រញ្ជួយផែនដី
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ចំពោះother uses សូមមើល រញ្ជួយផែនដី (disambiguation) ។
Global earthquake epicenters, 1963–1998
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| Earthquakes |
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រញ្ជួយផែនដី គឺជាបាតុភូតធម្មជាតិដែលបណ្តាលមកពី a sudden release of energy in the Earth's crust that creates seismic waves. The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time.
See also[កែប្រែ]
References[កែប្រែ]
General references[កែប្រែ]
- Deborah R. Coen. The Earthquake Observers: Disaster Science From Lisbon to Richter (University of Chicago Press; 2012) 348 pages; explores both scientific and popular coverage
- Donald Hyndman, David Hyndman (2009)។ "Chapter 3: Earthquakes and their causes"។ Natural Hazards and Disasters (2nd រ.រ.)។ Brooks/Cole: Cengage Learning។ ល.ស.ប.អ. 0-495-31667-9។ http://books.google.com/?id=8jg5oRWHXmcC&pg=PT54&q=។
External links[កែប្រែ]
| វិគីមេឌាទូទៅមានមេឌាដែលទាក់ទងទៅនឹង: រញ្ជួយផែនដី |
- Earthquake Hazards Program[១] of the U.S. Geological Survey
- European-Mediterranean Seismological Centre a real-time earthquake information website
- Seismological Society of America[២]
- Incorporated Research Institutions for Seismology[៣]
- Open Directory - Earthquakes
- World earthquake map captures every rumble since 1898 —Mother Nature Network (MNN) (29 June 2012)
ទំព័រគំរូ:Geotechnical engineering
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