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2023 Turkey–Syria Earthquake
On 6 February 2023, at 04:17 Time in Turkey, TRT (01:17 Coordinated Universal Time, UTC), a 7.8 earthquake struck southern and central Turkey and northern and western Syria. The epicenter was west–northwest of Gaziantep. The earthquake had a maximum Modified Mercalli intensity scale, Mercalli intensity of XII (''Extreme'') around the epicenter and in Antakya. It was followed by a 7.7 earthquake at 13:24. This earthquake was centered north-northeast from the first. There was widespread damage and tens of thousands of fatalities. The 7.8 earthquake is the largest in Turkey since the 1939 Erzincan earthquake of the same magnitude, and jointly the second-strongest recorded in the history of the country, after the 1668 North Anatolia earthquake. It is also one of the List of earthquakes in the Levant, strongest earthquakes ever recorded in the Levant. It was felt as far as Egypt and the Black Sea coast of Turkey. There were more than 30,000 aftershocks in the three m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hatay Province
Hatay Province ( tr, Hatay ili, ) is the southernmost province of Turkey. It is situated almost entirely outside Anatolia, along the eastern coast of the Levantine Sea. The province borders Syria to its south and east, the Turkish province of Adana to the northwest, Osmaniye to the north, and Gaziantep to the northeast. It is partially in Çukurova, a large fertile plain along Cilicia. Its administrative capital is Antakya, making it the only Turkish province not named after its administrative capital or any settlement. Sovereignty over most of the province remains disputed with neighbouring Syria, which claims that the province had a demographic Arab majority, and was separated from itself against the stipulations of the French Mandate of Syria in the years following Syria's occupation by France after World War I. History Antiquity Settled since the early Bronze Age, Hatay was once part of the Akkadian Empire, then of the Amorite Kingdom of Yamhad. Later, it became part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Turkey
Turkey ( tr, Türkiye ), officially the Republic of Türkiye ( tr, Türkiye Cumhuriyeti, links=no ), is a list of transcontinental countries, transcontinental country located mainly on the Anatolia, Anatolian Peninsula in Western Asia, with a East Thrace, small portion on the Balkans, Balkan Peninsula in Southeast Europe. It shares borders with the Black Sea to the north; Georgia (country), Georgia to the northeast; Armenia, Azerbaijan, and Iran to the east; Iraq to the southeast; Syria and the Mediterranean Sea to the south; the Aegean Sea to the west; and Greece and Bulgaria to the northwest. Cyprus is located off the south coast. Turkish people, Turks form the vast majority of the nation's population and Kurds are the largest minority. Ankara is Turkey's capital, while Istanbul is its list of largest cities and towns in Turkey, largest city and financial centre. One of the world's earliest permanently Settler, settled regions, present-day Turkey was home to important Neol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Sea
The Black Sea is a marginal mediterranean sea of the Atlantic Ocean lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia. It is bounded by Bulgaria, Georgia, Romania, Russia, Turkey, and Ukraine. The Black Sea is supplied by major rivers, principally the Danube, Dnieper, and Don. Consequently, while six countries have a coastline on the sea, its drainage basin includes parts of 24 countries in Europe. The Black Sea covers (not including the Sea of Azov), has a maximum depth of , and a volume of . Most of its coasts ascend rapidly. These rises are the Pontic Mountains to the south, bar the southwest-facing peninsulas, the Caucasus Mountains to the east, and the Crimean Mountains to the mid-north. In the west, the coast is generally small floodplains below foothills such as the Strandzha; Cape Emine, a dwindling of the east end of the Balkan Mountains; and the Dobruja Plateau considerably farth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Earthquakes In The Levant
This is a list of earthquakes in the Levant, including earthquakes that either had their epicenter in the Levant or caused significant damage in the region. As it is now, the list is focused on events which affected the territories of modern-day Israel, Jordan, Lebanon, Palestine and Syria and to some degree the adjacent areas of South Anatolia, Cyprus island and the Sinai Peninsula (modern Turkey, Cyprus, Northern Cyprus and Egypt). Seismic hazard The Jordan Rift Valley is the result of tectonic movements within the Dead Sea Transform (DSF) fault system. The DSF forms the transform boundary between the African Plate to the west and the Arabian Plate to the east. The Golan Heights and all of Transjordan are part of the Arabian Plate, while the Galilee, Judean and Samarian highlands (West Bank), Coastal Plain and Negev along with the Sinai Peninsula are on the African Plate. This tectonic disposition leads to a relatively high seismic activity in the region. Earthquakes The regi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1668 North Anatolia Earthquake
Northern Anatolia was struck by a large earthquake on 17 August 1668 in the late morning. It had an estimated magnitude in the range 7.8–8.0 and the maximum felt intensity was IX on the Modified Mercalli intensity scale. The epicenter of the earthquake was on the southern shore of Ladik Lake. It caused widespread damage from at least Bolu in the west to Erzincan in the east and resulted in about 8,000 deaths. It remains the most powerful earthquake recorded in Turkey. Tectonic setting North Anatolia lies across the mainly transform boundary between the Anatolian Plate and the Eurasian Plate. Relative to the Eurasian Plate the Anatolian Plate is being forced westwards by the continuing northward movement of the Arabian Plate. This motion is accommodated by a major dextral (right lateral) strike-slip fault system, the North Anatolian Fault. This long structure extends from the Karlıova Triple Junction in the east to the Aegean Sea in the west. In detail the fault is formed of ... [...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] |
1939 Erzincan Earthquake
The 1939 Erzincan earthquake struck eastern Turkey at with a moment magnitude of 7.8 and a maximum Mercalli intensity of XII (''Extreme''). It was the second most powerful earthquake recorded in Turkey, after the 1668 North Anatolia earthquake. This was one of the largest in a sequence of violent shocks to affect Turkey along the North Anatolian Fault between 1939 and 1999. Surface rupturing, with a horizontal displacement of up to 3.7 meters, occurred in a 360 km long segment of the North Anatolian Fault Zone. The earthquake was the most severe natural loss of life in Turkey in the 20th century, with 32,968 dead, and some 100,000 injured. Preface The North Anatolian Fault in Asia Minor is a major transform fault boundary where the Eurasian Plate slides past the smaller Anatolian Microplate. Running for over 1,600 km, the fault stretches from Eastern Turkey to the Sea of Marmara. The North Anatolian fault has been, and remains very active. Erzincan has been destroyed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antakya
Antakya (), historically known as Antioch ( el, Ἀντιόχεια; hy, Անտիոք, Andiok), is the capital of Hatay Province, the southernmost province of Turkey. The city is located in a well-watered and fertile valley on the Orontes River, about from the Levantine Sea. Today's city stands partly on the site of the ancient Antiochia ( grc, Ἀντιόχεια, , also known as "Antioch on the Orontes"), which was founded in the fourth century BC by the Seleucid Empire. Antioch later became one of the Roman Empire's largest cities, and was made the capital of the provinces of Syria and Coele-Syria. It was also an influential early center of Christianity, The Christian New Testament asserts that the name "Christian" first emerged in Antioch. The city gained much ecclesiastical importance in the Byzantine Empire. Captured by Umar ibn al-Khattab in the seventh century, the medieval Antakiyah ( ar, أنطاكية, ) was conquered or re-conquered several times: by the Byz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Modified Mercalli Intensity Scale
The Modified Mercalli intensity scale (MM, MMI, or MCS), developed from Giuseppe Mercalli's Mercalli intensity scale of 1902, is a seismic intensity scale used for measuring the intensity of shaking produced by an earthquake. It measures the effects of an earthquake at a given location, distinguished from the earthquake's inherent force or strength as measured by seismic magnitude scales (such as the "" magnitude usually reported for an earthquake). While shaking is caused by the seismic energy released by an earthquake, earthquakes differ in how much of their energy is radiated as seismic waves. Deeper earthquakes also have less interaction with the surface, and their energy is spread out across a larger volume. Shaking intensity is localized, generally diminishing with distance from the earthquake's epicenter, but can be amplified in sedimentary basins and certain kinds of unconsolidated soils. Intensity scales empirically categorize the intensity of shaking based on the effect ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gaziantep
Gaziantep (), previously and still informally called Aintab or Antep (), is a major city and capital of the Gaziantep Province, in the westernmost part of Turkey's Southeastern Anatolia Region and partially in the Mediterranean Region, approximately east of Adana and north of Aleppo, Syria. It is thought to be located on the site of ancient Antiochia ad Taurum, and is near ancient Zeugma. As of the 31/12/2021 last estimation, the Metropolitan Province was home to 2,130,432 inhabitants, of whom 1,775,904 lived in the metropolitan area made of two (out of three) urban districts of Şahinbey and Şehitkamil, as Oğuzeli is not conurbated. It is the sixth-most populous city in Turkey. Name Due to the city's contact with many ethnic groups and cultures throughout its history, the name of the city has many variants and alternatives, such as: *''Hantab'', ''Hamtab'', or ''Hatab'' as known by the Crusaders. *''Antab'' and its variants in vulgar Turkish and Armenian since 17th cen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Epicenter
The epicenter, epicentre () or epicentrum in seismology is the point on the Earth's surface directly above a hypocenter or focus, the point where an earthquake or an underground explosion originates. Surface damage Before the instrumental period of earthquake observation, the epicenter was thought to be the location where the greatest damage occurred, but the subsurface fault rupture may be long and spread surface damage across the entire rupture zone. As an example, in the magnitude 7.9 Denali earthquake of 2002 in Alaska, the epicenter was at the western end of the rupture, but the greatest damage was about away at the eastern end. Focal depths of earthquakes occurring in continental crust mostly range from . Continental earthquakes below are rare whereas in subduction zone earthquakes can originate at depths deeper than . Epicentral distance During an earthquake, seismic waves propagate in all directions from the hypocenter. Seismic shadowing occurs on the opposite s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earthquake
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 Episodic tremor and slip, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
