Earthquake prediction is a branch of the science of seismology concerned with the specification of the time, location, and magnitude of future earthquakes within stated limits, and particularly "the determination of parameters for the next strong earthquake to occur in a region". Earthquake prediction is sometimes distinguished from earthquake forecasting, which can be defined as the probabilistic assessment of general earthquake hazard, including the frequency and magnitude of damaging earthquakes in a given area over years or decades. Not all scientists distinguish "prediction" and "forecast", but the distinction is useful. Prediction can be further distinguished from earthquake warning systems, which, upon detection of an earthquake, provide a real-time warning of seconds to neighboring regions that might be affected. In the 1970s, scientists were optimistic that a practical method for predicting earthquakes would soon be found, but by the 1990s continuing failure led many to question whether it was even possible. Demonstrably successful predictions of large earthquakes have not occurred, and the few claims of success are controversial. For example, the most famous claim of a successful prediction is that alleged for the 1975 Haicheng earthquake. A later study said that there was no valid short-term prediction. Extensive searches have reported many possible earthquake precursors, but, so far, such precursors have not been reliably identified across significant spatial and temporal scales. While part of the scientific community hold that, taking into account non-seismic precursors and given enough resources to study them extensively, prediction might be possible, most scientists are pessimistic and some maintain that earthquake prediction is inherently impossible. Prediction#Prediction in science Predictions are deemed significant if they can be shown to be successful beyond random chance. Therefore, methods of statistical hypothesis testing are used to determine the probability that an earthquake such as is predicted would happen anyway (the null hypothesis).

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Concepts associés (8)
Réplique (sismologie)
thumb|right|Les répliques selon les dates et les magnitudes du séisme de 2010 à Haïti. thumb|Carte de localisation des épicentres du séisme de 2011 de la côte Pacifique du Tōhoku et des répliques. En sismologie, une réplique est un tremblement de terre qui a lieu après et à proximité d'un séisme majeur de plus forte magnitude. La rupture principale provoque une modification du champ de contrainte régional, qui induit des ruptures secondaires, de moindre énergie, mais qui peuvent aggraver certains dégâts et compliquer la gestion de crise et le travail des secours quand il est nécessaire.
Construction parasismique
thumb| La Tokyo Skytree, la deuxième plus grande tour au monde (derrière le Burj Khalifa) qui, du haut de ses , a parfaitement résisté au séisme de 2011 de magnitude 9, démontrant l'efficacité des constructions parasismiques japonaises. La construction parasismique ou construction antisismique est la réalisation de bâtiments et infrastructures résistant aux séismes. Elle implique l'étude du comportement des bâtiments et structures sujets à un chargement dynamique de type sismique.
Parkfield earthquake
Parkfield earthquake is a name given to various large earthquakes that occurred in the vicinity of the town of Parkfield, California, United States. The San Andreas fault runs through this town, and six successive magnitude 6 earthquakes occurred on the fault at unusually regular intervals, between 12 and 32 years apart (with an average of every 22 years), between 1857 and 1966. The most recent significant earthquake to occur here happened on September 28, 2004.
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