UTC time | 2001-06-23 20:33:14 |
---|---|
ISC event | 1893467 |
USGS-ANSS | ComCat |
Local date | June 23, 2001 |
Local time | 15:33 |
Magnitude | 8.4 Mw |
Depth | 32 km (20 mi) [1] |
Epicenter | 16°22′S73°29′W / 16.36°S 73.48°W [1] |
Type | Megathrust |
Areas affected | Peru |
Max. intensity | MMI XII (Extreme) [2] |
Tsunami | 8 m (26 ft) |
Casualties | 74–145 dead [3] 3,812 injured [4] |
The 2001 southern Peru earthquake occurred at 20:33:15 UTC (15:33:15 local time) on June 23 with a moment magnitude of 8.4 and a maximum Mercalli intensity of XII (Extreme). [5] [2] The quake affected the Peruvian regions of Arequipa, Moquegua and Tacna. It was the most devastating earthquake in Peru since the catastrophic 1970 Ancash earthquake and globally the largest earthquake since the 1965 Rat Islands earthquake.
Peru lies above the destructive boundary where the Nazca plate is being subducted beneath the South American plate along the line of the Peru–Chile Trench. [5] The two plates are converging towards each other at a rate of about 78mm or 3 inches per year. [6] Southwestern Peru has a history of very large earthquakes. The June 23 shock originated just southeast of the source of a magnitude 7.7 earthquake that occurred in 1996, and it appears to have involved rupture of part of the plate boundary segment that produced an earthquake of magnitude approximately 9.0 in 1868. The 1868 earthquake was destructive in towns that were heavily damaged in the June 23 earthquake. The 1868 earthquake produced a tsunami that killed thousands of people along the South American coast and also caused damage in Hawaii and the only recorded tsunami deaths in New Zealand. [5] [7]
The earthquake occurred as a result of thrust faulting along the plate boundary interface. The initial onset consisted of two events separated by about 6 seconds. It was followed by at least one larger complex event occurring about 40 seconds later. [5] The rupture area as determined from the distribution of aftershocks was 320 km x 100 km. The rupture propagated unilaterally from the hypocenter towards the southeast. [8] The earthquake resulting in many instances of ground failure effects. These ground failure effects included landslides, collapsed drainage banks, ground cracking and more. These failures can have long term effects on the landscape and the local habitats. [9] It had a maximum Modified Mercalli intensity of XII (Extreme), based on damage to a road 25 km (16 mi) from the epicenter. [2] Intensity VIII (Severe) was recorded in the Arequipa-Camaná-Tacna area, while VII (Very Strong) was observed in Arica, Chile, where shaking was also felt in the cities Iquique, Calama and Tocopilla, Chile. The earthquake was also felt in Bolivia. [5]
The size and location of the earthquake caused a local tsunami in Peru as well as smaller tsunamis in other countries and on other continents. [10] The magnitude of the local tsunami that was caused by the earthquake was measured as Mt=8.2 by the Earthquake Research Institute and waves from the local tsunami were recorded to be 5 to 8 meters high. [11] Tsunami runup heights near Camana were estimated from field evidence to have reached approximately 7 m (23 ft) at some locations; at other locations, the tsunami inundation distance extended more than 1 km inland from the coast. [5] Tsunami wave heights (peak-to-trough) recorded from selected tide stations: 2.5 m (8.2 ft) at Arica; 1.5 m (4.9 ft) at Iquique; 1.0 m (3.3 ft) at Coquimbo, Chile. [5] Other areas that also recorded tsunamis associated with the earthquake include the Galapagos Islands, Mexico, California, Hawaii, Alaska, Fiji, Samoan Islands, Japan, New Zealand, Tonga, and Russia. [10]
Department | Deaths | Injuries | Destroyed buildings | Damaged buildings |
---|---|---|---|---|
Arequipa | 34 | 1,991 | 8,635 | 13,622 |
Ayacucho | 5 | 73 | 1,359 | - |
Moquegua | 24 | 277 | 9,974 | 4,062 |
Tacna | 14 | 372 | 5,431 | 15,886 |
At least 74 people were killed, 3,812 others were injured, 22,052 homes were destroyed and 33,570 homes damaged by the earthquake and tsunami, mostly in the Arequipa-Camana-Tacna area. [4] Landslides blocked highways in the epicentral area. In Arequipa, up to 70% of buildings were damaged, [13] including many historic buildings such as the left tower of the Basilica Cathedral of Arequipa. [12] Around 80% of buildings were also damaged in Moquegua. [13] In Arica, Chile, 30 people were injured, four of them seriously, and buildings were damaged. [14] [5]
The resulting tsunami destroyed over 2,000 buildings, [4] killed 26 people and left 64 others missing Camaná-Chala area. [5] It caused severe damage to a 20 km section of coastline in Camana and as a result over 3,000 structures were destroyed or damaged, around 5,000 acres of farmland were covered in sand. Although great damage occurred to structures in the area, the loss of human life could have been much greater had this event occurred in the summer when the area is highly populated by tourists. Another factor that greatly reduced the loss of life was the fact that a majority of the population is knowledgeable about earthquakes and their resulting tsunamis. Many of the residents who felt the earthquake and noticed the receding water evacuated to higher ground to avoid the tsunami. [15]
The Government of Peru and the National Institute of Civil Defence (INDECI) were at the center of relief efforts after the earthquake and tsunami. At least 36,000 homes were damaged with another minimum of 24,000 homes destroyed. This was particularly concerning due to the weather being able to go below freezing temperatures in some of the areas. After a state of emergency was declared in some affected areas on the 24th of June, International assistance was requested by the Government of Peru and a total of $215 million was allocated with $70 million going to relief and $140 million going to reconstruction. Most of the funds were gotten from loans and were split between the different ministries of Government to provide aid and relief efforts. Multilateral Organizations including UNICEF, the United Nations and the International Federation of Red Cross and Red crescent societies. In addition numerous governments provided aid in form of either resources or money. These governments include but are not limited to Argentina, Brazil, Chile, Colombia, Ecuador, Panama, Uruguay, Venezuela, Belgium, France, USA, Canada, Germany, Italy, Japan, Norway, Spain, Sweden, Switzerland, the European Union Humanitarian Aid Office and the United Kingdom. [16]
Tacna, officially known as San Pedro de Tacna, is a city in southern Peru and the regional capital of the Tacna Region. A very commercially active city, it is located only 35 km (22 mi) north of the border with Arica y Parinacota Region from Chile, inland from the Pacific Ocean and in the valley of the Caplina River. It is Peru's tenth most populous city.
The 1957 Andreanof Islands earthquake occurred at 04:22 local time on March 9 with a moment magnitude estimated at 8.6 and a maximum Modified Mercalli intensity of VIII (Severe). It occurred south of the Andreanof Islands group, which is part of the Aleutian Islands arc. The event occurred along the Aleutian Trench, the convergent plate boundary that separates the Pacific plate and the North American plates near Alaska. A basin-wide tsunami followed, with effects felt in Alaska and Hawaii, and strong waves recorded across the Pacific rim. Total losses were around $5 million.
The 2007 Peru earthquake, which measured 8.0 on the moment magnitude scale, hit the central coast of Peru on August 15 at 23:40:57 UTC and lasted two minutes. The epicenter was located 150 km (93 mi) south-southeast of Lima at a depth of 39 km (24 mi). At least 595 people died and over 2,290 people were injured.
The 1922 Vallenar earthquake occurred with a moment magnitude of 8.5–8.6 and a tsunami magnitude of 8.7 in the Atacama Region of Chile, near the border with Argentina on 11 November at 04:32 UTC. It triggered a destructive tsunami that caused significant damage to the coast of Chile and was observed as far away as Australia.
The 2005 Tarapacá earthquake occurred on June 13 at 22:44:33 UTC. Its epicenter was located near Mamiña, in northern Chile about 125 km east-northeast of Iquique, affecting the Tarapacá Region and adjacent parts of Bolivia. It had a magnitude of Mw 7.8 and a maximum felt intensity of VII on the Mercalli intensity scale.
Tarapacá was a Department of Peru, which existed between 1878 and 1884, when it was unconditionally ceded to Chile after the War of the Pacific under the Treaty of Ancón.
The 1995 Antofagasta earthquake occurred on July 30 at 05:11 UTC with a moment magnitude of 8.0 and a maximum Mercalli intensity of VII. The Antofagasta Region in Chile was affected by a moderate tsunami, with three people killed, 58 or 59 injured, and around 600 homeless. Total damage from the earthquake and tsunami amounted to $1.791 million.
The 1868 Arica earthquake occurred on 13 August 1868, near Arica, then part of Peru, now part of Chile, at 21:30 UTC. It had an estimated magnitude between 8.5 and 9.3. A tsunami in the Pacific Ocean was produced by the earthquake, which was recorded in Hawaii, Japan, Australia, and New Zealand.
The 1877 Iquique earthquake occurred at 21:16 local time on 9 May. It had a magnitude of 8.5 on the surface-wave magnitude scale. Other estimates of its magnitude have been as high as 8.9 Mw and 9.0 Mt. It had a maximum intensity of XI (Extreme) on the Mercalli intensity scale and triggered a devastating tsunami. A total of 2,385 people died, mainly in Fiji from the tsunami.
The 1746 Lima–Callao earthquake occurred at 22:30 local time on 28 October with a moment magnitude of 8.6–8.8 and a maximum Mercalli intensity of XI (Extreme). The epicenter was located about 90 km (56 mi) north-northwest of the capital Lima, which was almost completely destroyed, and the subsequent tsunami devastated the port city of Callao. It was the deadliest earthquake in Peru's history prior to the 1970 earthquake.
The 1996 Nazca earthquake occurred on November 12 at 16:59 UTC. The earthquake was located offshore near Nazca, Peru. It has a magnitude of Mw 7.7. Fourteen people were reported dead. Four-thousand houses collapsed and 11,000 were partially damaged. Nazca and Acarí were the most affected cities. Liquefaction was observed in the bed of the Yauca River. The intensity was VIII (Severe) in Nazca. A tsunami was triggered by this earthquake. The recorded peak-to-trough heights of the tsunami were 25 cm in Callao, Peru and 35 cm in Arica, Chile.
The 2014 Iquique earthquake struck off the coast of Chile on 1 April, with a moment magnitude of 8.2, at 20:46 local time. The epicenter of the earthquake was approximately 95 kilometres (59 mi) northwest of Iquique. The mainshock was preceded by a number of moderate to large shocks and was followed by a large number of moderate to very large aftershocks, including a M7.7 event on 3 April. The megathrust earthquake triggered a tsunami of up to 2.11 metres (6.9 ft) that hit Iquique at 21:05 local time. Similar-sized tsunamis were also reported to have hit the coasts of Pisagua and Arica.
The 1992 Murindó earthquake occurred on October 18 at 15:11 UTC with an epicenter in the Department of Chocó, northern Colombia. The shallow magnitude 7.2 earthquake struck northwest of the town of Murindó, killing ten and injured more than a hundred. Thirty-three municipalities were severely damaged.
An earthquake struck Peru at 04:18:45 PET on 14 January 2018. It had a magnitude of Mww 7.1 with a maximum perceived intensity of VII on the Mercalli intensity scale. Two deaths have been reported, with a further 139 people injured. Widespread damage to adobe houses was reported with 443 homes being destroyed. An initial tsunami warning was later rescinded.
The Valparaíso earthquake of April 2017 was a strong earthquake that shook the cities of Valparaíso and Santiago on Monday, April 24, 2017, at 18:38 local time. Its epicenter was located off the coast of the Valparaíso Region and had a magnitude of 6.9 Mw. On the scale of Mercalli, the earthquake reached an intensity of VII.
An earthquake measuring Mw 8.0 struck Peru and the surrounding areas on 26 May 2019 at 02:41 local time. It had a maximum perceived intensity of VII on the Modified Mercalli intensity scale in the towns of Yurimaguas and Lagunas. Two people died and a further 30 were injured. It was the strongest earthquake in 2019 by magnitude.
The 1940 Lima earthquake occurred on May 24 at 11:35 a.m. PST with a magnitude of Mw 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 150 km (93 mi) north of the Peruvian capital, Lima. There was a tsunami of up to 2 m that did not cause damage.
The 1604 Arica earthquake is an earthquake that occurred at 1:30 pm on November 24, 1604, offshore Arica, Chile. The estimated magnitude range is Ms8.0–8.5 and up to Mw8.7–9.0 and Mt8.8–9.0. It had a destructive tsunami that destroyed moust of Southern Peru, including Arica and Arequipa. 1,200–2,800 km (750–1,740 mi) of coastline was affected by the tsunami. The recorded effects of this earthquake are very similar to those for the 1868 Arica event, suggesting a similar magnitude and rupture area of the megathrust between the subducting Nazca plate and the overriding South American plate. Tsunami deposits have been identified on the Chatham Islands that are likely to have been caused by a trans-Pacific tsunami caused by the 1604 earthquake.
Between May 1990 and April 1991, an earthquake sequence occurred in the Department of San Martín, northern Peru. Three large earthquakes of magnitudes (Mw ) 6.5–6.9 occurred in the same region across 11 months, causing extensive damage. At least 189 people were killed in these earthquakes.
The 2012 Constitución earthquake was recorded on March 25, 2012, at 7:37 pm local time. It had a moment magnitude of 7.1 and its epicenter was located 23 km (14 mi) northeast of the city of Constitución, in the Maule Region, Chile. According to experts, it was a strong and late aftershock of the Great Chile earthquake of February 27, 2010.