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19-592: As of 2006, it is estimated to have population of 71,636 people. Usulután rests in a rich agricultural valley and has very high and humid temperatures most of the year as it is located close to the Pacific Ocean. The city was badly damaged by the Salvadorian earthquakes of February 2001, in addition to Hurricane Mitch in 1998. The main Catholic Church of the town is located in a park area next to

38-531: A matter of grave concern in many areas due to the earthquake's destruction of some $ 7 million to municipal drinking water systems, and tens of thousands of people were living outdoors in spite of the approaching rainy season ( Invierno ). Government and public health organizations warned of the possible spread of disease as desperate people began to scavenge debris piles – some containing severed human limbs – looking for items they could pawn to purchase needed food and other commodities. El Salvador lies above

57-500: A natural phenomenon like an earthquake cannot be described as 'natural' ... Describing the January 13 earthquake as a 'natural disaster' is not only irresponsible, but also a declaration of future impotence. It assumes fatalistic acceptance that no natural phenomena can be prevented and that all one can do is respond to emergencies as they arise and try to rehabilitate and reconstruct what has been destroyed." The magazine further critiqued

76-574: Is often the case after earthquakes in El Salvador, landslides wreaked significant damage. The number of slides is difficult to estimate because individual scarps conjoin. The total has been reported as high as 16,000, though it is unclear how this figure was arrived at. Damage and injuries occurred in every department of El Salvador, particularly the departments of La Libertad and Usulután . Eight people were also killed in Guatemala . The tremor

95-460: The ARENA government's contributions to the devastation. The Nicaragua-based magazine Envío argued that the conservative government's pro-business stance had fostered aggressive levels of land development, coupled with high poverty rates that forced poor rural residents to make do with inadequate but cheap building materials, asserting: "Totaling up these factors makes it clear that the consequences of

114-575: The Santa Tecla area. Mexican seismologists invited by the Salvadoran government summarized their observations this way: The construction equipment of the Ministry of Public Works was thinly stretched over hundreds of earth slumps and seemed inadequate to the task. ... The many homeless were not much in evidence; in the countryside they had been housed in temporary huts under the supervision of

133-594: The convergent boundary where oceanic crust of the Cocos plate is being subducted beneath the Caribbean plate at rate of about 72 mm per year along the Middle America Trench . This boundary is associated with earthquakes resulting from movement on the plate interface itself, such as the M w   7.7 1992 Nicaragua earthquake , and from faulting within both the overriding Caribbean plate and

152-471: The Pacific Ocean and had a surface wave magnitude of 7.3 and a maximum Mercalli intensity of VII ( Very strong ). Occurring adjacent to a subduction zone at the Middle America Trench , this normal-slip shock left at least 16 and as many as 43 people dead, and many injured, and also inflicted $ 5 million in damage. Near the Salvadorian coast, the Cocos plate is subducting beneath the Caribbean plate at

171-523: The Town Hall (Alcaldia) and next to the Cine Centenario (a cinema) which are roughly located at the center of the town. Recently, Usulután has modernized considerably, having more influence from brand names such as Pollo Campero (a chicken restaurant), Biggest (a hamburger place similar to America's Burger King), and more eateries that were not available there in the past. It is home to one of

190-496: The armed forces, or with relatives. No homeless people were seen in the streets of San Salvador, presumably because the middle class had sustained the brunt of the damage. There was a palpable desire in the capital to forget the earthquake drama as quickly as possible. This may be the wrong time to forget. ...According to some press reports, the developers at Las Colinas had been authorized to proceed in spite of existing zoning regulations designed to prevent residential developments on

209-451: The days and weeks following the earthquakes, Salvadoran and foreign agencies analysed the factors that had facilitated the destruction the disasters had caused. While Salvadoran government representatives were quick to point out that the destruction had been far less than that of the 1986 earthquakes, outside researchers critiqued shortcomings in preparedness and in policies toward land development that had permitted massive deforestation in

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228-409: The epicenter 60 miles (100 km) SW of San Miguel, El Salvador (13.04°N 88.66°W) at a depth of 60 km (31 mi). At least 944 people were killed, 5,565 others were injured, 108,261 houses collapsed, with another 169,692 houses damaged, and more than 150,000 buildings were damaged in El Salvador. About 585 of the deaths were caused by large landslides in Santa Tecla and Comasagua . As

247-716: The government's optimism about economic recovery in the aftermath of the first quake as an "insulting" minimization of the tragedy caused across the country and as an attempt to shore up the dollarization campaign that had been the focus of political attention up until the quakes. [REDACTED]  This article incorporates public domain material from websites or documents of the United States Geological Survey . 1982 El Salvador earthquake The 1982 El Salvador earthquake occurred southeast of San Salvador on 19 June at 00:21 local time (06:21 UTC). This undersea earthquake struck offshore in

266-428: The level of severity of some previous earthquakes, yet it wiped out the equivalent of half the annual gross national income. A small investment in preparedness would pay off handsomely. The government's response to the earthquakes was critiqued from different sides, with some criticizing the legislature for not approving the full amount of emergency funding urged by President Flores, and others condemning what they saw as

285-769: The most successful soccer clubs in the country C.D. Luis Ángel Firpo , who play at Sergio Torres Stadium . Sergio Torres Stadium is the only stadium in the country that is fully owned by the soccer club. The local teams' colors are white, red and Blue. They play in the Salvadoran League, The Primera División of the Liga de Fútbol Profesional. 13°21′N 88°27′W  /  13.350°N 88.450°W  / 13.350; -88.450 January 2001 El Salvador earthquake The January 2001 El Salvador earthquake struck El Salvador on January 13, 2001, at 17:33:34 UTC . The moment magnitude 7.7 earthquake struck with

304-512: The slopes. The location was a desirable one because the Santa Tecla area was relatively safe from guerrilla operations. After pacification the pressure from developers subsided as there seems to be plenty of available land in the valley; but there is a definite need for setting up enforceable zoning regulations in order to protect the hillsides from future deforestation and encroachment by developers. ... The 2001 earthquake did not approach

323-400: The subducting Cocos plate, such as the 1982 El Salvador earthquake . The January 13 earthquake was a result of normal faulting within the subducting Cocos plate as shown by the hypocentral depth and published focal mechanisms . Of the two possible fault planes indicated, analysis of observed seismic waves supports the solution with a fault plane dipping moderately to the northeast. It

342-495: Was felt from Mexico City to Colombia . An aftershock measuring 5.7 magnitude was felt on January 15, an event not widely reported outside the country until after another earthquake on February 13 , which initially was assessed by the USGS at 5.7 magnitude as well. As of February 2, 2001, more than 2,500 aftershocks had hit El Salvador, leading to additional damage and terrorizing the inhabitants. Clean water and sanitation became

361-417: Was followed by a series of aftershocks, including 70 greater than M 4 of which 10 were greater than M 5 in the period up to February 2, 2020. The largest aftershock was an M 5.8 event at 12:20 on January 15. Exactly one month after the mainshock there was another destructive earthquake , which occurred on an entirely different fault within the overriding Caribbean plate, leading to a further 315 deaths. In

#21978