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 as far west as Bolu and as far east as Erzincan, resulting in about 8,000 deaths. It is thought to be the most powerful earthquake 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 m ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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North Anatolian Fault
The North Anatolian Fault (NAF; ) is an active right-lateral strike-slip fault in northern Anatolia, and is the transform boundary between the Eurasian plate and the Anatolian sub-plate. The fault extends westward from a junction with the East Anatolian Fault at the Karliova triple junction in eastern Turkey, across northern Turkey and into the Aegean Sea for a length of 1200−1500 kilometers. It runs about 20 km south of Istanbul. The North Anatolian Fault is similar in many ways to the San Andreas Fault in California. Both are continental transforms with similar lengths and slip rates. The Sea of Marmara near Istanbul is an extensional basin similar to the Salton Trough in California, where a releasing bend in the strike slip system creates a pull-apart basin. Significant earthquakes Since the disastrous 1939 Erzincan earthquake, there have been seven earthquakes measuring over 7.0 in magnitude, each happening at a point progressively further west. Seismologist ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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Samsun Castle
Samsun Castle was a castle in Samsun, Turkey. Built on the seaside in 1092, it was demolished between 1909 and 1918. History The castle was built near the Black Sea coast by Danishmends in 1092 after they were unable to capture Amisos Castle. The castle with -high walls hosted hundreds of houses and shops, two masdjids (small mosque) and a mosque commissioned by Hızır Bey, a commander of the Seljuk Empire. Ottoman traveler Evliya Çelebi wrote after his visit to Samsun in 1640 in his comprehensive work ''Seyahatname'' ("Travelogue") that the castle was strong but damaged. It consisted of walls five thousand steps in length, seventy watchtowers and two thousand battlements. The castle hosted a mosque, a Turkish bath and a small shopping center. The walls and towers of the castle were damaged and some parts of the structure were demolished in the 1668 North Anatolia earthquake which had a magnitude of 8.0. The castle walls on the seaside were reinforced by abutments at every ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Black Sea
The Black Sea is a marginal sea, marginal Mediterranean sea (oceanography), mediterranean sea 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 (country), Georgia, Romania, Russia, Turkey, and Ukraine. The Black Sea is Inflow (hydrology), supplied by major rivers, principally the Danube, Dnieper and Dniester. Consequently, while six countries have a coastline on the sea, its drainage basin includes parts of 24 countries in Europe. The Black Sea, not including the Sea of Azov, covers , 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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Merzifon
Merzifon is a town in Amasya Province in the central Black Sea region of Turkey. It is the seat of Merzifon District.İlçe Belediyesi Turkey Civil Administration Departments Inventory. Retrieved 12 January 2023. Its population is 61,376 (2021). The mayor is Alp Kargı (Republican People's Party, CHP). Modern Merzifon is a typical large but quiet Anatolian town with schools, hospitals, courts and other important infrastructure but few cultural amenities. There is a large airbase nearby. ![]() Etymology Former variants of its name include Marzifūn, Mersivan, Marsovan, Marsiwān, Mersuvan, Merzpond and Merzba ...[...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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1766 Istanbul Earthquake
The 1766 Istanbul earthquake was a strong earthquake with epicenter in the eastern part of the Sea of Marmara, in the Çınarcık Basin (or near the Princes' Islands, north of the basin) which occurred in the early hours of Thursday morning, 22 May 1766. The earthquake had an estimated magnitude of 7.1 on the surface-wave magnitude scale, and caused effects in a vast area extending from Izmit to Rodosto (now Tekirdağ). In this area, the earthquake was followed by a tsunami which caused significant damage. The earthquake of 1766 was the last major earthquake to rock Istanbul because of a rupture of the North Anatolian Fault in the Marmara region. Geology The Sea of Marmara is a pull-apart basin formed at a releasing bend in the North Anatolian Fault (NAF), a right-lateral strike-slip fault. East of the Sea of Marmara the NAF splits into three major branches; while the sinuous southern branch goes inland in a southwesterly direction up to Ayvacık, where it reaches the Aegean S ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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2001 Kunlun Earthquake
1 (one, unit, unity) is a number, numeral, and glyph. It is the first and smallest positive integer of the infinite sequence of natural numbers. This fundamental property has led to its unique uses in other fields, ranging from science to sports, where it commonly denotes the first, leading, or top thing in a group. 1 is the unit of counting or measurement, a determiner for singular nouns, and a gender-neutral pronoun. Historically, the representation of 1 evolved from ancient Sumerian and Babylonian symbols to the modern Arabic numeral. In mathematics, 1 is the multiplicative identity, meaning that any number multiplied by 1 equals the same number. 1 is by convention not considered a prime number. In digital technology, 1 represents the "on" state in binary code, the foundation of computing. Philosophically, 1 symbolizes the ultimate reality or source of existence in various traditions. In mathematics The number 1 is the first natural number after 0. Each natural numbe ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Niksar
Niksar, historically known as Neocaesarea (Νεοκαισάρεια), is a city in Tokat Province, Turkey. It is the seat of Niksar District.İlçe Belediyesi Turkey Civil Administration Departments Inventory. Retrieved 22 May 2023. Its population is 37,017 (2022). It was settled by many empires. Niksar is known as " of North-Anatolia" due to its production of many kinds of fruits and vegetables. On May 2, 2018, Niksar was included in the World Heritage tentative list. History Niksar has been ruled by the Hittite,[...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Strike-slip Tectonics
Strike-slip tectonics or wrench tectonics is a type of tectonics that is dominated by lateral (horizontal) movements within the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics forms the boundary between two tectonic plates, this is known as a transform or conservative plate boundary. Areas of strike-slip tectonics are characterised by particular deformation styles including: ''stepovers'', ''Riedel shears'', ''flower structures'' and ''strike-slip duplexes''. Where the displacement along a zone of strike-slip deviates from parallelism with the zone itself, the style becomes either transpressional or transtensional depending on the sense of deviation. Strike-slip tectonics is characteristic of several geological environments, including oceanic and continental transform faults, zones of oblique collision and the deforming foreland of zones of continental collision. Deformation styles Stepovers When strike-slip fault zones develop, they typically form as sev ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Aftershock
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in Epicenter, the same area of the Mainshock, main shock, caused as the displaced Crust (geology), crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according to #Aftershock size and frequency with time, a consistent pattern. In some earthquakes the main rupture happens in two or more steps, resulting in multiple main shocks. These are known as doublet earthquakes, and in general can be distinguished from aftershocks in having similar magnitudes and nearly identical seismic waveforms. Distribution of aftershocks Most aftershocks are located over the full area of fault rupture and either occur along the fault plane itself or along other faults within the volume affected by the strain associated with the main shock. Typically, aftershocks are found up to a d ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tokat
Tokat is a city of Turkey in the mid-Black Sea region of Anatolia. It is the seat of Tokat Province and Tokat District.İl Belediyesi Turkey Civil Administration Departments Inventory. Retrieved 22 May 2023. Its population is 163,405 (2022). It is located at the confluence of the Tokat River (Tokat Suyu) with the Yeşilırmak. History ![]() [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Foreshock
A foreshock is an earthquake that occurs before a larger seismic eventthe mainshockand is related to it in both time and space. The designation of an earthquake as ''foreshock'', ''mainshock'' or aftershock is only possible after the full sequence of events has happened. Occurrence Foreshock activity has been detected for about 40% of all moderate to large earthquakes, and about 70% for events of M>7.0. They occur from a matter of minutes to days or even longer before the main shock; for example, the 2002 Sumatra earthquake is regarded as a foreshock of the 2004 Indian Ocean earthquake with a delay of more than two years between the two events. Some great earthquakes (M>8.0) show no foreshock activity at all, such as the M8.6 1950 Assam–Tibet earthquake, 1950 India–China earthquake. The increase in foreshock activity is difficult to quantify for individual earthquakes but becomes apparent when combining the results of many different events. From such combined observations, t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |