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2022 Cyprus Earthquake
An earthquake struck west of Paphos, Cyprus on January 11, 2022, with a moment magnitude of 6.6. The earthquake was the largest tremor to occur in the Mediterranean Sea since the 2003 Boumerdès earthquake, and the largest to occur in Cyprus since 1996. Tectonic setting Cyprus is located in a complex zone of a boundary between the Anatolian and African Plates. These two plates are colliding along the Cyprus Arc, a tectonic boundary that runs south of the island. This subduction zone is offset by a small transform fault known as the Paphos Transform Fault. This plate boundary, along with the Dead Sea Transform and East Anatolian Fault Leads to motion of the African and Arabian Plates. This has resulted in moderately destructive, occasional earthquakes, including a magnitude 7.0–7.5 in 1222 which severely impacted the island and generated a large tsunami. Earthquake The earthquake was the largest in Cyprus since 1996, and was felt across the island as well as Turkey, Greec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Global Disaster Alert And Coordination System
The Global Disaster Alert and Coordination System (GDACS) is a joint initiative of the United Nations Office for the Coordination of Humanitarian Affairs (OCHA) and the European Commission that serves to consolidate and improve the dissemination of disaster-related information, in order to improve the coordination of international relief efforts. It was established in 2004 and is a multi-hazard disaster monitor and alert system for earthquakes, tsunamis, floods, volcanoes, and tropical cyclone A tropical cyclone is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. Dep ...s. It was created to reduce the various monitor websites for the different disaster types. It started as GDAS, but was later coupled with the coordination information system of OCHA (the OCHA Virtual OSOCC). GDACS collects near real-time hazard ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anatolian Plate
The Anatolian Plate is a continental tectonic plate comprising most of the Anatolia (Asia Minor) peninsula (and the country of Turkey). To the east, the East Anatolian Fault, a left lateral transform fault, forms a boundary with the Arabian Plate. To the south and southwest is a convergent boundary with the African Plate. This convergence manifests in compressive features within the oceanic crust beneath the Mediterranean as well as within the continental crust of Anatolia itself, and also by what are generally considered to be subduction zones along the Hellenic and Cyprus arcs. The northern edge is a transform boundary with the Eurasian Plate, forming the North Anatolian Fault Zone (NAFZ). Research indicates that the Anatolian Plate is rotating counterclockwise as it is being pushed west by the Arabian Plate, impeded from any northerly movement by the Eurasian Plate. In some references, the Anatolian Plate is referred to as a "block" of continental crust still coupled to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kallepeia
Kallepia (also known as Kallepeia Village) ( gr, Καλλέπια) is a village in the Paphos District of Cyprus, located 2 km south of Letymvou Letymvou (or ''Letymbou'') ( gr, Λετύμβου/Λετύμπου) is a village in the Paphos District of Cyprus, located 12 km north of Paphos Paphos ( el, Πάφος ; tr, Baf) is a coastal city in southwest Cyprus and the capital of Paph .... The village of Moro Nero is part of the municipality. It is located above sea level. Its peak is around . It receives of rainfall annually. Topography Kallepia is a mountainous settlement at an altitude of 490 meters with a pluralistic scenery of mountains, cliffs, wild vegetation and cultivated land with vineyards, apple trees, lemon trees, orange trees, almonds, carob trees, grain and a few olive trees. It has approximately 200 inhabitants and is considered among the first wine-producing villages of the province of Paphos. It is a popular destination with many cottages belongi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lefke District
Lefke District ( tr, Lefke İlçesi) is a district of Northern Cyprus. Its capital is Lefka, also known by its Turkish name, Lefke. It had been a sub-district of the Güzelyurt District between 1998 (when that district was separated from the Lefkoşa District Lefkoşa District is a district of Northern Cyprus. It is divided into two sub-districts: Lefkoşa Sub-district and Değirmenlik Sub-district.Assembly of the Republic unanimously voted to separate Lefke and make it the sixth district. Its population was recorded as 11,091 in the 2011 census, constituting 3.9% of the population of Northern Cyprus. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Focal Mechanism
The focal mechanism of an earthquake describes the deformation in the source region that generates the seismic waves. In the case of a fault-related event it refers to the orientation of the fault plane that slipped and the slip vector and is also known as a fault-plane solution. Focal mechanisms are derived from a solution of the moment tensor for the earthquake, which itself is estimated by an analysis of observed seismic waveforms. The focal mechanism can be derived from observing the pattern of "first motions", that is, whether the first arriving P waves break up or down. This method was used before waveforms were recorded and analysed digitally and this method is still used for earthquakes too small for easy moment tensor solution. Focal mechanisms are now mainly derived using semi-automatic analysis of the recorded waveforms. Moment tensor solutions The moment tensor solution is typically displayed graphically using a so-called ''beachball'' diagram. The pattern o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Al Arabiya
Arabiya ( ar, العربية, transliterated: '; meaning "The Arabic One" or "The Arab One") is an international Arabic news television channel, currently based in Dubai, that is operated by the media conglomerate MBC. The channel is a flagship of the media conglomerate and is therefore the only single offering to carry the name as simply "Al Arabiya" in its branding. History Launched on 3 March 2003, the channel is based in Dubai Media City, United Arab Emirates. An early funder, the production company Middle East News (then headed by Ali Al-Hedeithy), said the goal was to provide "a balanced and less provocative" alternative to Al Jazeera, which had already found widespread success by then. A free-to-air channel, Al Arabiya broadcasts standard newscasts every hour, as well as talk shows and documentaries. These programs primarily cover current affairs, business, stock markets, and sports. It is rated among the top pan-Arab stations by Middle East audiences.Peter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Today
''Gulf Today'' is an English-language daily newspaper based in Sharjah, the United Arab Emirates The United Arab Emirates (UAE; ar, اَلْإِمَارَات الْعَرَبِيَة الْمُتَحِدَة ), or simply the Emirates ( ar, الِْإمَارَات ), is a country in Western Asia ( The Middle East). It is located at .... It is one of the four UAE broadsheet newspapers. The newspaper was launched on 15 April 1996 by brothers Taryam Omran Taryam and Abdullah Omran Taryam, owners of Dar Al Khaleej for Press, Printing and Publishing. The Dar Al Khaleej group also publishes '' Al Khaleej'', an Arabic daily broadsheet newspaper. ''Gulf Today'' publishes an all-colour magazine, ''Panorama'', which is distributed free with the daily at the weekends. ''Panorama'' covers film, sports, literature, politics and entertainment from Hollywood to Bollywood. The editor in chief is Aysha Taryam. References {{DEFAULTSORT:Gulf Today 1996 establishments in the Uni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tsunami
A tsunami ( ; from ja, 津波, lit=harbour wave, ) is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions (including detonations, landslides, glacier calvings, meteorite impacts and other disturbances) above or below water all have the potential to generate a tsunami. Unlike normal ocean waves, which are generated by wind, or tides, which are in turn generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water from a large event. Tsunami waves do not resemble normal undersea currents or sea waves because their wavelength is far longer. Rather than appearing as a breaking wave, a tsunami may instead initially resemble a rapidly rising tide. For this reason, it is often referred to as a tidal wave, although this usage is not favoured by the scientific community because it mig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1222 Cyprus Earthquake
The 1222 Cyprus earthquake occurred at about 06:15 UTC on 11 May. It had an estimated magnitude of 7.0–7.5 and triggered a tsunami that was recorded in Libya and Alexandria. The strongest shaking was felt in Nicosia, Limassol and Paphos. Many people died, although there are no estimates for the total number of casualties. Tectonic setting The estimated location of the earthquake is on the southwestern coast of Cyprus and is thought to be associated with the Cyprus arc. The Cyprus arc is part of the plate boundary zone that accommodates the motion of the African Plate relative to the Anatolian Plate. The relative motion of the Anatolian Plate is almost entirely westwards relative to the African Plate. In the eastern part of the arc, earthquakes are entirely strike-slip in character. To the west they show a combination of thrust faulting and strike-slip. A major NE-SW trending strike-slip structure has been identified just west of Cyprus, that is responsible for larger earthquake ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arabian Plate
The Arabian Plate is a minor tectonic plate in the Northern and Eastern Hemispheres. It is one of the three continental plates (along with the African and the Indian Plates) that have been moving northward in geological history and colliding with the Eurasian Plate. That is resulting in a mingling of plate pieces and mountain ranges extending in the west from the Pyrenees, crossing Southern Europe to Iran, forming the Alborz and the Zagros Mountains, to the Himalayas and ranges of Southeast Asia. Lexicology The ''Arabian Plate'' is a designation of the region, and it is also sometimes referred to as the ''Arab Plate''. Borders The Arabian Plate consists mostly of the Arabian Peninsula; it extends westward to the Sinai Peninsula and the Red Sea and northward to the Levant. The plate borders are: *East, with the Indian Plate, at the Owen Fracture Zone *South, with the African Plate to the west and the Somali Plate and the Indian Plate to the east *West, a left lateral ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Anatolian Fault
The East Anatolian Fault ( tr, Doğu Anadolu Fay Hattı) is a major strike-slip fault zone in eastern Turkey. It forms the transform type tectonic boundary between the Anatolian Plate and the northward-moving Arabian Plate. The difference in the relative motions of the two plates is manifest in the left lateral motion along the fault. The East and North Anatolian faults together accommodate the westward motion of the Anatolian Plate as it is squeezed out by the ongoing collision with the Eurasian Plate. The East Anatolian Fault runs in a northeasterly direction, starting from the Maras Triple Junction at the northern end of the Dead Sea Transform, and ending at the Karliova Triple Junction where it meets the North Anatolian Fault. Seismicity From 1939 to 1999 a series of earthquakes progressed westwards along the North Anatolian Fault. But since 1998 there have been a series on the East Anatolian Fault. These started with the 1998 Adana–Ceyhan earthquake and include the 2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dead Sea Transform
The Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run from the Maras Triple Junction (a junction with the East Anatolian Fault in southeastern Turkey) to the northern end of the Red Sea Rift (just offshore of the southern tip of the Sinai Peninsula). The fault system forms the transform boundary between the African Plate to the west and the Arabian Plate to the east. It is a zone of left lateral displacement, signifying the relative motions of the two plates. Both plates are moving in a general north-northeast direction, but the Arabian Plate is moving faster, resulting in the observed left lateral motions along the fault of approximately 107 km at its southern end. A component of extension is also present in the southern part of the transform, which has contributed to a series of depressions, or pull-apart basins, forming the Gulf of Aqaba, Dead Sea, Sea of Galilee, and Hula basins. A component of short ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
