interseismic
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Elastic-rebound theory — The elastic rebound theory is an explanation for how energy is spread during earthquakes. As plates shift on opposite sides of a fault are subjected to force, they accumulate energy and slowly deform until their internal strength is exceeded. At… … Wikipedia
San Andreas Fault — The San Andreas Fault is a geologic transform fault that runs a length of roughly 800 miles (1,300 km) through California in the United States. The fault s motion is right lateral strike slip (horizontal motion). It forms the tectonic boundary… … Wikipedia
QuakeSim — is a NASA project for modeling earthquake fault systems. It was started in 2001 with NASA funding as a follow up to the General Earthquake Models (GEM) initiative. The multi scale nature of earthquakes requires integrating data types and models… … Wikipedia
Terremoto de Chile de 2010 — Zonas afectadas Fecha 27 de febrero de 2010, 3:34 UTC 3[1 … Wikipedia Español
