Volcano Deformation

Volcanoes and eruptions are dramatic surface man telemetry and processing, and volcano-deformation ifestations of dynamic processes within the Earth, source models over the past three decades. There has mostly but not exclusively localized along the been a virtual explosion of volcano-geodesy studies boundaries of Earth's relentlessly shifting tectonic and in the modeling and interpretation of ground plates. Anyone who has witnessed volcanic activity deformation data. Nonetheless, other than selective, has to be impressed by the variety and complexity of brief summaries in journal articles and general visible eruptive phenomena. Equally complex, works on volcano-monitoring and hazards mitiga however, if not even more so, are the geophysical, tion (e. g. , UNESCO, 1972; Agnew, 1986; Scarpa geochemical, and hydrothermal processes that occur and Tilling, 1996), a modern, comprehensive treat underground - commonly undetectable by the ment of volcano geodesy and its applications was human senses - before, during, and after eruptions. non-existent, until now. Experience at volcanoes worldwide has shown that, In the mid-1990s, when Daniel Dzurisin (DZ to at volcanoes with adequate instrumental monitor friends and colleagues) was serving as the Scientist ing, nearly all eruptions are preceded and accom in-Charge of the USGS Cascades Volcano Observa panied by measurable changes in the physical and tory (CVO), I first learned of his dream to write a (or) chemical state of the volcanic system. While book on volcano geodesy.

First book devoted specifically to volcano geodesy Only book available dealing with state-of-the-art technologies

Autorentext

Dr Zhong Lu and Dr Daniel Dzurisin have worked closely together for several years on InSAR projects in the Aleutian volcanic arc and have co-authored 16 papers on planetary geology and volcanology, as well as a chapter on InSar in Dr Dzurisin's first Springer-Praxis book, Volcano Deformation - Geodetic Monitoring Techniques.

Klappentext

Volcanic Deformation is the first book devoted to volcano geodesy, a specialisation of the still-young science of volcanology. It forms a part of the whole catalogue of methods used to monitor a restless or an erupting volcano, and demonstrates how risk from hazardous eruptions can be reduced.

With contributions from some of the most experienced and knowledgeable experts in the field, the book desbribes the state-of-the-art techniques used by volcanologists to successfully predict volcanic eruptions. With chapters on GPS and synthetic aperture radar interferometry, Volcanic Deformation covers both the "classical" and emerging methodologies, and looks at the future challenges faced by scientists when predicting volcanic eruptions.

Volcanic Deformation

• is an up-to-date, comprehensive treatment of volcanic geodesy and its applications;
• describes how volcanic geodesy complements other volcano monitoring approaches and tools;
• gives an extensive treatment of the key lessons volcanologists have learned at well-monitored deforming volcanoes.

Inhalt
1 The modern volcanologist's tool kit.- 1.1 Volcanoes in motion when deformation gets extreme.- 1.2 Volcanology in the information age.- 1.3 A brief survey of volcano-monitoring techniques.- 1.4 An introduction to geodetic sensors and techniques.- 2 Classical surveying techniques.- 2.1 Early geodetic surveys.- 2.2 Reference systems and datums.- 2.3 Geodetic networks.- 2.4 Trilateration and triangulation.- 2.5 Leveling and tilt-leveling surveys.- 2.6 Photogrammetry.- 2.7 Microgravity surveys.- 2.8 Magnetic field measurements.- 3 Continuous monitoring with in situ sensors.- 3.1 Seismometers.- 3.2 Tiltmeters.- 3.3 Strainmeters.- 3.4 Continuous GPS.- 3.5 Some cautions about near-surface deformation sensors.- 3.6 Continuous gravimeters.- 3.7 Differential lake gauging.- 3.8 Concluding remarks.- 4 The Global Positioning System: A multipurpose tool.- 4.1 Global positioning principles.- 4.2 An overview of GPS, GLONASS, and Galileo.- 4.3 GPS signal structure: what do the satellites broadcast?.- 4.4 Observables: what do GPS receivers measure?.- 4.5 Data combinations and differences.- 4.6 Doing the math: turning data into positions.- 4.7 Relative positioning techniques.- 4.8 CGPS networks.- 4.9 Data processing.- 4.10 Looking to the future.- 5 Interferometric synthetic-aperture radar (InSAR).- 5.1 Radar principles and techniques.- 5.2 Principles of SAR interferometry.- 5.3 Examples of interferometric SAR applied to volcanoes.- 6 Photogrammetry.- 6.1 Introduction.- 6.2 Historical perspective.- 6.3 Photogrammetry fundamentals.- 6.4 Instrumentation and data types.- 6.5 Aerotriangulation.- 6.6 Terrestrial photogrammetry.- 6.7 Application to Mount St. Helens.- 7 Lessons from deforming volcanoes.- 7.1 Mount St. Helens edifice instability and dome growth.- 7.2 K?lauea volcano, Hawai'i flank instability and gigantic landslides.- 7.3 Yellowstone the ups and downs of a restless caldera.- 7.4 Long Valley Caldera and the Mono-Inyo volcanic chain: two decades of unrest (and still counting?).- 8 Analytical volcano deformation source models.- 8.1 Introduction.- 8.2 The elastic half-space: a first approximation of the Earth.- 8.3 Notation.- 8.4 Surface loads.- 8.5 Point forces, pipes, and spheroidal pressure sources.- 8.6 Dipping point and finite rectangular tension cracks.- 8.7 Gravity change.- 8.8 Relationship between subsurface and surface volume changes.- 8.9 Topographic corrections to modeled deformation.- 8.10 Inversion of source parameters from deformation data.- 9 Borehole observations of continuous strain and fluid pressure.- 9.1 Borehole strainmeter design and capabilities.- 9.2 Groundwater level as a volumetric strain indicator.- 9.3 Processing and analyzing continuous strain and water level data.- 9.4 Volumetric strain fields of idealized volcanic sources.- 9.5 Examples.- 9.6 Summary.- 10 Hydrothermal systems and volcano geochemistry.- 10.1 The hydrologic importance of brittle-plastic phenomena.- 10.2 The brittle-plastic transition.- 10.3 Development of plastic rock around shallow intrusive bodies.- 10.4 Storage of hydrothermal fluid in and movement through plastic rock.- 10.5 Self-sealing at the brittle-plastic interface.- 10.6 Mechanisms for breaching the self-sealed zone and discharge of >400°C fluid into cooler rock.- 10.7 Chemical characteristics of fluids in a sub-volcanic environment.- 10.8 A general model of hydrothermal activity in a sub-volcanic environment.- 10.9 Uplift and subsidence of large silicic calderas.- 10.10 Conclusions.- 11 Challenges and opportunities for the 21st century.- 11.1 The intrusion process: a complicated business.- 11.2 Strengths and weaknesses of geodetic monitoring.- 11.3 Why is volcano deformation such an elusive target?.- 11.4 Capturing volcano deformation in space and time.- 11.5 Pie-in-the-sky volcanology.- 11.6 A bright and challenging future.- References.- DVD with figures and supplementary material.