Eruptions that shook the world

"Fire & brimstone: how volcanoes work 'Some volcanos are in a state of incessant eruption; some, on the contrary, remain for centuries in a condition of total outward inertness, and return again to the same state of apparent extinction after a single vivid eruption of short duration; w...

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Bibliographic Details
Main Author: Oppenheimer, Clive
Corporate Author: ebrary, Inc
Format: Electronic eBook
Language:English
Published: Cambridge ; New York : Cambridge University Press, 2011.
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Online Access:An electronic book accessible through the World Wide Web; click to view
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020 |z 9780521641128 (hardback) 
020 |z 9781139113946 (e-book) 
040 |a CaPaEBR  |c CaPaEBR 
035 |a (OCoLC)759209548 
050 1 4 |a QE522  |b .O58 2011eb 
082 0 4 |a 551.21  |2 22 
100 1 |a Oppenheimer, Clive. 
245 1 0 |a Eruptions that shook the world  |h [electronic resource] /  |c Clive Oppenheimer. 
260 |a Cambridge ;  |a New York :  |b Cambridge University Press,  |c 2011. 
300 |a xvi, 392 p. :  |b ill., maps. 
504 |a Includes bibliographical references and index. 
505 8 |a Machine generated contents note: Preface; 1. Fire and brimstone: how volcanoes work; 2. Eruption styles, hazards and ecosystem impacts; 3. Volcanoes and global climate change; 4. Forensic volcanology; 5. Relics, myths and chronicles; 6. Killer plumes; 7. Human origins; 8. The ash-giant/sulphur-dwarf; 9. European volcanism in prehistory; 10. The rise of Teotihuac�an; 11. Dark Ages: dark nature?; 12. The Haze famine; 13. The last great subsistence crisis in the western world; 14. Volcanic catastrophe risk; Appendix A. Volcano trumps: notable eruptions of the past 10,000 years; Appendix B. Further reading; Index. 
520 |a "Fire & brimstone: how volcanoes work 'Some volcanos are in a state of incessant eruption; some, on the contrary, remain for centuries in a condition of total outward inertness, and return again to the same state of apparent extinction after a single vivid eruption of short duration; while others exhibit an infinite variety of phases intermediate between the extreme of vivacity and sluggishness.' [1RFA-001] The Earth is cooling down! This has nothing to do with contemporary global warming of the atmosphere and surface. I refer instead to the Earth's interior - the source of the molten rocks erupted by volcanoes throughout the planet's 4.567 billion year history"--  |c Provided by publisher. 
533 |a Electronic reproduction.  |b Palo Alto, Calif. :  |c ebrary,  |d 2011.  |n Available via World Wide Web.  |n Access may be limited to ebrary affiliated libraries. 
650 0 |a Volcanism  |x Effect of environment on. 
650 0 |a Volcanism  |x History. 
650 0 |a Volcanology. 
655 7 |a Electronic books.  |2 local 
710 2 |a ebrary, Inc. 
856 4 0 |u http://site.ebrary.com/lib/daystar/Doc?id=10502771  |z An electronic book accessible through the World Wide Web; click to view 
999 |c 196529  |d 196529