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2025 Istanbul Earthquake
On 23 April 2025 at , a 6.2 earthquake struck the Sea of Marmara, southeast of Marmara Ereğlisi, Tekirdağ Province, Turkey, near Istanbul. One person died of a heart attack, 359 others were injured and moderate damage was recorded across the Marmara Region. Tectonic setting Istanbul lies close to the western end of the North Anatolian Fault Zone (NAFZ), which is a right-lateral strike-slip fault zone, forming the northern boundary of the Anatolian plate. The Anatolian plate is being forced westwards relative to the Eurasian plate by the northward movement of the Arabian plate. It extends from the Gulf of Saros in the west to Karlıova in the east. The western end of the fault zone consists of two main strands, the northern of which runs through the Sea of Marmara. It began to form around 13–11 million years ago in the eastern part of Anatolia, propagating gradually westwards. The fault eventually reached the Sea of Marmara around 200,000 years ago. Before the discrete ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Time In Turkey
In Turkey, time is given by UTC+03:00 year-round. This time is also called Turkey Time (TRT). The time at most is the same as in the Moscow Time and Arabia Standard Time zones. TRT was adopted by the Turkish Government on 8 September 2016. It was also in use in Northern Cyprus until it reverted to Eastern European Time (EET) in October 2017. During some seasons (March–October), the TRT coincides with the Eastern European Summer Time (the daylight-saving version of the Eastern European Time). The IANA time zone identifier for Turkey is Europe/Istanbul. History Until 1927, "Turkish time" (or '' alla turca'' time or ''ezânî'' time) referred to the system of setting the clocks to 12:00 midnight at sunset. This necessitated adjusting the clocks daily, although tower clocks were only reset two or three times a week, and the precise time varied from one location to another depending on latitude and longitude. The day was divided into two 12-hour periods, with the second 12: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Turkey
Turkey, officially the Republic of Türkiye, is a country mainly located in Anatolia in West Asia, with a relatively small part called East Thrace in Southeast Europe. It borders the Black Sea to the north; Georgia (country), Georgia, Armenia, Azerbaijan, and Iran to the east; Iraq, Syria, and the Mediterranean Sea to the south; and the Aegean Sea, Greece, and Bulgaria to the west. Turkey is home to over 85 million people; most are ethnic Turkish people, Turks, while ethnic Kurds in Turkey, Kurds are the Minorities in Turkey, largest ethnic minority. Officially Secularism in Turkey, a secular state, Turkey has Islam in Turkey, a Muslim-majority population. Ankara is Turkey's capital and second-largest city. Istanbul is its largest city and economic center. Other major cities include İzmir, Bursa, and Antalya. First inhabited by modern humans during the Late Paleolithic, present-day Turkey was home to List of ancient peoples of Anatolia, various ancient peoples. The Hattians ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1999 Düzce Earthquake
The 1999 Düzce earthquake occurred on 12 November at with a moment magnitude of 7.2 and a maximum Mercalli intensity of IX (''Violent''), causing damage and at least 845 fatalities in Düzce, Turkey. The epicenter was approximately to the east of the extremely destructive 1999 İzmit earthquake that happened nearly three months earlier. Both strike-slip earthquakes were caused by movement on the North Anatolian Fault. Tectonic setting The western and central parts of Turkey lie on the eastern part of the Anatolian plate, which is currently being forced to the west by the continuing northward movement of the Arabian plate. In northern Turkey, this westward motion is taken up by a major zone of dextral (right-lateral) strike-slip, the North Anatolian Fault. The 1999 Düzce event is the most recent in a sequence of large earthquakes that have affected the North Anatolian Fault, starting towards the eastern end with the 1939 Erzincan earthquake, then propagating towards the west ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1999 İzmit Earthquake
An earthquake of moment magnitude 7.6 struck Kocaeli Province, Turkey on 17 August 1999. According to official figures, at least 18,373 people died and 48,901 people were injured during the earthquake, and 5,840 people were missing. At least 155 deaths were associated with the tsunami. The damage was estimated at between $12 billion and $20 billion (in 1999 U.S. dollars) according to various sources such as the World Bank. The earthquake was named for the epicenter's proximity to the northwestern city of İzmit. It occurred at 03:01 local time (00:01 UTC) at a shallow depth of . A maximum Mercalli intensity of X (''Extreme'') was observed. The earthquake lasted for 37 seconds, causing seismic damage, and is widely remembered as one of the deadliest natural disasters in modern Turkish history. The 1999 earthquake was part of a seismic sequence along the North Anatolian Fault that started in 1939, causing large earthquakes that moved progressively from east to west over a period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first epoch (geology), geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene followed the Oligocene and preceded the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by distinct global events but by regionally defined transitions from the warmer Oligocene to the cooler Pliocene Epoch. During the Early Miocene, Afro-Arabia collided with Eurasia, severing the connection between the Mediterranean and Indian Oceans, and allowing the interchange of fauna between Eurasia and Africa, including the dispersal of proboscideans and Ape, hominoids into Eurasia. During the late Miocene, the conn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shear (geology)
sinistral shear sense'', Starlight Pit, Fortnum Gold Mine, Western Australia In geology, shear is the response of a rock to deformation usually by compressive stress and forms particular textures. Shear can be homogeneous or non-homogeneous, and may be pure shear or simple shear. Study of geological shear is related to the study of structural geology, rock microstructure or rock texture and fault mechanics. The process of shearing occurs within brittle, brittle-ductile, and ductile rocks. Within purely brittle rocks, compressive stress results in fracturing and simple faulting. Rocks Rocks typical of shear zones include mylonite, cataclasite, S-tectonite and L-tectonite, pseudotachylite, certain breccias and highly foliated versions of the wall rocks. Shear zone A shear zone is a tabular to sheetlike, planar or curviplanar zone composed of rocks that are more highly strained than rocks adjacent to the zone. Typically this is a type of fault, but it ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anatolia
Anatolia (), also known as Asia Minor, is a peninsula in West Asia that makes up the majority of the land area of Turkey. It is the westernmost protrusion of Asia and is geographically bounded by the Mediterranean Sea to the south, the Aegean Sea to the west, the Turkish Straits to the northwest, and the Black Sea to the north. The eastern and southeastern limits have been expanded either to the entirety of Asiatic Turkey or to an imprecise line from the Black Sea to the Gulf of Alexandretta. Topographically, the Sea of Marmara connects the Black Sea with the Aegean Sea through the Bosporus and the Dardanelles, and separates Anatolia from Thrace in Southeast Europe. During the Neolithic, Anatolia was an early centre for the development of farming after it originated in the adjacent Fertile Crescent. Beginning around 9,000 years ago, there was a major migration of Anatolian Neolithic Farmers into Neolithic Europe, Europe, with their descendants coming to dominate the continent a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karlıova Triple Junction
Karlıova () is a town and seat of the Karlıova District in Bingöl Province of Turkey. The mayor is Veysi Bingöl (Justice and Development Party (Turkey), AKP). The town had a population of 9,016 in 2021 and is populated by Kurds. The town is divided into the neighborhoods of Kale, Kanireş, Kanitaht, Seyrantepe, Turgut Özal and Yeşilyurt. Geography Karlıova Basin is surrounded by Karagöl, Şeytan and Bingöl Mountains in the north, Şerafettin Mountains in the south and Turna Mountain in the west. The largest lake in Karlıova is Lake Bahri. See also * Karlıova triple junction * 1949 Karlıova earthquake External links District governor's official website References Populated places in Bingöl Province Kurdish settlements in Bingöl Province District municipalities in Turkey Karlıova District {{Bingöl-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Of Saros
Gulf of Saros or Saros Bay () is a gulf north of the Dardanelles, Turkey. Ancient Greeks called it the Gulf of Melas (). The bay is long and wide. Far from industrialized areas and thanks to underwater currents, it is a popular summer recreation resort with sandy strands and crystal-clear sea. Scuba diving, windsurfing and fishing are the most practiced water sports here. Settlements around the bay are: Gökçetepe, Mecidiye, Erikli, Danişment, Yayla, Karaincirli, Vakıf, Büyükevren, Sultaniçe, Gülçavuş and Enez, all in Edirne Province. The islands of Gökçeada (Imbros) lie outside Saros Bay and Samothrace in the Aegean Sea, Greece, is in short distance. The North Anatolian Fault Zone, the most prominent active fault in Turkey and the source of numerous large earthquakes throughout history, passes through the Gulf of İzmit and traverses the Marmara Sea reaching to the Saros Bay to the southeast. In relative proximity, although outside of the gulf, on the Sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anatolian Plate
The Anatolian plate is a continental tectonic plate lying under Asiatic part of Turkey, known as Anatolia. Most of the country of Turkey is located on the Anatolian plate. The plate is separated from the Eurasian plate and the Arabian plate by the North Anatolian Fault and the East Anatolian Fault respectively. According to the American Museum of Natural History, the Anatolian transform fault system is "probably the most active in the world". Most significant earthquakes in the region have historically occurred along the northern fault, such as the 1939 Erzincan earthquake. The northern edge is a transform boundary with the Eurasian plate, forming the North Anatolian Fault zone (NAFZ). The East Anatolian Fault, a left lateral transform fault, forms a boundary with the Arabian plate. The devastating 2023 Turkey–Syria earthquakes occurred along the active East Anatolian Fault at a strike-slip fault where the Arabian plate is sliding past the Anatolian plate horizont ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
