GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Cambridge :Cambridge University Press,  (1)
  • Springer  (1)
  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Volcanism -- Effect of environment on. ; Volcanism -- History. ; Volcanology. ; Electronic books.
    Description / Table of Contents: Did volcanic eruptions extinguish the dinosaurs and shape human civilisation? Clive Oppenheimer explores the greatest volcanic events of the past quarter of a billion years, using rich geological, historical, archaeological and palaeoenvironmental records. His forensic approach to volcanology links cause and effect, providing important lessons for future catastrophe risk management.
    Type of Medium: Online Resource
    Pages: 1 online resource (410 pages)
    Edition: 1st ed.
    ISBN: 9781139113946
    DDC: 551.21
    Language: English
    Note: Cover -- Title -- Copyright -- Contents -- Preface -- Acknowledgements -- 1 Fire and brimstone: how volcanoes work -- 1.1 Origins of volcanoes: the mantle -- 1.2 Magma -- 1.3 Eruption parameters -- 1.3.1 Explosive and effusive volcanism -- 1.3.2 Magnitude -- 1.3.3 Intensity -- 1.4 Summary -- 2 Eruption styles, hazards and ecosystem impacts -- 2.1 Eruption clouds -- 2.1.1 Hazards -- 2.2 Tephra falls -- 2.2.1 Hazards -- 2.2.2 Ash fertilisation -- 2.3 Pyroclastic currents & -- caldera formation -- 2.3.1 Hazards -- 2.4 Lava flows and domes -- 2.4.1 Hazards -- 2.5 Rock avalanches and mudflows -- 2.5.1 Hazards -- 2.6 Tsunami -- 2.6.1 Hazards -- 2.7 Earthquakes -- 2.7.1 Hazards -- 2.8 Volcanic gas emissions -- 2.8.1 Hazards -- 2.9 Recovery of ecosystems -- 2.10 Volcanic disasters -- 2.11 Summary -- 3 Volcanoes and global climate change -- 3.1 Pinatubo's global cloud -- 3.1.1 Optical illusions -- 3.2 Atmospheric and climatic change -- 3.2.1 Effects on light and heat radiation -- 3.2.2 Summer cooling, winter warming -- 3.2.3 Oceanic response -- 3.2.4 Biological feedbacks -- 3.2.5 Stratospheric ozone depletion -- 3.3 Recipe for a climate-forcing eruption -- 3.3.1 Sulphur content and eruption magnitude -- 3.3.2 Eruption intensity and style -- 3.3.3 Eruption location -- 3.3.4 Eruption timing -- 3.4 Summary -- 4 Forensic volcanology -- 4.1 Reading the rocks -- 4.1.1 Characteristics of tephra deposits -- 4.1.2 Estimating eruption parameters -- Eruption magnitude -- Eruption intensity -- 4.1.3 Dating eruptions -- Potassium and argon -- Radiocarbon -- Fission tracks -- 4.1.4 Tephrochronology -- 4.1.5 Volatile yields -- 4.2 Ice cores -- 4.2.1 Geochemical fingerprinting -- 4.2.2 Volatile yields -- 4.3 Tree rings -- 4.4 Summary -- 5 Relics, myths and chronicles -- 5.1 Archaeological perspectives -- 5.1.1 El Salvador's 'Pompeii'. , 5.1.2 Arenal volcano, Costa Rica -- 5.1.3 Papua New Guinea -- 5.2 Oral traditions -- 5.2.1 Mt Pinatubo 1991: an eruption foretold -- 5.2.2 Kīlauea -- 5.2.3 Mt Mazama -- 5.3 Crepuscular lights, cannonades and chronicles -- 5.3.1 Visual arts -- 5.4 Volcano forensics: a case study -- 5.4.1 The 1861 eruption of Dubbi volcano -- 5.5 Summary -- 6 Killer plumes -- 6.1 Mass extinctions -- 6.2 More about LIPs -- 6.3 LIP origins -- 6.4 LIPs, bolides and extinctions: the coincidences -- 6.4.1 The end of the dinosaurs -- 6.4.2 Is the Earth's mantle a serial killer? -- 6.5 Kill mechanisms -- 6.6 Hot LIPS and cold SLIPS -- 6.6.1 LIPs, 'volcanic winters' and 'snowball Earth' -- 6.7 Summary -- 7 Human origins -- 7.1 The East African Rift Valley -- 7.2 The first humans -- 7.3 The Middle Stone Age and modern humans -- 7.3.1 Human migrations: push and pull -- 7.3.2 Out of Africa (again) -- 7.4 Summary -- 8 The ash giant/sulphur dwarf -- 8.1 The eruption -- 8.1.1 When did it happen? -- 8.1.2 What was it like? -- 8.2 Sulphur yield of the eruption -- 8.3 Climate change -- 8.3.1 Climate models -- 8.3.2 Palaeoenvironmental evidence -- 8.4 The human story -- 8.4.1 Counter-arguments -- 8.5 Focus on India -- 8.6 Summary -- 9 European volcanism in prehistory -- 9.1 The Campanian eruption and the human revolution in Palaeolithic Europe -- 9.1.1 Climate impact -- 9.1.2 Human impact -- 9.2 'Cultural devolution' and the Laacher See eruption -- 9.2.1 Climate impact -- 9.2.2 Human impact -- Tasmania -- 9.3 Eruption of Santorini and decline of the Minoan civilisation -- 9.3.1 The Minoan world -- 9.3.2 The eruption -- 9.3.3 Dating the eruption -- 9.3.4 Tsunami and human impact -- 9.4 Summary -- 10 The rise of Teotihuacán -- 10.1 Popocatepetl -- 10.2 The Ilopango eruption -- 10.3 Summary -- 11 Dark Ages: dark nature? -- 11.1 The Mystery Cloud of 536 CE. , 11.1.1 The aerosol veil in contemporary literature -- 11.1.2 Plague -- 11.1.3 Consequences for the Empire -- 11.2 Veils and whips -- 11.2.1 Ice cores -- 11.2.2 Identifying the mystery eruption -- 11.2.3 Machine-gun volcanism and the Little Ice Age -- 11.2.4 Religious fervour and regime change -- 11.3 Summary -- 12 The haze famine -- 12.1 The eruption -- 12.2 Gas emissions and aerosol veil -- 12.2.1 Spread of the volcanic cloud -- 12.3 Weather and climate -- 12.4 The haze famine -- 12.5 Long reach of the eruption -- 12.5.1 Mortality crisis in England -- 12.5.2 Africa and Asia -- 12.5.3 The French Revolution -- 12.6 Summary -- 13 The last great subsistence crisis in the Western world -- 13.1 Sumbawa before the disaster -- 13.2 The eruption -- 13.2.1 Initial blasts -- 13.2.2 Cataclysmic eruption -- 13.2.3 Darkness at noon -- 13.2.4 Tsunami -- 13.2.5 Pumice rafts -- 13.3 Atmospheric and climate impacts -- 13.4 Human tragedy -- 13.5 Global reach of the eruption -- 13.5.1 Disease, demography, economics and politics -- 13.6 Summary -- 14 Volcanic catastrophe risk -- 14.1 Three catastrophe scenarios -- 14.1.1 Explosive eruption near a major city -- 14.1.2 Volcanogenic pollution crisis -- 14.1.3 'Super-eruption' scenario -- 14.2 Risk control -- 14.2.1 Vulnerability versus resilience -- 14.2.2 Risk analysis and the problem of extremes -- 14.2.3 Preparation and response -- Preparing for emergency evacuation -- International frameworks -- 14.3 Global warming: fake volcanoes and real eruptions -- 14.3.1 Stratospheric geo-engineering -- 14.3.2 Could climate change trigger eruptions? -- 14.4 Shaken but not stirred -- Appendix A: Large eruptions -- Appendix B: Further reading and data sources -- Chapter 1 -- Chapter 2 -- Chapter 3 -- Chapter 4 -- Data sources -- Chapter 5 -- Chapter 6 -- Chapter 7 -- Chapter 8 -- Chapter 9 -- Chapter 10 -- Chapter 11 -- Chapter 12. , Chapter 13 -- Chapter 14 -- References -- Index.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2022-06-08
    Description: This chapter is arguably the most complete compilation of sulfur volcanism of any given volcano on Earth: Poás. Sulfur volcanism at Poás is described in historical literature since 1828, and in scientific literature since the 1960’s. We first classify the various manifestations of sulfur volcanism at crater lake bearing volcanoes (subaerial and sublacustrine sulfur pools, sulfur spherules, flows, cones/hornitos, and sweat, and pyroclastic and burning sulfur), based on work by Japanese pioneers of the early 1900s. Their first observations and models have passed the test of time and still stand as theories today. Comparing the sulfur volcanism at Poás with the one at other (55) volcanoes, it is honest to say that only White Island (New Zealand) and Kawah Ijen (Indonesia) are the only ones comparable with Poás, being the most dynamic of them all.
    Description: Published
    Description: 45-78
    Description: 4V. Processi pre-eruttivi
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...