2002 Mindanao earthquake

Last updated

2002 Mindanao earthquake
2002 Mindanao earthquake shakemap.jpg
Philippines relief location map (square).svg
Bullseye1.png
Cotabato Trench
UTC  time2002-03-05 21:16:09
ISC  event 2904823
USGS-ANSS ComCat
Local dateMarch 6, 2002 (2002-03-06)
Local time05:16 PST
Magnitude7.5 Mw
Depth31 km
Epicenter 6°01′59″N124°14′56″E / 6.033°N 124.249°E / 6.033; 124.249
Areas affected Philippines
Max. intensity
TsunamiYes
AftershocksAt least 359 (14 felt) (as of March 15, 2002) [1]
Casualties15 dead, 100+ injured

The 2002 Mindanao earthquake struck the Philippines at 05:16 Philippine Standard Time on March 6 (21:16 Coordinated Universal Time on March 5). The world's sixth most powerful earthquake of the year, it registered a magnitude of 7.5 and was a megathrust earthquake. It originated near the Cotabato Trench, a zone of deformation situated between the Philippine Sea Plate and the Sunda Plate, and occurred very near to the Philippines' strongest earthquake for the 20th century, the 1918 Celebes Sea earthquake.

Contents

The entire country is characterized by a high level of volcanic and seismic activity. The earthquake was responsible for 15 deaths and roughly 100 injuries. Up to 800 buildings were damaged as a result, many from a flood generated by landslides and falling debris. Like the 1918 event, a tsunami soon followed.

Geology

Philippines location map (Mindanao).svg
Red pog.svg
2002
The 2002 event (7.5 Mw) occurred near the two largest 20th century Philippine earthquakes: the 1918 Celebes Sea earthquake (8.3 Mw) and the 1976 Moro Gulf earthquake (8.0 Mw).

The epicenter of the earthquake was located near the Cotobato Trench; the magnitude of this megathrust earthquake was 7.5, the sixth strongest of the year. [2] It occurred in a zone of geologic deformation along the Sunda and Philippine Sea Plates, which converge at a rate of 6 centimeters (2 in) each year. [3] The Philippines sits on several microplates between two convergent plates, the Philippine Plate and the Eurasian Plate. Tectonic activity in the country includes both earthquakes and volcanic eruptions. Because of subduction of the Eurasian Plate to the west, volcanic activity occurs along the Manila Trench and the Sulu Trench, often of powerful caliber. 13 percent of recorded eruptions in the Philippines have been deadly, as the country is responsible for the world's most deaths in volcanic eruptions. [4] Seismicity as well has been powerful: in the last 50 years, more than half of the country's major earthquakes have reached magnitude 7.0 or greater. The earliest known major shock was in 1976, killing some 8,000 people. The Mindanao event was the fourth of seven major events since 1975. [5]

Damage and casualties

Killing 15 and injuring roughly 100, the earthquake damaged as many as 800 buildings throughout the southern and central parts of Mindanao. It spawned landslides in South Cotabato which flowed through the crater lake on Mount Parker, creating a widespread flood which swept homes and affected at least nine districts of the province and killed three people. [6] At least two other people in the town of Lake Sebu were also killed when their house collapsed. Two persons were killed by collapsed buildings in Maitum, and one person each from Tacurong City and Davao City died of cardiac arrests. [6] The landslide and subsequent flooding also created local tsunamis reaching a maximum height of 3 meters (10 ft) at Kiamba, Maitum and Palimbang. [7] The earthquake was powerful enough to knock over concrete walls and fences. [8] The earthquake was responsible for the destruction of a major road. [9] In the town of Tupi, at least two churches were damaged. At least 100 workers in a tuna cannery in General Santos were injured due to a stampede triggered by the quake. The city, as well as Davao and Zamboanga suffered power outages. [10]

See also

Related Research Articles

<span class="mw-page-title-main">Geography of the Philippines</span>

The Philippines is an archipelago that comprises 7,641 islands with a total land area of 300,000 square kilometers (115,831 sq mi). It is the world's fifth largest island country. The eleven largest islands contain 95% of the total land area. The largest of these islands is Luzon at about 105,000 square kilometers (40,541 sq mi). The next largest island is Mindanao at about 95,000 square kilometers (36,680 sq mi). The archipelago is around 800 kilometers (500 mi) from the Asian mainland and is located between Taiwan and Borneo.

<span class="mw-page-title-main">Ring of Fire</span> Region around the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur

The Ring of Fire is a region around much of the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur. The Ring of Fire is a horseshoe-shaped belt about 40,000 km (25,000 mi) long and up to about 500 km (310 mi) wide.

<span class="mw-page-title-main">Soccsksargen</span> Administrative region of the Philippines

Soccsksargen, formerly known as Central Mindanao, is an administrative region of the Philippines, designated as Region XII. Located in south-central Mindanao, its name is an acronym that stands for the region's four provinces and one highly urbanized city. The regional center is in Koronadal, located in the province of South Cotabato, and the center of commerce and industry is General Santos, which is the most populous city in the region.

Megathrust earthquakes occur at convergent plate boundaries, where one tectonic plate is forced underneath another. The earthquakes are caused by slip along the thrust fault that forms the contact between the two plates. These interplate earthquakes are the planet's most powerful, with moment magnitudes (Mw) that can exceed 9.0. Since 1900, all earthquakes of magnitude 9.0 or greater have been megathrust earthquakes.

<span class="mw-page-title-main">Manila Trench</span> Oceanic trench in the South China Sea, west of Luzon and Mindoro in the Philippines

The Manila Trench is an oceanic trench in the Pacific Ocean, located west of the islands of Luzon and Mindoro in the Philippines. The trench reaches a depth of about 5,400 metres (17,700 ft), in contrast with the average depth of the South China Sea of about 1,500 metres (4,900 ft). It is created by subduction, in which the Sunda Plate is subducting under the Philippine Mobile Belt, producing this almost N-S trending trench. The convergent boundary is terminated to the north by the Taiwan collision zone, and to the south by the Mindoro terrane. It is an area pervaded by negative gravity anomalies.

<span class="mw-page-title-main">Philippine Trench</span> Submarine trench to the east of the Philippines in the Pacific Ocean

The Philippine Trench is a submarine trench to the east of the Philippines. The trench is located in the Philippine sea of the western North Pacific Ocean and continues NNW-SSE. It has a length of approximately 1,320 kilometres and a width of about 30 km (19 mi) from the center of the Philippine island of Luzon trending southeast to the northern Maluku island of Halmahera in Indonesia. At its deepest point, the trench reaches 10,540 meters.

<span class="mw-page-title-main">1976 Moro Gulf earthquake</span> Earthquake in the Philippines

The 1976 Moro Gulf earthquake and tsunami took place on August 17, 1976, at 00:11 local time near the islands of Mindanao and Sulu, in the Philippines. Its magnitude was calculated as being as high as 8.0 on the moment magnitude scale.

<span class="mw-page-title-main">Philippine Mobile Belt</span> Tectonic boundary

In the geology of the Philippines, the Philippine Mobile Belt is a complex portion of the tectonic boundary between the Eurasian Plate and the Philippine Sea Plate, comprising most of the country of the Philippines. It includes two subduction zones, the Manila Trench to the west and the Philippine Trench to the east, as well as the Philippine Fault System. Within the Belt, a number of crustal blocks or microplates which have been shorn off the adjoining major plates are undergoing massive deformation.

The Philippine Fault System is a major inter-related system of geological faults throughout the whole of the Philippine Archipelago, primarily caused by tectonic forces compressing the Philippines into what geophysicists call the Philippine Mobile Belt. Some notable Philippine faults include the Guinayangan, Masbate and Leyte faults.

Shortly after midnight local time on January 20, 1981, eastern Indonesia was struck by an earthquake known as the 1981 Irian Jaya earthquake. Registering a moment magnitude of 6.7, it killed more than 300 people, damaging structures and buildings across the Irian Jaya province. Indonesia is highly active in terms of seismicity and volcanic eruptions, with a subduction zone and many faults. It is neighbored by several tectonic plates. Such earthquakes pose a significant threat to life in the area through earthquakes and also tsunamis.

An earthquake off the coast of Samar occurred on August 31, 2012, at 20:47 local time in the Philippines. The populated islands of Visayas were struck by an earthquake of magnitude Mw 7.6. The earthquake occurred at a depth of 45 km. A tsunami warning was announced within the Pacific area and was lifted after two hours. The Philippine archipelago is located in the Pacific Ring of Fire, where earthquakes and volcanic activity are common.

<span class="mw-page-title-main">1918 Celebes Sea earthquake</span> Earthquake in the Philippines

The 1918 Celebes Sea earthquake occurred on August 15 at 12:18 UTC near the Moro Gulf coast of Mindanao. It had a magnitude of 8.3 on the moment magnitude scale and a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale.

The Cotabato Trench is an oceanic trench in the Pacific Ocean, off the southwestern coast of Mindanao in the Philippines. Along this trench the oceanic crust of the Sunda Plate beneath the Celebes Sea is being subducted beneath the Philippines Mobile Belt. It forms part of a linked set of trenches along the western side of the Philippines formed over east-dipping subduction zones, including the Manila Trench and the Negros Trench. At its northern end the rate of convergence across this boundary is about 100 mm per year. It is a relatively young structure, forming during the late Miocene to Pliocene. This age is consistent with the estimated age of the sedimentary rocks in the accretionary wedge associated with the trench and the age of adakitic arc rocks on Mindanao thought to date the onset of subduction.

The 2019 Cotabato earthquakes were an earthquake swarm which struck the province of Cotabato on the island of Mindanao in the Philippines in October 2019. Three of these earthquakes were above 6.0 on the moment magnitude scale with a Mercalli intensity of VIII. More than 40 people have been reported dead or missing and nearly 800 were injured as a result of these events.

At 14:11 PST on December 15, 2019, the province of Davao del Sur on the island of Mindanao in the Philippines was struck by an earthquake measuring 6.8 Mw. It had a maximum perceived intensity of VII on the Modified Mercalli Intensity Scale. At least 13 people were killed and another 210 injured.

On 9 July 2019, at 8:36 PM (PST), an earthquake measuring Mw 5.6 jolted the province of North Cotabato, Davao del Sur, and other nearby provinces. The National Disaster Risk Reduction and Management Council reported one dead and three injured in Makilala after the earthquake, and a total of 164 families affected in Cotabato Province. Near the epicenter of the earthquake, the severity of strong ground motion was assigned VI (Strong) on the Modified Mercalli intensity scale. A total of 106 schools, 119 houses, and 14 other infrastructures were damaged by the earthquake.

On February 7, 2021, at 12:22 PM PST, an earthquake measuring Mw  6.0 struck Davao del Sur and Cotabato. The event registered a Modified Mercalli Intensity Scale (MMI) of VIII (Severe) with VII on the PHIVOLCS Earthquake Intensity Scale (PEIS).

On August 12, 2021, at 01:46:12 PST, a strong Mw  7.1 earthquake struck the island of Mindanao at a depth of 56.7 kilometers (35.2 mi). It perceived Intensity V on the PHIVOLCS Earthquake Intensity Scale. No damage or injuries were reported but a young man was killed by the earthquake.

The 1955 Lanao earthquake struck Lanao del Sur on April 1 at 02:17 local time. The earthquake measuring 7.4 on the moment magnitude scale and assigned a maximum intensity of VIII (Severe) on the Modified Mercalli intensity scale was one of the largest to hit Mindanao. It caused immense damage around Lake Lanao and the southern reaches of the Visayan islands. It killed at least 465 individuals and injured a further 898.

References

  1. "Philippines - Earthquake OCHA Situation Report No. 3". ReliefWeb . March 15, 2002.
  2. "Magnitude 7 and Greater Earthquakes in 2002". United States Geological Survey. December 1, 2003. Archived from the original on February 18, 2012. Retrieved May 31, 2010.
  3. "Magnitude 7.5 Mindanao, Philippines". United States Geological Survey. November 13, 2003. Archived from the original on February 13, 2010. Retrieved May 30, 2010.
  4. "Tectonics and Volcanoes of the Philippines". Volcano World. Oregon State University. 2010. Archived from the original on July 18, 2010. Retrieved May 31, 2010.
  5. "Historic World Earthquakes". United States Geological Survey. November 23, 2009. Archived from the original on July 28, 2010. Retrieved May 31, 2010.
  6. 1 2 "12 dead in Mindanao earthquake". Philippine Daily Inquirer . March 16, 2002. Archived from the original on April 17, 2002. Retrieved November 12, 2022.
  7. "Poster of the Mindanao, Philippines Earthquake of 05 March 2002 - Magnitude 7.5". United States Geological Survey. October 19, 2009. Archived from the original on February 13, 2010. Retrieved May 29, 2010.
  8. "Strong earthquake rocks southern Philippines, killing four people, injuring 15 and cutting power". Associated Press. March 6, 2002.
  9. "Members safe after earthquake". The Deseret News . March 16, 2002. Archived from the original on July 13, 2012. Retrieved May 31, 2010.
  10. "12 dead in Mindanao earthquake". Philippine Daily Inquirer . March 16, 2002. Archived from the original on April 7, 2002. Retrieved November 12, 2022.