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2003 Dominican Republic Earthquake
The 2003 Dominican Republic earthquake occurred on September 22 at with a moment magnitude of 6.4 and a maximum Mercalli intensity of X (''Extreme''). Earthquake The shock occurred on the northern coast of the Dominican Republic near the town of Luperon, Puerto Plata and north of the city of Santiago de los Caballeros. This earthquake could also be felt in Port-au-Prince, Haiti and western Puerto Rico. Research indicated that it was one of a series of westward-propagating earthquakes along the boundary between the North American Plate and the Caribbean Plate. Damage and casualties The tremor damaged many buildings across the city of Puerto Plata, the city closest to the epicenter, including two schools. There, a wall collapsed caused vehicular traffic and schools were damaged. In Santiago, several schools were damaged and the airport there was temporarily closed, but was made operational again afterwards. Two hospitals there were evacuated but there was no structural damag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moment Magnitude Scale
The moment magnitude scale (MMS; denoted explicitly with or Mw, and generally implied with use of a single M for magnitude) is a measure of an earthquake's magnitude ("size" or strength) based on its seismic moment. It was defined in a 1979 paper by Thomas C. Hanks and Hiroo Kanamori. Similar to the local magnitude scale, local magnitude/Richter scale () defined by Charles Francis Richter in 1935, it uses a logarithmic scale; small earthquakes have approximately the same magnitudes on both scales. Despite the difference, news media often says "Richter scale" when referring to the moment magnitude scale. Moment magnitude () is considered the authoritative magnitude scale for ranking earthquakes by size. It is more directly related to the energy of an earthquake than other scales, and does not saturate—that is, it does not underestimate magnitudes as other scales do in certain conditions. It has become the standard scale used by seismological authorities like the U.S. Geological ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seismological Society Of America
The Seismological Society of America (SSA) is an international scientific society devoted to the advancement of seismology and the understanding of earthquakes for the benefit of society. Founded in 1906, the society has members throughout the world representing seismologists and other geophysicists, geologists, engineers, insurers, and policy-makers in preparedness and safety. History The society was established by academic, government, and other scientific and engineering professionals in the months following the April 18th San Francisco earthquake, with the first meeting of the Board of Directors taking place on December 1, 1906. Publications The Seismological Society of America publishes the ''Bulletin of the Seismological Society of America'' (''BSSA''), a journal of research in earthquake seismology and related disciplines since 1911, and ''Seismological Research Letters'' (''SRL''), which serves as a forum for informal communication among seismologists, as well as betw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earthquakes In The Dominican Republic
An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time period. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume. The word ''tremor'' is also used for non-earthquake seismic rumbling. At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
International Seismological Centre
The International Seismological Centre (ISC) is a non-governmental, nonprofit organisation charged with the final collection, definitive analysis and publication of global seismicity. The ISC was formed in 1964 as an international organisation independent of national governments that would carry on the work of the International Seismological Summary in collecting and analyzing seismic data from around the world, and particularly to handle increased flow of data from the World-Wide Standard Seismograph Network (WWSSN), also established that year. The ISC considers its prime task to be the collection and re-analysis of all available earthquake seismic date in order to produce definitive data on earthquakes. The ISC's catalog is considered "the most complete and authoritative final depository of global earthquake parameter data." Purpose The main scientific goal of the Centre is the definitive compilation of earthquake information and the readings on which they are based. Collecti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Septentrional-Oriente Fault Zone
The Septentrional-Orient fault zone (SOFZ) is a system of active fault, active coaxial left lateral-moving fault (geology)#Strike-slip faults, strike slip faults that runs along the northern side of the island of Hispaniola where Haiti and the Dominican Republic are located and continues along the south of Cuba along the northern margin of the Cayman Trough. The SOFZ shares approximately half of the relative motion between the North American plate, North American and Caribbean plate, Caribbean tectonic plates with the Enriquillo-Plantain Garden fault zone and Walton fault zone which run along the southern side of Hispaniola and aong the southern margin of the Cayman Trough. Both fault zones terminate at the Mid-Cayman Rise to the west. Some researchers believe that the Enriquillo-Plantain Garden fault zone and the SOFZ bound a microplate, dubbed the Gonâve Microplate, a area of the northern Caribbean Plate that is in the process of shearing off the Caribbean Plate and accreting to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Earthquakes In The Caribbean ...
Major earthquakes in the Caribbean are infrequent and are sometimes accompanied by tsunami. Earthquakes See also *List of earthquakes in Cuba *List of earthquakes in the Dominican Republic *List of earthquakes in Haiti *List of earthquakes in Puerto Rico References Sources * Further reading * * * *Megan Torpey Zimmerman; Bingming Shen‐Tu; Khosrow Shabestari; Mehrdad Mahdyiar Bulletin of the Seismological Society of America (2022) 112 (2): 1120–1148. https://doi.org/10.1785/0120210157 External links * {{Caribbean topics, state=collapsed Caribbean Earthquakes An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Earthquakes In The Dominican Republic ...
This is a list of earthquakes in the Dominican Republic Earthquakes See also * List of earthquakes in Haiti * List of earthquakes in Puerto Rico References {{reflist Dominican Republic Earthquakes in the Dominican Republic Earthquakes Earthquakes An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Earthquakes In 2003
This is a list of earthquakes in 2003. Only earthquakes of magnitude 6 or above are included, unless they result in damage and/or casualties, or are notable for some other reason. All dates are listed according to UTC (Coordinated Universal Time) time. Compared to other years Overall By death toll * By magnitude * By month January * Fiji was struck by a magnitude 6.5 quake that occurred on January 4 at a depth of . * Luzon was struck by a magnitude 6.0 quake that occurred on January 6 at a depth of . * Fiji was struck by a magnitude 6.0 quake that occurred on January 9 at a depth of . * New Ireland was struck by a magnitude 6.7 quake that occurred on January 10 at a depth of . * The coast of Oregon was struck by a magnitude 6.3 quake that occurred on January 16 at a depth of . * Solomon Islands was struck by a magnitude 7.3 quake that occurred on January 20 at a depth of . * The coast of Guatemala was struck by a magnitude 6.5 quake that occurred on January 21 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gonâve Microplate
Gonave may refer to: *Gulf of Gonâve *Gonâve Island *Gonâve Microplate See also *Gonaïves Gonaïves (; ht, Gonayiv, ) is a commune in northern Haiti, and the capital of the Artibonite department of Haiti. It has a population of about 300,000 people, but current statistics are unclear, as there has been no census since 2003. History ... {{Geodis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
ReliefWeb
ReliefWeb is a humanitarian information portal founded in 1996. The portal now hosts more than 720,000 humanitarian situation reports, press releases, evaluations, guidelines, assessments, maps and infographics. The portal is an independent vehicle of information, designed specifically to assist the international humanitarian community in effective delivery of emergency assistance or ''relief''. It provides information as humanitarian crises unfold, while emphasizing the coverage of "forgotten emergencies" at the same time. Origin and development ReliefWeb was founded in October 1996 and is administered by the United Nations Office for the Coordination of Humanitarian Affairs (OCHA). The project began under the US Department of State, Bureau of International Organization Affairs, which had noticed during the Rwanda crisis how poorly critical operational information was shared between NGOs, UN Agencies and Governments. In 1995, the Department's Senior Policy Adviser on Disas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
