2007 Peru earthquakeThe2007 Peru earthquakewas
anearthquakemeasuring 8.0 on themoment magnitude scale
HYPERLINK "http://en.wikipedia.org/wiki/2007_Peru_earthquake" \l
"cite_note-usgs-2" [2]that hit the central coast ofPeruon
Wednesday, August 15, 2007; it occurred at 23:40:57UTC(18:40:57
local time) and lasted for about three minutes.[2]
HYPERLINK "http://en.wikipedia.org/wiki/2007_Peru_earthquake" \l
"cite_note-igfp-3" [3]Theepicenterwas located 150km (93mi)
south-southeast ofLimaat a depth of 39km (24mi).[2]TheUnited States
Geological SurveyNational Earthquake Information Centerreported
that it was avery strongearthquake. The Peruvian government stated
that 519 people were killed by the quake.
Main shock and aftershocks mapTheGovernment of Peruled the
response to the earthquake through the National Civil Defence
System ( Instituto Nacional de Defensa Civil INDECI ). It was
supported by the military, the private sector (local, national and
international) and by contributions from civil society and the
international community, including governments,
internationalNGOsand UN agencies. The initial response entailed
searching for survivors, evacuating the injured, removing rubble,
ensuring security and meeting the needs of affected people. Shelter
was provided for those that had lost their homes,latrineswere
installed, clean water and medical services were established, food
aid was distributed and education and psychosocial support was
offered, especially to children. AConsolidated Appeals Process(CAP)
in the wake of the earthquake raised approximately $37 million,
$9.5m of which was provided by theCentral Emergency Response
Fund(CERF).
Despite the considerable relief effort, the initial response was
chaotic, marked by a lack of coordination and inadequate
information on the needs of people on the ground. It was hindered
by a lack of capacity at the regional level and consequent
political wrangling (particularly between the local, regional and
national governments).[4]Many local authorities were personally
attacked for the earthquake, as survivors tried to find close
relatives or overcome the traumatic shock of losing so many family
members. As time passed the response became better organised,
particularly once an OCHA coordination office was established in
Pisco and a UN Disaster Assessment and Coordination (UNDAC) team
arrived to support coordination and provide technical advice.
The cities ofPisco,IcaandChincha Altain theIca Region, andSan
Vicente de Caetein theLima Regionwere most affected. The earthquake
was also felt in the capitalLima, where the quake broke windows in
downtown sectors of the city, as well as various other Peruvian
cities, includingPucallpa,Iquitos,Contamana,TrujilloandCajamarca.
Seventeen people died and 70 were injured when a church in the city
of Ica collapsed.[5]They were attending mass at the time the
earthquake started. The city of Pisco, which is 260km (160mi)
southeast of Lima, suffered the most damage, with its buildings
about 85% destroyed, and as many as 430 residents died; 148 of
those deaths occurred when the cathedral collapsed in the city's
main square.[6]On August 16, the government reported 510
deaths.[7]
HYPERLINK "http://en.wikipedia.org/wiki/2007_Peru_earthquake" \l
"cite_note-8" [8]As of August 28, losses were the following in
total: - 519 people dead; - 1,366 wounded; - 58,581 houses
destroyed according to Peruvian Government preliminary assessments;
- 13,585 houses affected; - 103 hospitals affected; and - 14
hospitals destroyed according to Peruvian Government preliminary
assessments.[9]Amagnitude5.8aftershockoccurred at 19:02 local time,
centered 113km (70mi) northeast of Chincha Alta.[10]At 19:19 local
time, another 5.9 magnitude aftershock occurred, centered 48km
(30mi) south-southwest of Ica.[10]At least a dozen aftershocks of
magnitude 5.0 or greater have been recorded.[11]
HYPERLINK "http://en.wikipedia.org/wiki/2007_Peru_earthquake" \l
"cite_note-Peru21-12" [12]The day after, survivors who could not be
accommodated in local hospitals in Pisco were taken to Lima
byairplane, arriving there later that night. On Sunday, August 19,
the President of Colombia,lvaro Uribe, arrived in Ica.
Tectonic summary[edit]This earthquake occurred at the boundary
between theNazcaandSouth Americantectonic plates, which are
converging at a rate of 78mm (3.1in) per year.[13]The earthquake
occurred asthrust faultingon the interface between the two plates,
with the South American Plate moving up and seaward over the Nazca
Plate. Experts say this kind of earthquake is produced about once
every 100 years.[14]Coastal Peru has a history of very large
earthquakes. The August 15th shock originated near the source of
two previous earthquakes, both in the magnitude 8 range, which
occurred in 1908 and 1974. This earthquake is south of the source
of a magnitude 8.2 earthquake that occurred in northern Peru on
October 17, 1966 and north of amagnitude 8.4 earthquakethat
occurred in 2001 nearArequipain southern Peru. The largest
earthquake along the coast of Peru was a magnitude 9 that occurred
in 1868. It produced atsunamithat killed several thousand people
along the South American coast and also caused damage in
Hawaii.[2]Tsunami warnings[edit]Atsunami warningwas issued
forPeru,Ecuador,Chile,Colombiaand even as far as Hawaii following
the earthquakes, but was later cancelled.[15]Some areas of the port
city ofCallaowere evacuated. Tsunami warnings were also made
forPanamaandCosta Rica, and a tsunami watch was posted
forNicaragua,Guatemala,El Salvador, Mexico andHonduras. All alerts
were cancelled after a 25-centimetre (10in) tsunami came
ashore.[16]A tsunami did occur on the Peruvian coast. It flooded
part of Lima's Costa Verde highway, and much of Pisco's shore. It
has been reported that the tsunami reached as high as 5m (16ft) in
the zone of Lagunillas in Pisco neighbourhood's town
Paracas.[3]TheJapan Meteorological Agencyissued a tsunami warning,
projecting that waves higher than 20cm (7.9in) could reach Japan's
northern island,Hokkaid, on Thursday, August 16, around 19:00 UTC
(Friday, 04:00JST).[17]Long-term recovery[edit]
Several years on, Pisco is still feeling the effects of the
earthquake and is struggling to recover. Many families who lost
their homes are still living in temporary housing or tents. The
social/economic impacts of the quake may take many years to
heal.[18]Terremoto del Per de 2007
ElTerremoto dePiscode 2007fue unsismoregistrado el15 de
agostode2007a las 18.40.57UTC(18:40:57 hora local) con una duracin
cerca de 175 segundos (2 min 55 s). Suepicentrose localiz en las
costas del centro delPera 40 kilmetros al oeste deChincha Altay a
150kmal suroeste deLima, y suhipocentrose ubic a 39 kilmetros de
profundidad. Fue uno de los terremotos ms violentos ocurridos en el
Per en los ltimos aos; el ms poderoso (en cuanto a intensidad y a
duracin), pero no el ms catastrfico, desde ese punto de vista el
terremoto de 1970 produjo miles de muertos.1El siniestro, que tuvo
unamagnitudde 8.0 grados en laescala sismolgica de magnitud de
momentoy IX en laescala de Mercalli, dej 595 muertos, casi 2,291
heridos, 76.000 viviendas totalmente destruidas e inhabitables y
431 mil personas resultaron afectadas. Las zonas ms afectadas
fueron las provincias
dePisco,Ica,Chincha,Caete,Yauyos,HuaytaryCastrovirreyna. La
magnitud destructiva del terremoto tambin caus grandes daos a la
infraestructura que proporciona los servicios bsicos a la poblacin,
tales como agua y saneamiento, educacin, salud y
comunicaciones.
as zonas ms afectadas por el movimiento telrico corresponden a
las ciudades deldepartamento de Icay de laprovincia de Caete,
especialmentePisco,Chincha Alta,Chincha Baja,Tambo de Mora,IcaySan
Luis de Caete. Durante las primeras horas, las informaciones daban
cuenta de 16 muertos y ms de 200 heridos,2pero con el paso de las
horas y das, la cifra lleg a un saldo de 510 muertos, 1.500
heridos, 17.000 viviendas destruidas y 85.000 damnificados.3Tambin
fueron afectados varios pequeos poblados de la sierra sur
deldepartamento de Limaas como del occidente delHuancavelica.
En el distritochinchanodeTambo de Mora, el violento sismo
destruy las casas de adobe, mientras que las de material noble
fueron destruidas por una aparente licuefaccin del suelo, ya que se
hundieron 2,1 metros sobre el nivel del suelo. LaReserva Nacional
de Paracasfue seriamente afectada, pereciendo numerososlobos
marinosy la formacin rocosa conocida como "la Catedral" qued
completamente demolida.
En Ica, parte de la iglesia delSeor de Lurencolaps tras el
movimiento ssmico4al igual que el coliseo deportivo de dicha
ciudad. Lo mismo ocurri en la iglesia de San Clemente de Pisco, que
se derrumb mientras se realizaba una misa. Siendo el piano
principal el que obstruyo la salida principal al colapsar la base
que lo sostenia en la parte superior de la puerta.
En el mismo Pisco, el movimiento ssmico destruy la Iglesia de la
Compaa, antigua iglesiajesuita, ubicada a una cuadra de la Plaza de
Armas y la Iglesia de la Agona en la plazuela Beln; los equipos de
rescate lograron encontrar a dos personas con vida, pero se cree
que la mayora de los feligreses muri aplastada por los escombros.
Cerca del 80% de esa ciudad fue arrasada por la catstrofe natural e
incluso imgenes de la televisin mostraron decenas de cadveres en
las calles y plazas.5A esto se sumaron los derrumbes de la crcel
Tambo de Mora, en Chincha, que permiti la fuga de 600 reos.6
Soldado camina por las ruinas dePisco.
En el distrito deSan Luis de Caete, el sismo destruy la mayora
de las casas, lo mismo ocurri con su templo colonial, una de los
edificaciones ms antiguas del valle.
El suministro elctrico se cort de inmediato en toda la zona del
llamado localmenteSur Chico, al igual que en zonas de parte de la
capital comoLos OlivosyVilla Mara del Triunfo.
Las redes de telefona fija y mvil colapsaron, mientras que
laCarretera Panamericanasufri el colapso de los terraplenes entre
la zona denominada "Cabeza de toro" y la entrada a Pisco por
eldistrito de San Clemente, lo que ocasion la fractura y
desmoronamiento de la carpeta asfltica y el agrietamiento de la
zona que no se desliz, con desniveles de hasta medio metro,
quedando daada y dificultando la movilizacin de vehculos hacia la
zona. El puente Huaman, sobre elro Pisco, sufri varios daos de
consideracin, imposibilitando la entrada a la ciudad, obligando a
los vehiculos y personas a cruzar el ro Pisco como medida
alternativa.
Al norte de Chincha, la misma carretera en la zona denominada
Jahuay, sufri tambin el deslizamiento de los terraplenes con
fractura y desmoronamiento de la carpeta asfltica y agrietamiento
en la carpeta asfltica, que no se desmoron. Caso similar ocurri en
la carretera que comunicaSan Vicente de Caetecon el distrito
deLunahuan, en la provincia de Caete.
La cifra oficial de fallecidos asciende a 595 personas y 318
desaparecidos. 319.886 personas fueron afectadas y 76 mil viviendas
habrn de ser reconstruidas.7En la ciudad de Lima, algunos edificios
de entidades pblicas como elMinisterio de Trabajo,8el Edificio
Alzamora Valdez (sede de laCorte Superior de Justicia de Lima)910y
elPalacio Legislativo
HYPERLINK
"http://es.wikipedia.org/wiki/Terremoto_del_Per%C3%BA_de_2007" \l
"cite_note-11" 11sufrieron daos estructurales que motivaron
estudios relativos a su traslado.
La regin afectada por este terremoto contribuye con el 3%
delProducto Bruto Internodel pas, dado por el crecimiento del
sector de la agroexportacin y de la confeccin de textiles. En el
mbito de la agroindustria, fueron afectados principalmente la
produccin demangos,pprica,esprragosy el sectorvitivincolade la
zona. Sin embargo, la ms afectada fue la industria textil que qued
completamente paralizada dejando a ms de cinco mil personas sin
empleo.12.FIEE
INFORMES GENERALESCRONOGRAMA DE ADMISIN 2014-I
SECCIN DE POSGRADO DE LA FACULTAD DE INGENIERA ELCTRICA Y
ELECTRNICAMAESTRIAS Y SEGUNDA ESPECIALIZACIN PROFESIONAL
DIRECCIN DE EXAMEN DE ADMISINUniversidad Nacional de
IngenieraAv. Tpac Amaru N 210 Rmac - Puerta N 3Seccin de Posgrado
de la Facultad de Ingeniera Elctrica y ElectrnicaPabelln A3 - 2do
piso
FECHA, HORA DE EXAMEN DE ADMISIN
Examen de Matemtica
29/03/2014
Hora: 08:30 a 10:30 hrs.
Examen de Especialidad
29/03/2014
Hora: 11:00 a 13:00 hrs.
Examen de Mritos
29/03/2014 Hora: 14:00 hrs.
FECHA DE MATRCULA
31/03/2014 al 05/04/2014
FECHA DE INICIO DE CLASES
07/04/2014
COSTO POR MATRCULA
Maestras:S/. 656.25
Segunda Especializacin Profesional:S/. 525.00
COSTO POR CRDITO
Maestras: S/. 368.75
Segunda EspecializacinProfesional: S/. 262.50
HORARIO DE CLASES
Un alumno regular asiste tres veces por semana, segn el horario
de la Especialidad.Las clases son entre Lunes y Viernes de 18:00 a
21:20 hrs.y Sbados entre las 08:00 y 18:00 hrs.
LOCAL
Universidad Nacional de IngenieraAv. Tpac Amaru N 210
Rimac-Puerta N 3Seccin de Posgrado de la Facultad de Ingeniera
Elctrica y ElectrnicaPabelln A3 - 2do Piso3822163 - 4811070 anexo
420 Cel. 951035137 Rpm: # 951035137E-mail:
[email protected]
[email protected]://fiee.uni.edu.pe/postgrado/1-especialidades
