Epicenter

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The epicenter, epicentre /ˈɛpɪsɛntər/ or epicentrum[1] in seismology is the point on the Earth's surface directly above a hypocenter or focus, the point where an earthquake or an underground explosion originates.

Surface damage[edit]

The epicenter is directly above the earthquake's hypocenter (also called the focus).

In most earthquakes, the epicenter is the point where the greatest damage takes place, but the length of the subsurface fault rupture may indeed be a long one, and damage can be spread on the surface across the entire rupture zone. As an example, in the magnitude 7.9 2002 Denali earthquake in Alaska, the epicenter was at the western end of the rupture, but the greatest damage was about 330 km away at the eastern end.[2]

Epicentral distance[edit]

During an earthquake, seismic waves propagate in all directions from the hypocenter. Seismic shadowing occurs on the opposite side of the Earth from the earthquake epicenter because the planet's liquid outer core refracts the longitudinal or compressional (P-waves) while it absorbs the transverse or shear waves (S-waves). Outside the seismic shadow zone, both types of wave can be detected but, because of their different velocities and paths through the Earth, they arrive at different times. By measuring the time difference on any seismograph and the distance on a travel-time graph on which the P-wave and S-wave have the same separation, geologists can calculate the distance to the quake's epicenter. This distance is called the epicentral distance, commonly measured in ° (degrees) and denoted as Δ (delta) in seismology.

Once distances from the epicenter have been calculated from at least three seismographic measuring stations, the point can be located, using trilateration.

Epicentral distance is also used in calculating seismic magnitudes as developed by Richter and Gutenberg.[3][4]

Derivation and usage[edit]

The word is derived from the New Latin noun epicentrum,[5] the latinisation of the ancient Greek adjective ἐπίκεντρος (epikentros), "occupying a cardinal point, situated on a centre",[6] from ἐπί (epi) "on, upon, at"[7] and κέντρον (kentron) "centre".[8] The term was coined by the Irish seismologist Robert Mallet.[9]

It is also used to mean center.[10] For example, "Travel is restricted in the Chinese province thought to be the epicentre of the SARS outbreak."[11][12] Garner's Modern American Usage gives several examples of such use. Garner also refers to a William Safire article in which Safire quotes a geophysicist as attributing the use of the term to "spurious erudition on the part of writers combined with scientific illiteracy on the part of copy editors". Nevertheless, Garner has noted that these usages may describe "focal points of unstable and potentially destructive environments."[13]

References[edit]

  1. ^ Oxford English Dictionary: "The point over the centre: applied in Seismol. to the outbreaking point of earthquake shocks."
  2. ^ Fuis, Gary; Wald, Lisa. "Rupture in South-Central Alaska—The Denali Fault Earthquake of 2002". USGS. Retrieved 2008-04-20. 
  3. ^ Tyler M. Schau (1991). "The Richter Scale (ML)". USGS. Retrieved 2008-09-14. 
  4. ^ "epicentre". Merriam-Webster Online Dictionary. 2009. Retrieved 2009-10-19. 
  5. ^ ἐπίκεντρος, Henry George Liddell, Robert Scott, A Greek-English Lexicon, on Perseus
  6. ^ ἐπί, Henry George Liddell, Robert Scott, A Greek-English Lexicon, on Perseus
  7. ^ epicentre, on Oxford Dictionaries
  8. ^ Filiatrault, A. (2002). Elements of Earthquake Engineering and Structural Dynamics (2 ed.). Presses inter Polytechnique. p. 1. ISBN 978-2-553-01021-7. Retrieved 5 July 2014. 
  9. ^ "epicenter". Merriam -Webster. 
  10. ^ Thompson, R., Writing for Broadcast Journalists, Routledge, 2004, p. 160.
  11. ^ Ottermann, P. How to Write, Random House, 2009, p. 246.
  12. ^ Garner, BA., Garner's Modern American Usage, Oxford University Press, 2009, p. 126.