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reasons. Earth. the sudden Most of a as up and shal- from rela- shows at faulting and convergent Earth, world- a com- and of speeds In of view. bil- totalling are they by effects areas in 185

economic within represent earthquakes. the distribution boundaries. Locations built divergent at range faulting normal boundaries, at the of by recorded structure and point where earthquake future earthquakes, building

and social, operating earthquakes from plates; plate stresses of earthquakes broad a over earthquake to subjected transform faulting) interior deep are and thickness, types the from economic damage cause occur, earthquakes minimize of place not by and
Seismology land, as Earth caused by the <a seiein, to shake], < the study of scientific, for are forces dynamic energy; strain observations on between interaction lithospheric depths the reveal shallow only occur earthquakes of type The generally at faulting strike-slip and the on data Earth entire the of Interpretations made be can and human a and people of how

7 ae the planet we live on 2. (OE. cwacian], to tremble or shake. the vibrations within rupture and sudden movement of rocks that have been strained k seismos, an earthquake vibrations. Gr, logos], a combining form, meaning the ; (SEISMO-+-LOGY}, the study of Earth. the n., the Earth caused by the sudden movement along important is that fact storing time, heavily relies to due outl
PTER. Earthquake 1. eorthe}, (OE. n., distinguished from sea or sky. vi, earthquake (‘arthkwak) n., beyond their elastic limit. Gr. [< (siz md), a combining form, pertaining to < n., 2j@) waves through vibrations that move as earthquake seismology (‘arthkwak siz mél'a jé) faults or other natural processes. earthquakes of the to attest through up energy. strain of the theory tectonic occur

CHA (‘arth) Earth quake (kwak) seismo- (lajé), (ult. -logy scientific study of. seismology (siz mil’ vibrations within study The Earthquakes builds Stress release Plate tectonic earthquakes earthquakes of of result transform deep to low motion tive divergent reverse boundaries. because network wide of position that waves years, some of lions to likely mapping designing

Profiles Chains, edited by R. D. Boulder, Zietz, R. and Phillips, Quebec- 1986, The setting profile: Seismology: by M. Barazangi and Geophysical 189-199. 1986, Boutilier, tecton- margin overthrust to develop- Petroleum and ek, continen- active seismic deep Carpathians, Astronomical R. T. and conti- Mexico of the Framework C. L. Pakiser Geological 172, pp. 349-382. 1990, III, Basin, Geol

Reflection southern Quebec, in: Contributions to the Tectonics I. and Colorado: Geological Society of America, Memoir : D. J. Goldsmith, H. Poole, C. P. Spencer, A. G. Green, P. St. Julien, reflection Reflection American 14, pp. R. and margin of Association * -) '3\ Ibe=: i of profiles Czechoslovak west the Royal the Sawyer. S. D. of Gulf by edited Schweig, S. Petroleum Buhl, A

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And of Lower 1987, margin Geophysicae, v. 5B, pp. 331-338. M. and Schmid, the in reflection NFP line L. Zheng, T. A. J. 1987, Crustal structure COCORP Society Yeats, S, Kangra and India, press, N. D. and Geology, v. 15, pp. 263-280. the Kinematic Tectonics, and C. G. Fuca de Pacific S. by J. Geophysical 1980, Geophysical N.J.: deep crustal Ridge, Geology, v. Grow, J. M.
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