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  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: SCIENCE / Earth Sciences / General. ; Electronic books.
    Description / Table of Contents: This thought-provoking book presents a compelling account of recent and historical disasters, both natural and human-caused, drawing out common themes and providing a holistic understanding of hazards, disasters and mitigation, for anyone interested in this important and topical subject.
    Type of Medium: Online Resource
    Pages: 1 online resource (324 pages)
    Edition: 1st ed.
    ISBN: 9781108111621
    DDC: 363.346
    Language: English
    Note: Cover -- Half-title page -- Title page -- Copyright page -- Dedication -- Contents -- Online Appendix -- Preface -- Acknowledgments -- 1 Black and White Swans, Communication, Evolution, and Markets -- Long-Term Risk, Listening Skills, and Evolution -- Cost of Disasters and the Role of Markets -- 2 What Is a Natural Disaster? Where Do They Occur and Why? Are They Different from Human-Made Disasters? -- Earth's Natural Cycles: Volcanoes, Climate, and Earthquakes -- How Does the Motion of Plates Lead to Earthquakes and Tsunamis? -- Volcanoes and Climate -- Hurricanes, Flooding, and Sea-Level Rise -- 3 If We Know So Much about Natural Disasters, Why Do We Remain Vulnerable? -- Scientific Uncertainty -- Time Lag, Sticky Infrastructure, and the Challenge of Relocation -- The Importance of Building Codes -- Cost versus Benefit -- 4 Japanese Earthquakes and Nuclear Power Plant Failures -- Hydrogen: Why Is It Produced in Nuclear Power Plant Accidents? Why Is It Dangerous? What's It Got to Do with the Hindenburg? -- How Bad Was Fukushima? -- What Went Wrong? -- A Disturbing Precursor -- Regulation and Transparency -- 5 Future Earthquake and Tsunami Disasters -- Sleepless in Seattle -- Tsunamis in Switzerland -- The Orient Express -- 6 Nuclear Power, Coal, and Tuna: The Concept of Relative Risk -- The Toxic Legacy of Lead -- Mercury and Coal -- Deaths from Coal versus Deaths from Nuclear Power -- Carbon Capture and Storage -- What about Solar? -- 7 Past and Future Coastal Flooding: Galveston, New Orleans, Bangladesh, and the Specter of Sea-Level Rise -- The Great Galveston Hurricane of 1900 -- New Orleans and Hurricane Katrina -- River Deltas, Subsidence, and Levees -- Could It Happen Again? -- Sea-Level Rise: A Slow Disaster in the Making -- Slow Sea-Level Rise and Rapid Flooding -- What Other Regions Are at Risk? -- Summary. , 8 What's All the Fuss about Global Warming? -- Communication: The Need for Long-Term Data and the Challenge of Explaining Them -- The Time Lag Problem: Why We Need to Think Long Term -- Economic Consequences -- Some Lessons from Greenland -- 9 Solutions -- Communication -- Transparency -- Let Markets Work Their Magic -- The Magic of New Technology: Blue LEDs, the Tesla, and Photosynthesis -- R& -- D and Taxes -- Avoiding the "Coal Trap" -- Independent Boards -- Lessons Learned -- The Challenge of Large Infrastructure Projects -- Summary -- Summary of Recommendations by Chapter -- References and Further Reading -- Index.
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  • 2
    Keywords: Subduction zones ; Thrust faults (Geology) ; Earthquake prediction ; Konferenzschrift ; Aufsatzsammlung ; Erdbeben ; Aufschiebung ; Subduktion ; Seismologie ; Kontinentalrand ; Seismizität ; Störung
    Type of Medium: Book
    Pages: IX, 680 S , Ill., graph. Darst , 26 cm
    ISBN: 0231138660 , 9780231138666
    Series Statement: MARGINS theoretical and experimental earth science series
    DDC: 551.22
    Language: English
    Note: MARGINS Program sponsored by the U.S. National Science Foundation (NSF)
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  • 3
    In: Journal of geophysical research / B, Washington, DC : Union, 1978, 0148-0227
    Description / Table of Contents: New seismic and geodetic data from Costa Rica provide insight into seismogenic zone processes in Central America, where the Cocos and Caribbean plates converge. Seismic data are from combined land and ocean bottom deployments in the Nicoya peninsula in northern Costa Rica and near the Osa peninsula in southern Costa Rica. In Nicoya, inversion of GPS data suggests two locked patches centered at 14 ± 2 and 39 ± 6 km depth. Interplate microseismicity is concentrated in the more freely slipping intermediate zone, suggesting that small interseismic earthquakes may not accurately outline the updip limit of the seismogenic zone, the rupture zone for future large earthquakes, at least over the short (~1 year) observation period. We also estimate northwest motion of a coastal "sliver block" at 8 ± 3 mm/yr, probably related to oblique convergence. In the Osa region to the south, convergence is orthogonal to the trench. Cocos-Caribbean relative motion is partitioned here, with ~8 cm/yr on the Cocos-Panama block boundary (including a component of permanent shortening across the Fila Costeña fold and thrust belt) and ~1 cm/yr on the Panama blockCaribbean boundary. The GPS data suggest that the Cocos platePanama block boundary is completely locked from ~10-50 km depth. This large locked zone, as well as associated forearc and back-arc deformation, may be related to subduction of the shallow Cocos Ridge and/or younger lithosphere compared to Nicoya, with consequent higher coupling and compressive stress in the direction of plate convergence.
    Type of Medium: Microfilm
    Pages: graph. Darst
    ISSN: 0148-0227
    Language: English
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  • 4
    Publication Date: 2021-10-25
    Description: Estimates of flood susceptibility and land loss in the world's coastal regions depend on our knowledge of sea level rise (SLR) from increases in ocean mass and volume, as well as knowledge of vertical land motion. Conventional approaches to the latter include tide-gauge and Global Positioning System (GPS) measurements relative to well-anchored monuments few meters below the surface. However, in regions of rapid Holocene sedimentation, compaction of this material can add a significant component to the surface lowering. Unfortunately, this process has been difficult to quantify, especially for the shallowest material above the monument. Here we use a new technique, GPS interferometric reflectometry, to estimate the rate of this process in the Mississippi Delta and the eastern margin of the North Sea. We show that the rate of shallow compaction is comparable to or larger than the rate of global SLR, adding 35% and 65%, respectively, to the rate of relative SLR by 2100.
    Keywords: 526.3 ; 551 ; GPS ; interferometric reflectometry ; tide gauge ; coastal subsidence ; shallow subsidence ; Holocene sediment compaction
    Language: English
    Type: map
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  • 5
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] It has long been recognized that New Orleans is subsiding and is therefore susceptible to catastrophic flooding. Here we present a new subsidence map for the city, generated from space-based synthetic-aperture radar measurements, which reveals that parts of New Orleans underwent rapid ...
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2018-04-25
    Description: New seismic and geodetic data from Costa Rica provide insight into seismogenic zone processes in Central America, where the Cocos and Caribbean plates converge. Seismic data are from combined land and ocean bottom deployments in the Nicoya peninsula in northern Costa Rica and near the Osa peninsula in southern Costa Rica. In Nicoya, inversion of GPS data suggests two locked patches centered at 14 ± 2 and 39 ± 6 km depth. Interplate microseismicity is concentrated in the more freely slipping intermediate zone, suggesting that small interseismic earthquakes may not accurately outline the updip limit of the seismogenic zone, the rupture zone for future large earthquakes, at least over the short (∼1 year) observation period. We also estimate northwest motion of a coastal “sliver block” at 8 ± 3 mm/yr, probably related to oblique convergence. In the Osa region to the south, convergence is orthogonal to the trench. Cocos-Caribbean relative motion is partitioned here, with ∼8 cm/yr on the Cocos-Panama block boundary (including a component of permanent shortening across the Fila Costeña fold and thrust belt) and ∼1 cm/yr on the Panama block–Caribbean boundary. The GPS data suggest that the Cocos plate–Panama block boundary is completely locked from ∼10–50 km depth. This large locked zone, as well as associated forearc and back-arc deformation, may be related to subduction of the shallow Cocos Ridge and/or younger lithosphere compared to Nicoya, with consequent higher coupling and compressive stress in the direction of plate convergence.
    Type: Article , PeerReviewed
    Format: text
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