| 1999 İzmit earthquake | |
| Timestamp: | 1999-08-17 00:01:38 |
| Anss-Url: | usp0009d4z |
| Isc-Event: | 1655218 |
| Local-Time: | 03:01 |
| Duration: | 37 seconds[1] |
| Magnitude: | 7.6 7.8 [2] |
| Depth: | 15km (09miles) |
| Location: | 40.748°N 29.864°W |
| Fault: | North Anatolian Fault |
| Type: | Strike-slip |
| Affected: | Turkey |
| Damages: | 3–8.5 billion USD |
| Intensity: | [3] |
| Pga: | 0.45 g |
| Tsunami: | 2.52m (08.27feet) |
| Casualties: | 17,127–18,373 dead 43,953–48,901 injured 5,840 missing |
The 1999 İzmit earthquake had a magnitude of 7.6 and struck Kocaeli Province, Turkey on 17 August. Between 17,127 and 18,373 people died as a result, and the damage was estimated at US $6.5 billion.[4] It was named for the quake's proximity to the northwestern city of İzmit. The earthquake occurred at 03:01 local time (00:01 UTC) at a shallow depth of 15 km. A maximum Mercalli intensity of X (Extreme) was observed. The earthquake lasted for 37 seconds, causing seismic damage, and is widely remembered as one of the deadliest natural disasters in modern Turkish history.
The 1999 earthquake was part of a seismic sequence along the North Anatolian Fault that started in 1939, causing large earthquakes that moved progressively from east to west over a period of 60 years.[5] The earthquake encouraged the establishment of a so-called earthquake tax aimed at providing assistance to those affected by the earthquake.[6]
The North Anatolian Fault Zone (NAFZ), where the earthquake occurred, is a right-lateral strike-slip fault zone. It extends from the Gulf of Saros to Karlıova. It formed around 13–11 million years ago in the eastern part of Anatolia and developed westwards. The fault eventually developed at the Marmara Sea around 200,000 years ago despite the shear-related movement in a rather broad zone which had already started in late Miocene.[7]
The fault zone is seismically active and has a diverse geomorphological structure. It produced a series of earthquakes as large as 8.0 on the moment magnitude scale. Since the 17th century, it has shown cyclical behavior, with century-long large earthquake cycles beginning in the east and continuing westward. Although the record is less clear for earlier times, active seismicity was likely to have occurred. The 20th century earthquake record has shown that the earthquakes concentrate the stress at the western tips of the ruptured areas, leading to westward migration of larger earthquakes. The İzmit and November 12, 1999 events increased stress on the Marmara segment of the fault. An earthquake of up to magnitude 7.6 event was expected between 2005 and 2055 with a probability of 50 percent on this segment.[7] Presently, the deformation of rocks by stress in the Marmara Sea region is asymmetric. This is conditioned by the regional geology and is believed to be representative of most of the NAFZ.[7]
The 17 August 1999 earthquake was the seventh in a sequence of westward-migrating seismic sequence along the NAFZ. This earthquake sequence began in 1939 and ruptured along a 1000-km part of the fault zone, with horizontal displacements of up to 7.5m (24.6feet).
The maximum observed ground motion was 0.45 g. The earthquake lasted 35–45 seconds according to various sources. The closest cities affected were İzmit, Gölcük, Yalova, and Adapazarı, all of which are located near the eastern end of the Marmara Sea, within the Gulf of İzmit. The earthquake also caused serious damage in Istanbul, especially in the district of Avcılar which is located in the western part of the city, around 70km (40miles) away from the epicenter. Despite the distance, it killed about 1,000 people in the district. The earthquake caused a surface rupture comprising four segments; the Hersek/Karamürsel–Gölcük, İzmit–Lake Sapanca, Lake Sapanca–Akyazı, Akyazı–Gölyaka and Gölyaka–Düzce segments. These segments altogether measured over 125 km. All the segments are separated by pull-apart stepovers of NaNkm (-2,147,483,648miles) in width. The maximum offset throughout the rupture was measured on the Sapanca–Akyazı segment where the surface break displaced a road and a tree line by 5.2m (17.1feet). It also showed pure strike-slip, and the fault plane is almost vertical in most of the places where a surface break was observed. Most of the major aftershocks (M>4) were located near Düzce, south of Adapazarı, in Sapanca, in İzmit, and the Çınarcık area. At Değirmendere, a small coastal town west of Gölcük, the rupture cut the edge of a fan delta where the center of the town was located, which caused a slump measuring 300m (1,000feet) long and 100m (300feet) wide. As a result, part of the town center slid under the water, including a hotel and several shops and restaurants. At another fan delta east of Gölcük, which is within the step-over area of the ruptures, the fault produced a 2 m-high normal fault scarp.[8]
Data was used from seven broadband stations as well as some other short-period stations across the area to calculate the regional moment tensor of the mainshocks and larger aftershocks. As a result, most of the earthquakes were found to be split in segments, with the moment tensor's focal mechanism reading either a strike-slip on the fault which is west-east striking, or normal faulting which is between rupture segments. This also proves that the main characteristic of the quake is dextral strike-slip.[9]
From the timing of P-wave and S-wave arrivals at seismometers, there is strong evidence that the rupture propagated eastwards from the epicenter at speeds in excess of the S-wave velocity, making this a supershear earthquake.[10]
See also: Earthquake engineering.
| Deaths | Injuries | |
|---|---|---|
| Bolu | 264 | 1,163 |
| Bursa | 263 | 333 |
| Eskişehir | 86 | 83 |
| Istanbul | 978 | 3,547 |
| Kocaeli | 8,644 | 9,211 |
| Sakarya | 2,627 | 5,084 |
| Tekirdağ | 0 | 35 |
| Yalova | 2,501 | 4,472 |
| Zonguldak | 3 | 26 |
Over 800 people were killed in İzmit.[14] In Gölcük, at least 4,556 people died, 5,064 were injured, thousands were left missing and at least 500 buildings collapsed, trapping about 20,000 families.[15] About 200 sailors went missing after a naval base collapsed.[14] There was also destruction in Yalova; 2,501 people died, 4,472 were injured and 10,134 buildings collapsed. The cause of most damage in Yalova was suspected to be liquefaction-induced. Since the area mostly comprised Quaternary alluvial soil, it was prone to liquefaction. The approximately 200 drilling sites and boreholes, and many streams and rivers, factored in the severe liquefaction.[16]
In Istanbul, at least 978 people were killed and 3,547 others sustained injuries.[15] Severe damage in the city was concentrated in Avcılar district. Avcılar was built on relatively weak ground, mainly composed of poorly consolidated Cenozoic sedimentary rocks, which made the district vulnerable to earthquakes.[17] In Eskişehir, there were 86 deaths and 70 buildings collapsed. At least 263 people died and 333 others were injured in Bursa. Three deaths and 26 injuries were reported in Zonguldak. At least 2,627 people were also killed and 5,084 others were hurt in Sakarya Province.
Private contractors faced backlash for using cheap materials in their construction of residential buildings. Many of these contractors were prosecuted but few were found guilty. Government officials also faced backlash for not properly enforcing earthquake resistant building codes.[18] Direct cost of damage is estimated at US $6.5 billion, but secondary costs exceeded US $20 billion.[19] In 2010, the research branch of the Grand National Assembly of Turkey stated there were 18,373 deaths as a result. In the same report, it stated there were 48,901 injured, 505 permanently injured, 96,796 homes heavily damaged or destroyed, 15,939 businesses heavily damaged or destroyed, 107,315 homes moderately damaged, 16,316 businesses moderately damaged, 113,382 homes slightly damaged, 14,657 businesses slightly damaged, 40,786 prefabricated homes distributed and 147,120 people rehoused into these homes.[20]
There was extensive damage to several bridges and other structures on the Trans-European Motorway, including 20 viaducts, 5 tunnels, and several overpasses. Damage ranged from spalling concrete to total deck collapse.[21]
The earthquake triggered a fire at the Tüpraş petroleum refinery. The fire began at a state-owned tank farm and was initiated by naphtha that had spilled from a holding tank. Breakage in water pipelines and earthquake damage made firefighting attempts ineffective. Aircraft were called in to douse the flames with foam, but the fire spread for several days. An evacuation was warranted for an area within 5km (03miles) of the refinery. The fire was declared under control five days later after claiming at least 17 tanks and an unknown quantity of complex piping.[22] People within NaNmiles of the refinery had to evacuate despite some areas still being in the process of search and rescue.[23]
At least 155 deaths were associated with the tsunami.[24] Many field studies were made about the tsunami in the Gulf of İzmit. Along the northern coast of the gulf, in the basin between Hereke and Tüpraş Petroleum Refinery, the tsunami was recorded as a leading depression wave. The run-up wave heights in this area ranged from . The first series of waves arrived at the north coast a few minutes after the earthquake, and had a period of around a minute. The hardest hit areas were Şirinyalı, Kirazlıyalı, Yarımca, Körfez, and the refinery. The tsunami carried mussels into buildings, and damaged doors and windows. Körfez experienced flooding up to in some areas. Later, watermarks were seen on the walls of buildings, including the police station in Hereke, and at a restaurant near Körfez. Locals reported the first waves arrived at Kirazlıyalı from a southeastern direction, and at Körfez from a southern direction. Along the southern coast of the gulf between Değirmendere and Güzelyalı, run-up measured . The tsunami was recorded as a leading depression wave to the west of Kavaklı up to Güzelyalı. There, the wave was noticed by locals immediately after the earthquake. There was severe coastal subsidence and slumping of a park near Değirmendere. The subsided area was along the shore and perpendicular to shore. The same area included two piers, a hotel, a restaurant, a cafe and several trees. Locals at the coast near Değirmendere observed the sea receding by about in less than two minutes. When the sea came back, it swept inland up to, as shown by the mussels and dead fish left in the flooded areas.[25] The tsunami also caused damage to the naval base nearby.[26]
A 5.2 aftershock hit near İzmit on August 31, causing one additional fatality and 166 injuries, with tremors being felt in Istanbul.[27] Another 5.9 aftershock hit on September 13, causing seven deaths and 422 injuries.[28] Another aftershock measuring 5.2 occurred on September 29, killing one person in Istanbul.[29] A 5.0 aftershock on November 7 killed one person in Sakarya Province,[30] while another 5.7 event on November 11 in the same province caused two deaths and 171 injuries.[31] On 23 August 2000, a 5.3 earthquake caused 22 injuries in Sakarya.[32] Another 5.0 event hit on 26 August 2001, causing two injuries in Bolu.[33]
| Bolu | 3,226 | 4,782 | 3,233 |
| Bursa | 32 | 109 | 431 |
| Eskişehir | 70 | 32 | 204 |
| Istanbul | 3,614 | 12,370 | 10,630 |
| Kocaeli | 23,254 | 21,316 | 21,481 |
| Sakarya | 20,104 | 11,381 | 17,953 |
| Yalova | 10,134 | 8,870 | 14,470 |
| Total: | 60,434 | 58,860 | 68,391 |
See also: Greek–Turkish earthquake diplomacy. A massive international response was mounted to assist in digging for survivors and to assist the wounded and homeless. Rescue teams were dispatched within 24–48 hours of the disaster, and the assistance to the survivors was channeled through NGOs, Turkish Red Crescent and local search and rescue organizations.The following table shows the breakdown of rescue teams by country in the affected locations:
| Location | Foreign search and rescue teams | |
|---|---|---|
| Hungary, Israel, France, South Korea, Belgium, Russia | ||
| Germany, Hungary, Israel, Poland,[34] United Kingdom, France, Japan, Austria, Romania, South Korea | ||
| Greece, Germany | ||
| Russia, Hungary, France, Germany, Austria, Switzerland, United States, Iceland, South Korea | ||
| Bulgaria, Egypt, Germany, Spain | ||
| Poland, United Kingdom | ||
| Italy | ||
| Azerbaijan |
Search and Rescue Effort as of 19 August 1999. Source: USAID[35]
In total, teams from 12 countries assisted in the rescue effort. Greece was the first nation to pledge aid and support. Within hours of the earthquake, the Greek Ministry of Foreign Affairs contacted their counterparts in Turkey, and the minister sent his personal envoys. The Greek Ministry of Public Orders sent a rescue team of 24 people and two trained rescue dogs, as well as fire-extinguishing planes to help put out the fire in the Tüpraş Oil refinery.[36]
Oil Spill Response Limited was activated by BP and deployed from the United Kingdom to the Tüpraş Refinery. Responders successfully contained the previously uncontrolled discharge of oil from the site into the sea.[37]
The UK announced an immediate grant of £50,000 to help the Turkish Red Crescent, while the International Red Cross and Red Crescent pledged £4.5 million to help victims. Blankets, medical supplies and food were flown from Stansted airport. Engineers from Thames Water went to help restore water supplies.[38]
US President Bill Clinton later visited Istanbul and İzmit to examine the level of destruction and meet with the survivors.[39]
There has been an increased seismic activity in the Eastern Sea of Marmara since 2002 and a quiescence of earthquakes on the Princes' Islands Segment of the North Anatolian Fault off the southern coast of Istanbul. This suggests that the 150km (90miles) long submarine seismic gap below the Sea of Marmara could result in another large earthquake. These possibilities are quite important, with respect to the segmentation of major fault ruptures along the North Anatolian Fault Zone in north-western Turkey. With the possible activation of segments towards the metropolitan areas of Istanbul, the Princes' Islands gap should be considered to have an impact on the large seismic hazard potential for Istanbul.[40]
Despite a long-term earthquake catalogue existing for the North Anatolian Fault Zone and for the Istanbul area in particular, the basic understanding of the seismicity there is still lacking. The observation of a seismic gap in the vicinity of the Istanbul metropolitan area was made possible through deploying a dense network of seismic stations and small arrays near the fault trace, south of the Princes' Islands. This improved monitoring along the Princes' Islands segment, which is west of the İzmit 1999 rupture and southeast of Istanbul's city center. It has highlighted the location of likely rupture points for future earthquake. It also limits the maximum size of future events along the whole Marmara seismic gap in case of cascade behavior. Knowing this, a regional earthquake early warning system for Istanbul and surroundings could be beneficial. The aseismic part of the Princes' Islands segment represents a likely high-slip area for a future large earthquake. Fault characterization is likewise very relevant to determine the directivity of earthquake waves approaching Istanbul. Modelling of potential impacts to Istanbul from different scenarios have shown to improve the estimation of hazards that the seismic gaps pose. Improved and denser seismic monitoring is expected from on-going efforts to install an underground (borehole-based) seismograph network in the Sea of Marmara.[40]
Istanbul, being the most populated city in Turkey, lies right near the segments of the North Anatolian Fault Zone, making it at very high risk to an earthquake-related disaster which could cause thousands of casualties and severe damage. Following the 1999 earthquake, there was an urgent need for the government to mitigate these risks. With the help of organizations like the World Bank, hundreds of buildings have been retrofitted and reconstructed, and thousands of citizens have been trained in disaster preparedness.[41]