three styles of unrest since 1982, distinguished by a ground uplift (measured at Pozzuoli, near the centre of the caldera) of 178 cm in 1982–84; a subsidence of 93 cm in 1985–2005; and an uplift of 118 cm between 2005 and November 2023. Double-difference seismic locations and concentrations of seismic energy release have revealed impermeable horizons that correspond to the cap rock and self-sealed base of the geothermal system at depths of 1.5 and 3 km, respectively. Most earthquakes have been shallower than 3 km, consistent with the brittle upper crust being stretched over a zone of pressurization below the geothermal system. The 1982–84 uplift decayed after a major seismic swarm on April 1st, 1984, breached the lower impermeable horizon, which increased the flux of escaping gas and reduced the source pressure. Continued gas escape promoted subsidence until the lower horizon had resealed itself and initiated a new episode of uplift while gas from depth re-accumulated beneath. Compared with 1982–84, a greater proportion of recent seismicity has occurred at shallower depths below the actively degassing fumaroles of Solfatara-Pisciarelli, north-east of Pozzuoli. The associated high seismic b-values, between 1 and 2, are consistent with high fluid pressures and, hence, with locations more favourable to fracturing. Continued uplift may thus persist until fracturing of the shallow crust allows faster rates of gas release and depressurization of the pressure source.
    Description: Published
    Description: 118530
    Description: OSV2: Complessità dei processi vulcanici: approcci multidisciplinari e multiparametrici
    Description: JCR Journal
    Keywords: Campi Flegrei caldera ; Hydrothermal system ; Volcanic unrest ; Seismicity ; Fluid circulation ; Brittle/ductile transition
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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