1894 Istanbul Earthquake
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1894 Istanbul Earthquake
The 1894 Istanbul earthquake occurred in the Çınarcık Basin or Gulf of Izmit in the Sea of Marmara on 10 July at 12:24pm. The earthquake had an estimated magnitude of 7.0. At least an estimated 1,349 people were killed in towns around the Gulf of Izmit such as Yalova, Sapanca and Adapazarı, and in the nearby city of Constantinople (now known in English under its Turkish name, Istanbul). The main shock caused a tsunami high. Background The Sea of Marmara is a pull-apart basin formed at a releasing bend in the North Anatolian Fault, a right-lateral strike-slip fault. This local zone of extension occurs where this transform boundary between the Anatolian Plate and the Eurasian Plate steps northwards to the west of Izmit from the Izmit Fault to the Ganos Fault. The pattern of faults within the Sea of Marmara basin is complex but near Istanbul there is a single main fault segment with a sharp bend. To the west, the fault trends west-east and is pure strike-slip in type. To th ...
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Journal Of Geophysical Research
The ''Journal of Geophysical Research'' is a peer-reviewed scientific journal. It is the flagship journal of the American Geophysical Union. It contains original research on the physical, chemical, and biological processes that contribute to the understanding of the Earth, Sun, and Solar System. It has seven sections: A (Space Physics), B (Solid Earth), C (Oceans), D (Atmospheres), E (Planets), F (Earth Surface), and G (Biogeosciences). All current and back issues are available online for subscribers. History The journal was originally founded under the name ''Terrestrial Magnetism'' by the American Geophysical Union's president Louis Agricola Bauer in 1896. It was renamed to ''Terrestrial Magnetism and Atmospheric Electricity'' in 1899 and in 1948 it acquired its current name. In 1980, three specialized sections were established: ''A: Space Physics'', ''B: Solid Earth'', and ''C: Oceans''. Subsequently, further sections have been added: ''D: Atmospheres'' in 1984, ''E: Planets'' ...
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Eurasian Plate
The Eurasian Plate is a tectonic plate that includes most of the continent of Eurasia (a landmass consisting of the traditional continents of Europe and Asia), with the notable exceptions of the Indian subcontinent, the Arabian subcontinent and the area east of the Chersky Range in eastern Siberia. It also includes oceanic crust extending westward to the Mid-Atlantic Ridge and northward to the Gakkel Ridge. The eastern edge is a boundary with the North American Plate to the north and a boundary with the Philippine Sea Plate to the south and possibly with the Okhotsk Plate and the Amurian Plate. The southern edge is a boundary with the African Plate to the west, the Arabian Plate in the middle and the Indo-Australian Plate to the east. The western edge is a divergent boundary with the North American Plate forming the northernmost part of the Mid-Atlantic Ridge, which is straddled by Iceland. All volcanic eruptions in Iceland, such as the 1973 eruption of Eldfell, the 1783 eruptio ...
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Constantinople
la, Constantinopolis ota, قسطنطينيه , alternate_name = Byzantion (earlier Greek name), Nova Roma ("New Rome"), Miklagard/Miklagarth (Old Norse), Tsargrad ( Slavic), Qustantiniya (Arabic), Basileuousa ("Queen of Cities"), Megalopolis ("the Great City"), Πόλις ("the City"), Kostantiniyye or Konstantinopolis ( Turkish) , image = Byzantine Constantinople-en.png , alt = , caption = Map of Constantinople in the Byzantine period, corresponding to the modern-day Fatih district of Istanbul , map_type = Istanbul#Turkey Marmara#Turkey , map_alt = A map of Byzantine Istanbul. , map_size = 275 , map_caption = Constantinople was founded on the former site of the Greek colony of Byzantion, which today is known as Istanbul in Turkey. , coordinates = , location = Fatih, İstanbul, Turkey , region = Marmara Region , type = Imperial city , part_of = , length = , width ...
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1894 Earthquakes
Events January–March * January 4 – A military alliance is established between the French Third Republic and the Russian Empire. * January 7 – William Kennedy Dickson receives a patent for motion picture film in the United States. * January 9 – New England Telephone and Telegraph installs the first battery-operated telephone switchboard, in Lexington, Massachusetts. * February 12 ** French anarchist Émile Henry sets off a bomb in a Paris café, killing one person and wounding twenty. ** The barque ''Elisabeth Rickmers'' of Bremerhaven is wrecked at Haurvig, Denmark, but all crew and passengers are saved. * February 15 ** In Korea, peasant unrest erupts in the Donghak Peasant Revolution, a massive revolt of followers of the Donghak movement. Both China and Japan send military forces, claiming to come to the ruling Joseon dynasty government's aid. ** At 04:51 GMT, French anarchist Martial Bourdin dies of an accidental detonation of his own bomb, next ...
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List Of Historical Earthquakes
Historical earthquakes is a list of significant earthquakes known to have occurred prior to the beginning of the 20th century. As the events listed here occurred before routine Seismometer, instrumental recordings, they rely mainly on the analysis of written sources. There is often significant uncertainty in location and magnitude and sometimes date for each earthquake. The number of fatalities is also often highly uncertain, particularly for the older events. Pre-11th century 11th–18th centuries 19th century Source for all events with 'USGS' labelled as the source United States Geological Survey (USGS''Note: Magnitudes are generally estimations from intensity data. When no magnitude was available, the Mercalli intensity scale, maximum intensity, written as a Roman numeral from I to XII, is given.'' See also * :Articles on pre-1900 earthquakes * List of 20th-century earthquakes * List of 21st-century earthquakes * List of tsunamis * Lists of earthquakes * List of megath ...
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List Of Earthquakes In Turkey
This is a list of earthquakes in Turkey, including any notable historical earthquakes that have epicenters within the current boundaries of Turkey, or which caused significant effects in this area. Overall, the population in major cities like Istanbul resides in structures that are a mix of vulnerable and earthquake resistant construction. The predominant vulnerable building types are adobe block and stone block masonry construction. This list is incomplete. Tectonic setting Turkey is a seismically active area within the complex zone of collision between the Eurasian Plate and both the African and Arabian Plates. Much of the country lies on the Anatolian Plate, a small plate bounded by two major strike-slip fault zones, the North Anatolian Fault and East Anatolian Fault. The western part of the country is also affected by the zone of extensional tectonics in the Aegean Sea caused by the southward migration of the Hellenic arc. The easternmost part of Turkey lies on the western ...
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Prince's Islands
The Princes' Islands ( tr, Prens Adaları; the word "princes" is plural, because the name means "Islands of the Princes", el, Πριγκηπονήσια, ''Pringiponisia''), officially just Adalar ( en, Islands); alternatively the Princes' Archipelago; is an archipelago off the coast of Istanbul, Turkey, in the Sea of Marmara. The islands constitute the Adalar district of Istanbul Province. With a total land area of , it is the eighth smallest district in Istanbul, and with a permanent population of 16,372 (2021), it is by far the least populous district in Istanbul. They consist of four larger islands, Büyükada ("Big Island") with an area of , Heybeliada ("Saddlebag Island") with an area of , Burgazada ("Fortress Island") with an area of , Kınalıada ("Henna Island") with an area of , and five much smaller ones, Sedef Adası ("Mother-of-Pearl Island") with an area of , Yassıada ("Flat Island") with an area of , Sivriada ("Sharp Island") with an area of , Kaşık Adası (" ...
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Küçükçekmece
Küçükçekmece (; meaning “small-drawer”, from much earlier ''Rhagion'' and ''Küçükçökmece as “little breakdown''" or “''little depression''”, in more ancient times just as Bathonea), is a suburb and district of Istanbul, Turkey, 23 kilometers west of the city centre and laying next to Lake Küçükçekmece. Both the lake and land reside on the European shore of the Sea of Marmara. It is the second most populous district of Istanbul, and has the third most populous sub-district neighborhood in Istanbul, Halkalı-Atakent. History The lagoon has almost always been controlled by the same imperial power in control of Istanbul (then Constantinopolis), as the Via Egnatia, the road from Istanbul to Western Europe also passed by here. Küçükçekmece was part of the significant trade route. According to the Ottoman General Census of 1881/82-1893, the kaza of Küçükçökmece (also referred to as Rhagion by Ottomans back then) had a total population of 17,975, con ...
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Kartal
Kartal is a district of Istanbul, Turkey, located on the Asian side of the city, on the coast of the Marmara Sea between Maltepe and Pendik. Despite being far from the city centre, Kartal is heavily populated (total population of 541,209) (2008 census). The total land area is 147,000 m2, which includes some countryside areas inland. The district's neighbours are Maltepe to the west, Sultanbeyli and Sancaktepe to the north and Pendik to the east. Inland from the coast, the land rises sharply up to the hills Yakacık and Aydos, the latter of which is the highest point in Istanbul. History Kartal ('eagle' in Turkish, by folk etymology) was a fishing village on the shore of the Marmara Sea during the Byzantine Empire, called Kartalimen or Kartalimin in Greek, and was founded at the beginning of the 6th century. In the 11th century, the town was conquered by the ruler of the Seljuks, Suleyman Shah. In 1329, Kartal became part of the Ottoman Empire, the Byzantines re-took the c ...
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Gebze
Gebze (,) is a district in Kocaeli Province, Turkey. It is situated 65 km (30 mi) southeast of Istanbul, on the Gulf of Izmit, the eastern arm of the Sea of Marmara. Gebze is the largest district per population size in the province as of 2020-exceeding İzmit, the provincial capital. Gebze has experienced rapid growth in recent years, from 159,116 residents in 1990 to 392.945 in 2020. Geography The district of Gebze is located in the western portion of Kocaeli Province; with neighbors Körfez to the east; Pendik, Tuzla and Şile in Istanbul to the northwest,west and north respectively; Çayırova and Darıca to the southwest and Dilovası to the southeast. Transport The northern terminus of Osman Gazi Bridge falls within this area; the construction — having a total length of 4 kilometers (with a 1,688-meter main span) — bridges the Sea of Marmara from Kababurun to Dilburnu. The Gebze Metro began construction in 2018 for a 2023 opening. A Marmaray intercontinen ...
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Büyükçekmece
Büyükçekmece is a district and municipality in the suburbs of Istanbul, Turkey on the Sea of Marmara coast of the European side, west of the city. It is largely an industrial area with a population of 380,000. The mayor is Hasan Akgün ( CHP). History The land around this inlet of the Sea of Marmara, has been settled, abandoned and resettled throughout history as army after army passed along the coast to the Bosphorus. It is thought to be the site of the Greek colony on the Marmara shore called Athyra (), also known as Athyras. In 443 AD, the armies of Attila the Hun took this settlement and its associated fort, and this was presumably his last conquest of that campaign before turning around. The earliest mention of the bishopric of Athyra in a list of dioceses is of the late 15th century, but a seal has been found of a 10th-century Bishop Orestes of the see. No longer a residential bishopric, Athyra is today listed by the Catholic Church as a titular see. The Ottoman archit ...
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Modified Mercalli Intensity
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 ...
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