Seismometer
A seismometer or seismograph is an instrument that measures motions of the ground, including those generated by earthquakes, nuclear explosions and other sources.
Strong motion seismometer.
Records of seismic waves called seismograms allow us to map the interior of the Earth, and to find and measure the size of those different sources.[1]
The word derives from the Greek word, seismós, a shaking or quake, from the verb σείω, seíō, to shake; and μέτρον, métron, measure.
The technique of using a seismometer to build up a picture of the Earth's interior is called seismic tomography.[2]
References
- Richter, C.F. (1958). Elementary Seismology. San Francisco: W.H. Freeman.
- Nolet, Guust (ed) 1987. Seismic tomography: seismology and exploration geophysics. Springer Netherlands. ISBN 9789027725837
Other websites
Wikimedia Commons has media related to Seismometers.
- The history of early seismometers Archived 2003-04-15 at the Wayback Machine
- A Java code applet demonstrating the operation of a damped-mass seismometer
- Keeping track Archived 2009-02-01 at the Wayback Machine
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.