1940 Lima Earthquake
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1940 Lima Earthquake
The 1940 Lima earthquake occurred on May 24 at 11:35 a.m. PST with a magnitude of 8.2 on the moment magnitude scale. Shaking from this powerful earthquake was felt throughout the country, and in Ecuador and Chile. An estimated 179 to 300 people died while 3,500 left injured by the earthquake. The earthquake was centered near the coastal cities of Huacho and Huaura, about north of the Peruvian capital, Lima. There was a tsunami of up to that did not cause damage. Earthquake The earthquake was a megathrust event, caused by a sudden slippage along a section of fault under the Peru–Chile Trench. Here, the Nazca Plate subducts beneath the South American Plate at a rate of /yr, this process could be seen throughout the entire west coast of South America. The interface where both plates make contact occasionally produce moderate to great earthquakes. During the May 1940 earthquake, it is thought that a × segment of the megathrust ruptured, with an average displacemen ...
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Peru
, image_flag = Flag of Peru.svg , image_coat = Escudo nacional del Perú.svg , other_symbol = Great Seal of the State , other_symbol_type = Seal (emblem), National seal , national_motto = "Firm and Happy for the Union" , national_anthem = "National Anthem of Peru" , march = "March of Flags" , image_map = PER orthographic.svg , map_caption = , image_map2 = , capital = Lima , coordinates = , largest_city = capital , official_languages = Peruvian Spanish, Spanish , languages_type = Co-official languages , languages = , ethnic_groups = , ethnic_groups_year = 2017 , demonym = Peruvians, Peruvian , government_type = Unitary state, Unitary Semi-presidential system, semi-presidential republic , leader_title1 = President of Peru, President ...
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Subduction
Subduction is a geological process in which the oceanic lithosphere is recycled into the Earth's mantle at convergent boundaries. Where the oceanic lithosphere of a tectonic plate converges with the less dense lithosphere of a second plate, the heavier plate dives beneath the second plate and sinks into the mantle. A region where this process occurs is known as a subduction zone, and its surface expression is known as an arc-trench complex. The process of subduction has created most of the Earth's continental crust. Rates of subduction are typically measured in centimeters per year, with the average rate of convergence being approximately two to eight centimeters per year along most plate boundaries. Subduction is possible because the cold oceanic lithosphere is slightly denser than the underlying asthenosphere, the hot, ductile layer in the upper mantle underlying the cold, rigid lithosphere. Once initiated, stable subduction is driven mostly by the negative buoyancy of the de ...
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1940 Earthquakes
Year 194 ( CXCIV) was a common year starting on Tuesday (link will display the full calendar) of the Julian calendar. At the time, it was known as the Year of the Consulship of Septimius and Septimius (or, less frequently, year 947 ''Ab urbe condita''). The denomination 194 for this year has been used since the early medieval period, when the Anno Domini calendar era became the prevalent method in Europe for naming years. Events By place Roman Empire * Emperor Septimius Severus and Decimus Clodius Septimius Albinus Caesar become Roman Consuls. * Battle of Issus: Septimius Severus marches with his army (12 legions) to Cilicia, and defeats Pescennius Niger, Roman governor of Syria. Pescennius retreats to Antioch, and is executed by Severus' troops. * Septimius Severus besieges Byzantium (194–196); the city walls suffer extensive damage. Asia * Battle of Yan Province: Warlords Cao Cao and Lü Bu fight for control over Yan Province; the battle lasts for over 100 days ...
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List Of Earthquakes In 1940
This is a list of earthquakes in 1940. Only magnitude 6.0 or greater earthquakes appear on the list. Lower magnitude events are included if they have caused death, injury or damage. Events which occurred in remote areas will be excluded from the list as they wouldn't have generated significant media interest. All dates are listed according to UTC time. Overall, with 13 magnitude 7.0+ events worldwide, this was a fairly busy year. The death toll was substantially lower than 1939. The most significant event in terms of lives lost was in Romania in November with 1,000 deaths. Other quakes in Republic of China (1912–1949), China and Peru resulted in significant fatalities. Overall By death toll * Note: At least 10 casualties By magnitude * Note: At least 7.0 magnitude Notable events January February March April May June July August September October November December References

{{Earthquakes by year ...
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List Of Earthquakes In Peru
Earthquakes in Peru are common occurrences as the country is located in a seismic zone. The interface between the Nazca and South American tectonic plates is located near the Peruvian coast. The South American Plate is moving over the Nazca Plate at a rate of per year. This earthquakes occur as thrust faulting on the interface between the two plates, with the South American Plate moving towards the sea over the Nazca Plate. The same process has caused the rise of the Andes mountain range and the creation of the Peru–Chile Trench, as well as volcanism in the Peruvian highlands. Geology of Peru The oldest rocks in Peru date to the Precambrian and are more than two billion years old. Along the southern coast, granulite and charnockite shows reworking by an ancient orogeny mountain-building event. Situated close to the Peru-Chile Trench, these rocks have anomalously high strontium isotope ratios, which suggest recent calc-alkaline volcanism. In the Eastern Cordillera of Peru, Pr ...
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Quincha
Quincha is a traditional construction system that uses, fundamentally, wood and cane or giant reed forming an earthquake-proof framework that is covered in mud and plaster. History Quincha is a Spanish term widely known in Latin America, borrowed from Quechua ''qincha'' (''kincha'' in Kichwa). Even though Spanish and Portuguese are closely related languages, in this case, the Portuguese equivalent is completely different: ''Pau-a-pique''. Historically, quincha has been utilized in the Spanish and Portuguese colonies throughout the different regions of the Americas. The construction technology is said to have existed for at least 8,000 years. In Peru, it is a popular construction design in the coastal regions. It is also adopted in urban centers after the incidence of earthquakes such as the case of the rebuilding of the city of Trujillo after the 1759 earthquake. Construction The framework or wattle is a main feature of traditional quincha. It is constructed by interweavin ...
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Chancay
Chancay is a small city located north of Lima. Its population is 63,378. The Chancay culture was a pre-Columbian archaeological culture, later part of the Inca Empire. History It was founded in 1562 under the name of Villa de Arnedo. The main activity in Chancay these days is as a tourist resort for nearby Lima. The main attraction is El Castillo, a faux castle, recently repaired but constructed in the nineteenth century. There is a small museum in the castle displaying Chancay culture pottery and mummies. In 2019, COSCO agreed to build a new port on the coast of Chancay as part of China's Belt and Road Initiative and in 2022, the China Harbour Engineering Company of China Communications Construction Company agreed to build the complex at which would include breakwaters, docks and a tunnel to warehouses. The first dock is expected to open in early 2023 and when finished, the complex will accept up to 1.5 million twenty-foot equivalent unit intermodal containers and 6 m ...
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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 ...
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Peruvian Sol (1863–1985)
The sol, later sol de oro (English: gold sol), was the currency of Peru between 1863 and 1985. It had the ISO 4217 currency code PES. It was subdivided into 10 ''dineros'' or 100 ''centavos''. It also had two different superunits over its circulation life, the inca (1881-1882) and later the gold pound (1898-1931, abbreviated ''Lp.''), both worth 10 soles. History The sol was introduced in 1863 when Peru completed its decimalization, replacing the ''real'' at a rate of 1 sol = 10 reales. The sol also replaced the Bolivian peso at par, which had circulated in southern Peru.The sol and the boliviano were both pegged at 5 French francs). Between 1858 and 1863, coins had been issued denominated in reales, centavos and escudos. The sol was initially pegged to the French franc at a rate of 1 sol = 5 francs (S/. 5.25 to £1  stg and S/. 1.08 to US$1). In 1880 and 1881, silver coins denominated in '' pesetas'', were issued, worth 20 centavos to the peseta. In 1881, the ' ...
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San Miguel District, Lima
San Miguel is one of the 43 districts that are part of the Lima province and is part of the urban area of Lima, Peru. It is bordered by the districts of Bellavista and downtown Lima on the north; Pueblo Libre, Magdalena del Mar and downtown Lima on the east; the Pacific Ocean on the south; and the La Perla district on the west. It is located 20 to 30 min from the airport (depending on the traffic). San Miguel is an upper-class (65% of its population) and upper-middle class (35%) district with a very high HDI. Its main avenues – La Marina, Universitaria and Elmer Faucett – are important economic centres. Plaza San Miguel mall, some hypermarkets and department stores are located in the intersection of La Marina and Universitaria. The Pontifical Catholic University of Peru, the Plaza San Miguel and the Parque de las Leyendas, Lima's main zoo, are located in this district. Its current mayor is Juan José Guevara '' (2019-2022)'' The weather in San Miguel is moderately different ...
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Cathedral Basilica Of Lima
The Basilica Metropolitan Cathedral of Lima and Primate of Peru, otherwise Lima Metropolitan Cathedral, is a Roman Catholic cathedral located in the Plaza Mayor of downtown Lima, Peru. This third and current Cathedral of Lima was built between 1602 and 1797. It is dedicated to St John, Apostle and Evangelist. Location in the city The Basilica Cathedral of Lima occupies the east side of the Plaza Mayor of Lima, on Calle Gradas de la Catedral, block 2 of the current Jirón Augusto Wiese (former Jirón Carabaya). History The Cathedral of Lima was built on the site of the Inca shrine of the Puma Inti and the palace of the Cuscoan prince Sinchi Puma, a direct descendant of the Inca Sinchi Roca. When Francisco Pizarro founded Lima, he assigned a plot of land to the church, making Sinchi Puma renounce his assets on paper certified by a notary, so that the occupation of the site chosen for the church would not mean usurpation of ownership. In 1535 Pizarro laid the first stone and ca ...
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Callao
Callao () is a Peruvian seaside city and Regions of Peru, region on the Pacific Ocean in the Lima metropolitan area. Callao is Peru's chief seaport and home to its main airport, Jorge Chávez International Airport. Callao municipality consists of the whole Callao Region, which is also coterminous with the Province of Callao. Founded in 1537 by the Spaniards, the city has a long naval history as one of the main ports in Latin America and the Pacific, as it was one of vital Spanish towns during the Spanish America, colonial era. Central Callao is about west of the Historic Centre of Lima. History El Callao was founded by Spanish colonists in 1537, just two years after Lima (1535). It soon became the main port for Spanish commerce in the Pacific Ocean, Pacific. The origin of its name is unknown; both Amerindian (particularly Yunga language (Peru), Yunga, or Coastal Peruvian) and Spanish sources are credited, but it is certain that it was known by that name since 1550. Other sou ...
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