2/22/2005 Kerman,Iran Quake

Updated 3/20/2005

This 6.4M quake hit Central Iran Tuesday, February 22, 2005 at 02:25AM (GMT) or 5:55 AM local time.

The epicenter was:
55 km (35 miles) NNW of Kerman, Iran
185 km (115 miles) NE of Sirjan, Iran
270 km (165 miles) ESE of Yazd, Iran
745 km (465 miles) SE of TEHRAN, Iran

According to the USGS at least 602 people were killed and 991 injured. The quake hit a rural area with no large cities, lessening the impact. Five villages were reported very heavily damaged with perhaps 50 more having substantial damage. Rescue efforts were somewhat hampered by heavy rains and freezing temperatures but there were also reports that rescue units were already on alert for fear that the rain would cause damage. Roads to some of the area have been blocked by landslides, making it difficult for needed heavy equipment to reach the scene. Numerous aftershocks kept many out of doors for fear of further damage to buildings. Most of the casualties were from collapsed buildings. Gas and electricity supplies have been disrupted and the government has asked people to limit use of mobile phones to allow better communications among emergency personnel. The Iranian government declared a national day of mourning for the dead.

The earthquake was caused by stresses generated by the northward movement of the Arbaian Plate into the Eurasian Plate at about 1 inch per year. This is sufficient to cause frequent quakes throughout Iran. The February 22 earthquake is 125 km northwest of the destructive earthquakes of June 11, 1981 (magnitude 6.6, approximately 3,000 deaths) and July 28, 1981 (magnitude 7.3, approximately 1,500 deaths) and about 250 km northwest of the devastating Bam earthquake of December 26, 2003 (magnitude 6.6, over 30,000 deaths).

(See the Plate Tectonics page for more information on these processes.) The US Geological Survey (USGS) is an invaluable resource in understanding and tracking earthquakes.

See also the following news stories:

12/26/2004 Sumatra Earthquake and Tsunami

Updated 3/20/2005

At 9.0 Magnitude, this was the largest earthquake in the world since the 1964 Alaskan quake. It struck on December 26 at 6:58 AM local time (00:58 GMT). The epicenter was 255 km (160 miles) SSE of Banda Aceh, Sumatra, Indonesia 315 km (195 miles) W of Medan, Sumatra, Indonesia 1260 km (790 miles) SSW of BANGKOK, Thailand 1590 km (990 miles) NW of JAKARTA, Java, Indonesia.

Casualties have been very high, with over 283,000 dead, especially from the tsunami generated by the earthquake. The tsunami, reported as 15 - 20 feet high, fanned out over the Indian Ocean causing severe and sudden flooding in Sri Lanka, India, Thailand, Indonesia and other areas. Over a million people have been reported as homeless in Sri Lanka alone, at least 5 million were left without the basic necessities of life. Over 100,000 are reported dead in Indonesia. This tsunami was one of the largest ever in terms of casualties because it hit in heavily populated low lying coastal areas that were not well prepared. The lack of a warning system meant that most people were caught by surprise. It has been a long time since there has been a tsunami in this region. Unlike the Pacific Ocean, which has a well developed warning system, the Indian Ocean has no way to warn of an impending tsunami. Scientists knew as soon as the quake happened that it posed a danger of tsunami, but there was no way to get the word to the coastal areas in time. There were only a few minutes to a couple of hours between the quake and the tsunami. Communications were not up to the task.

The scope of this disaster is well beyond what is normal for even a strong earthquake. The tsunami hit 14 different countries, with severe damage in four (Indonesia, Thailand, India and Sri Lanka), spread out over thousands of miles. India reported that they had sufficient resources to provide needed aid in their own country and send some to Sri Lanka as well. Sri Lanka has a long coastline that suffered badly needs assistance, but with the interior undamaged can mobilize fairly well to receive and distribute aid. Indonesia is much worse off. They have to cope with quake damage and tsunami damage, as well as a less well developed infrastructure that make communications and travel difficult. There are shortages of petrol and machinery, such as forklifts that would make the relief effort easier.

People reported seeing the ocean pull back, exposing the sea floor and then return as a swift rise in the sea level, like an extremely high tide, inundating villages near the coast. The wave then pulled back, sucking houses, trees, people...everything in its path out to sea. These waves have a long period, so there are many minutes until the next wave hits. The process is similar to the ripples formed when a stone is thrown into water. Each successive wave carries more debris, causing more damage. The zone of damage extends up to 2 miles inland along the entire coast. Most buildings in this zone are severly damaged or destroyed, with a thick layer of mud covering everything. Food, water, electricity, and housing are all non existant or in short supply.

The area of the quake itself in Aceh province has seen severe damage from the earthquake and from the tsunami in coastal areas. Reports suggest that there may be over 100,000 dead in Sumatra alone. There have been reports of many buildings destroyed. Large amounts of international aid were desparately needed and relief supplies were sent from throughout the world. Some of the most severely affected areas did not receive any aid for a week after the disaster due to the huge need and difficulty of reaching remote areas. Observers repeatedly reported that the scope of the disaster was unbelievable, with almost complete destruction along hundreds of miles of coastal areas.

There have been many powerful aftershocks along the whole 745 mile fault that was affected, notably in the Andaman and Nicobar islands. Three months after the initial quake, aftershocks over magnitude 5 occur every few days along the fault line.

Both Aceh province and parts of Sri Lanka have been embroiled in civil wars that have slowed the flow of information and may hinder the distribution of government aid in contested or rebel held areas. Aceh has been under military control with very little access for foreigners. An independece movement has been fighting the Indonesian government for several years. Portions of Sri Lanka that were hard hit are under the control of Tamil rebels, in a war that has lasted for many years.

The scope of the disaster made it difficult to even bury the dead. Most have been buried in mass graves, although efforts were made to photograph the dead with photos and in places take DNA samples. It is hoped that these will help relatives identify victims. The World Health Organization has warned of danger of disease outbreaks that could kill thousands more. They say that dead bodies do not pose a threat, although they are unpleasant, but contaminated water supplies do. There have already been reports of outbreaks of diarhea, but the main danger is in the next few weeks. Water supplies within the affected areas have all been contaminated. Sanitation was already precarious in some of these areas. Now they have nothing. Clean water is high on the priority list for aid. Hundreds of millions of dollars of aid have been pledged from many countries around the world. Naval vessels are on the way to help but took several days to arrive. Because of the huge area involved and the limited communications available, it took days to even get reports from many areas, especially in Indonesia.

This explanation of the quake from the BBC:
How the Quake unfolded (BBC 12/27/04)

According to the USGS "The devastating megathrust earthquake of December 26th, 2004 occurred on the interface of the India and Burma plates and was caused by the release of stresses that develop as the India plate subducts beneath the overriding Burma plate. The India plate begins its descent into the mantle at the Sunda trench which lies to the west of the earthquake's epicenter. The trench is the surface expression of the plate interface between the Australia and India plates, situated to the southwest of the trench, and the Burma and Sunda plates, situated to the northeast." The interactions of these plates, along with the Indian Plate, the Pacific Plate and the Phillipines Plate, make this one of the most seismiscally and volcanically active regions of the world. Subduction earthquakes are the largest known. The 1964 Alaskan quake and the 9.5 Magnitude Chilean quake of 1960 were both subduction quakes.

In this case the subducting plate is being forced down into the earth under an overriding plate. Heat rising as the plate hits the earth's mantle and melts rises to form a volcanic island chain - Indonesia. Since the descending plate is fairly rigid and flat, when the magma rises, it creates an arc of volcanic islands on the curved surface of the Earth, which shows the direction of the plate movement nicely. The Aleutian Islands are another nice example of this process.

(See the Plate Tectonics page for more information on these processes.)

A tsumani, or tidal wave, occurs when an earthquake displaces a portion of the seafloor. In this case, according to USA Today, a section of seafloor 745 miles long was raised 100 feet by the quake. This sudden movement displaced a massive amount of water, which fanned out from the epicenter. This wave moved at 500 miles an hour across the Bay of Bengal, the Indian Ocean and the Pacific Ocean. If you look at a map of the region you will see that the areas hardest hit were across the Bay of Bengal from the epicenter at the Western edge of Indonesia.

See also the following news stories:

12/26/2003 Iranian Earthquake

Updated 1/7/2004

The 6.7 Magnitude earthquake struck at 01:58 GMT 12/26/03. This was 05:28 am local time. The epicenter was in Bam, a city of 80,000, with 200,000 in the surrounding area, in southern Iran, 620 miles southeast of Teheran. The BBC reported within hours of the quake, "A huge relief operation involving ordinary Iranians, the army, Islamic volunteer groups and local rescue teams is under way." The death toll has been estimated at over 30,000 people with over 30,000 injured. Two hospitals collapsed in the quake and remaining ones were strained to help the thousands injured. Electricity and telephone service were knocked out. Over 70% of the houses in Bam are reported to be destroyed.

The quake had been preceeded the night before by a foreshock strong enough to cause some people to sleep out of doors. Undoubtably some lives were saved as people were not inside when houses collapsed. People have continued to sleep outside due to the many aftershocks, which are typical after a major quake.

Relief efforts appear to have been well coordinated at the local level. Teams of people were working to dig out survivors soon after the quake. The dead were quickly buried in mass graves. Health and religious authorities both insisted on quick but respectful burials. Although the huge numbers of dead strained resources, this was accomplished. Trenches were dug with backhoes, groups of about 50 bodies were laid in them and covered with dirt by bulldozers. Then a new trench was started and the process repeated over and over again.

International aid arrived quickly to help survivors and help with reconstrution. Visa requirements were waived for aid workers and for the first time since the revolution 25 years ago, Americans were welcomed into Iran. There is some hope that this could be an opportunity to improve relations between the two countries.

Also destroyed was the Citadel,Arg-e-Bam, mostly dating from the Safavid period in the 16th and 17th C. This was a major historic structure, parts of which date back 2,000 years. As the largest mud brick structure in the world, and a major historic site, it was on the Unesco's list of World Heritage Sites. Bam is on major trade routes to India and the far east, as well as being an oasis in the desert has given it a special importance. The Citadel was a major tourist attraction, the loss of which will be devastating to the nation's cultural heritage and the local economy. Authorities say that it will be reconstructed, but that, of course, is far from the same as having the original.

International aid is on the way, with teams from Russia, Turkey and many other nations. Turkey has been especially responsive with aid teams, following devastating earthquakes in 1999, which raised their awareness of the need for quick aid following large quakes.

Despite frequent large quakes, Iran does not have strong building codes and many houses are built out of mud bricks and unreinforced masonry, which do not stand up well to earthquakes. Mud brick crumbles into a heavy powder without air pockets. Heavy cement roofs collapsed into houses crushing the occupants. Consequently, casualties and damage is much higher than in a similar quake elsewhere in the world. For example, the Northridge quake in Los Angeles in 1994 was a little stronger than this one but only killed about 100 people. In Kobe Japan in 1995 a similar quake killed about 5,000. There too, heavy tile roofs collapsed into many houses. Other factors contribute to the severity of a quake, but earthquake resistant buildings can make a huge different in the number of injuries.

Here is the USGS preliminary report on the causes of the quake:

This earthquake occurred as the result of stresses generated by the motion of the Arabian plate northward against the Eurasian plate at a rate of approximately 3 cm/yr (about one inch per year). Deformation of the Earth's crust in response to the plate motion takes place in a broad zone that spans the entire width of Iran and extends into Turkmenistan. Earthquakes occur as the result of both reverse faulting and strike-slip faulting within the zone of deformation. Preliminary analysis of the pattern of seismic-wave radiation from the December 26 earthquake is consistent with the earthquake having been caused by right-lateral strike-slip motion on a north-south oriented fault. The earthquake occurred in a region within which major north-south, right-lateral, strike-slip faults had been previously mapped, and the epicenter lies near the previously mapped, north-south oriented, Bam fault. However, field investigations will be necessary to determine if the earthquake occurred on the Bam fault or on another, possibly not yet mapped, fault. The December 26 earthquake is 100 km south of the destructive earthquakes of June 11, 1981 (magnitude 6.6, approximately 3,000 deaths) and July 28, 1981 (magnitude 7.3, approximately 1,500 deaths). These earthquakes were caused by a combination of reverse-motion and strike-slip motion on the north-south oriented Gowk fault.

(See the Plate Tectonics page for more information on these processes.)

See also the following news stories:

5/21/2003 Algeria Earthquake

Updated 5/24/2003

The 6.7 Magniture earthquake struck at 18:44 GMT 5/21/03. This was 7:44 pm local time. The epicenter was in Bourmedes, 45 miles east of Algiers in Northern Algeria. Scores of buildings collapsed in the first seconds of the quake. Over 1,875 have died, over 1.000 in Bourmedes and over 7,000 injured. Thousands more camp out in the streets because their homes have been destroyed or out of fear of aftershocks. Accoridng to the BBC, "In Reghaia, 35km (22 miles) east of Algiers, authorities requisitioned the municipal stadium, setting up tents for families whose houses were destroyed in the earthquake. " There have indeed been many strong aftershocks. Rescuers have been desperately digging in the rubble with bulldozers and their bare hands desperately trying to find people who are still alive. After the first two days there is little hope of finding more survivors. Hospitals are totally overwhelmed with thousands of people coming in with serious injuries. Communications are difficult with phone lines down. Many roads have been damaged, huge traffic jams make access to the area difficult. Remote villages are especially cut off with roads cracked and blocked with debris. Large crowds of relatives are pouring into the area, adding to the congestion. Medical supplies are in short supply.

Algeria has requested international aid to cope with the massive damage. France has sent aid, including rescue equipment and rescue dogs. The dogs have been trained to find people under debris. Other countries are also contributing. French President, Jacques Chirac stressed historic ties between France, the former colonial power, and Algeria, in sending aid. UNICEF, the Red Cross and Red Crescent Societies and others are contributing to the effort.

Two days after the quake, crowds turned their grief and anger towards the Algerian President when he toured the disaster area. Boos and stone throwing were reported. Local Newspapers also attack the lack of preparations and response to a quake in this very seismically active region. They accuse the government of an inadequate response and of allowing substandard construction of the buildings that collapsed. The government has been accused of slow response and poor co-ordination of the rescue efforts. Foreign aid workers are finding that government security concerns are also slowing them down. They are experiencing tight checks at the border. Conflicts between government security forces and Islamic militants complicate the issue. Road crews are working with armed escorts and the government is reluctant to send rescuers into areas where they might be caught up in the conflict.

This quake was casued by the collision between the African Tectonic Plate, which is moving northward into Europe. The Northern Algerian area has been hit repeatedly by severe quakes. The USGS describes this process as follows: "The earthquake occurred in the boundary region between the Eurasian plate and the African plate. Along this section of the plate boundary, the African plate is moving northwestward against the Eurasian plate with a velocity of about 6 mm per year. The relative plate motions create a compressional tectonic environment, in which earthquakes occur by thrust-faulting and strike-slip faulting. Analysis of seismic waves generated by this earthquake shows that it occurred as the result of thrust-faulting. Algeria has experienced many destructive earthquakes. On October 10, 1980, the city of El Asnam (formerly Orleansville and today Ech-Cheliff) was severely damaged by a magnitude 7.1 earthquake that killed at least 5000 people. The site of El Asnam is situated approximately 220 km to the west of the recent earthquake. The same city, as Orleansville, had been heavily damaged on September 9, 1954, by a magnitude 6.7 earthquake that killed over 1000 people. On October 29, 1989, a magnitude 5.9 earthquake struck about 110 km to the west of the recent earthquake and killed at least 30 people."

(See the Plate Tectonics page for more information on these processes.)

See also the following news stories:

2/24/2003 China Earthquake

Updated 2/27/2003

The earthquake was given a magnitude of 6.4 by the US Geological Survey. It struck at 02:03 GMT Monday morning. This was 10:03 local time but because the area is in the extreme west of China's one time zone, it was shortly after dawn and many people were at breakfast. Others had just started school or work. The epicenter was in Xinjiang province 65 miles from the city of Kashi. This is in the extreme west of China, 2070 miles west of Beijing. It is generally poor, sparsely populated region, inhabited by Uighurs, a Muslim people, related to those in Kyrgyzstan and other Central Asian countries nearby.

The death toll was confirmed at 266, following strong aftershocks on 2/25/03 that killed 5 more people, including some rescue workers. Estimates of injuries range from 1,000 to 4,000. Over 9,000 buildings were destroyed. Most casualties were caused when people were trapped in their collapsing houses. CNN reported: "Almost all the dead were in Bachu County, where flimsy building construction seemed to have contributed to the death toll, officials said. The neighboring county of Jiashi was closer to the epicenter but suffered little damage; its homes have been reinforced following severe quakes in recent years."

The BBC reported: "The quake had a severe effect on the local economy, which is heavily dependent on farming. Some 11,000 cattle were killed and at just one farm in Qiongkuerqiake, 190 sheep were crushed. Local residents cannot eat them because they have not been butchered according to Muslim tradition. "

The army immediately sent in rescue crews to help dig survivors out of the rubble. Dogs are also being used to locate survivors. The Chinese government is providing aid but has not issued an international appeal.

This quake was casued by the collision between the Indian Sub-continent, which is plowing northward into Asia. This collision raised the Himalayan Range and causes earthquakes throughout the whole Central Asian region. The USGS describes this process as follows:

"This earthquake occurred near the boundary between the Tarim Basin and the Tian Shan mountain range in the north-west Tarim Basin. In a broad sense, earthquakes in this region result from stresses induced by the collision of the Indian and Eurasian continental plates, even though the boundary between these plates lies about 1000 km to the south.

The Indian Plate continuously moves northward at a rate of 4.5 cm per year relative to the Eurasian Plate generating massive mountain ranges including the Himalaya and causing the uplift of the Tibetan Plateau. These stresses are transmitted to the north, through the rigid and undeforming Tarim Basin, where they generate the Tian Shan mountains and numerous earthquakes like this recent event. Several nearby mapped faults have orientations similar to the thrust fault that the earthquake occurred on, although seismologists have not yet associated the quake with a specific fault.

The region surrounding this earthquake has produced several deadly earthquakes in the past decade. The most destructive include a magnitude 6.3 event on March 19, 1996, a magnitude 5.9 on January 21, and a magnitude 6.2 on April 11, 1997. Each quake killed between 10 and 24 people, and destroyed thousands of buildings. The most recent significant earthquake occurred on August 27, 1998 killing 2 and destroying 3,600 homes. " (See the Plate Tectonics page for more information on these processes.)

USGS Bulletin for the 2/24/03 China quake

See also the following news stories:

6/22/2002 Iran Earthquake

Updated 6/30/2002

On Saturday June 22, 2002 at 7:28 AM local time (02:58 GMT) a magniture 6.5 earthquake hit northwest Iran. It was centered around the town of Bou'in-Zahra, in northern Qazvin province about 240 miles west of Teheran. The death toll was originally thought to be over 500 but within a few days was revised downwards to 245. There were an estimated 1,500 injuries and 5,000 homes were destroyed leaving 25,000 people homeless. Nearly 100 villages were badly damaged or destoyed, according to the Red Crescent. Most of the dead were buried when their unreinforced homes collapsed. Emergency services were strained, with local people complaining that the government was too slow to get help to the region and that the death toll was actually higher than the official reports. Efforts to prevent the spread of disease include spraying disinfectant.

International aid has been offered by many countries, including the US, in spite of the strained relations between the two countries. Iran has declared that it will accept some US humanitarian aid.

There have been many strong aftershocks, up to 5.1 Magnitude.

This quake was casued by the movement of the Arabian Plate as it moves to the northwest relative to the Eurasian Plate. The quake had a shallow focus as the earth's crust adjusted to the strain caused by this collision. Frequent shallow focus quakes are the rule in this area. The USGS describes this process as follows: " This recent Iranian earthquake occurred in the Zagros fold-and-thrust belt. This highly seismic region forms the boundary between the Arabian and Eurasian plates. The Arabian Plate is a small plate split from the African Plate by rifting along the Red Sea. As it collides with the massive Eurasian Plate it causes uplift of the Zagros mountains and numerous damaging earthquakes. " (See the Plate Tectonics page for more information on these processes.)

See also the following news stories:

3/25/2002 Afghan Earthquake

Updated 3/28/2002

On the morning of March 25, 2002 at 6:18 GMT GMT a 6.1 magnitude earthquake was felt in Northern Afghanistan. Initial reports set the death toll at 1,800 but that has been revised downwards to about 1,000. The shallow focus of the quake led to more severe shaking at the surface and thus more damage than a deeper quake of the same magnitude. Buildings are not built to resist quakes, using stone and masonry, which are easily damaged by the frequent earthquakes. The area hit has suffered from drought, famine and war in the last few years. Whole villages are reported to have been leveled with thousands homeless. The initial quake has been followed by a series of severe aftershocks and related quakes that compounded the damage. The same general area has been hit by major earthquakes on a regular basis.

Aid was immediately rushed to the area. Roads to the affected areas are difficult under the best of circumstances and made worse by earthquake caused landslides. Aid has gotten through by helicopter, with the international peacekeeping force in Kabul helping out. Many aid workers are already in the country helping victims of famine and war. Relief efforts may be hampered by landmines and the fear of Al Quaeda attacks. A statement apparently from Al Quaeda blames the quake on God's Punishment for the war against the Taliban. This quake was casued by the movement of the Indian Plate as it moves northward into the Eurasian Plate. The quake had a shallow focus as the earth's crust adjusted to the strain caused by this collision. (See the Plate Tectonics page for more information on these processes.)

See also the following news stories: