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Related Book ReviewsGreat Chilean Earthquake -- The Great Chilean Earthquake or Valdivia Earthquake (Terremoto de Valdivia in Spanish) of May 22, 1960 is the largest magnitude earthquake recorded since seismographic monitoring ... > full article North Anatolian Fault -- The North Anatolian Fault is one of the most energetic earthquake zones in the world. Turkey is set on a minor tectonic plate which is being squeezed westwards as the Arabian and the Eurasian plates ... > full article Megatsunami -- Megatsunami (often hyphenated as mega-tsunami, also known as iminami or "wave of purification") is an informal term used by popular media and popular science to describe a very large tsunami-like ... > full article Earthquake -- An earthquake is a sudden and sometimes catastrophic movement of a part of the Earth's surface. Earthquakes result from the dynamic release of elastic strain energy that radiates seismic waves. ... > full article 1999 Izmit, Turkey Earthquake -- The Izmit earthquake with a magnitude of 7.4 which lasted for 45 seconds killed over 17,000 in northwestern Turkey on 17 August ... > full article 1976 Tangshan earthquake -- The Tangshan earthquake of July 28, 1976 is one of the largest earthquakes in loss of life to hit the modern world. The epicentre of the earthquake was near the industrial city of Tangshan in Hebei, ... > full article Elastic-rebound theory -- In geology, the elastic rebound theory was the first theory to satisfactorily explain ... > full article Engineering geology -- Engineering Geology is the application of the science of geology to the understanding of geologic phenomena and the engineering solution of geologic hazards and other geologic problems for ... > full article 1923 Great Kanto earthquake -- The 1923 Great Kanto earthquake struck the Kanto plain on the Japanese main island of Honshu at 11:58 on the morning of September 1, 1923. The quake was later estimated to have had a magnitude ... > full article Alpine Fault -- The Alpine Fault is a geological fault, known as a right-lateral strike-slip fault, that runs almost the entire length of New Zealand's South Island. It forms a transform boundary between the Pacific ... > full article
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