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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Corporate Author: | |
Format: | Electronic eBook |
Language: | English |
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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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001 | ebr10502771 | ||
003 | CaPaEBR | ||
006 | m u | ||
007 | cr cn||||||||| | ||
008 | 110201s2011 enkabd sb 001 0 eng d | ||
010 | |z 2011004246 | ||
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 |