1999 İzmit earthquake

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1999 İzmit earthquake
Izmit eart6.jpg
1999 İzmit earthquake is located in Marmara
1999 İzmit earthquake
1999 İzmit earthquake is located in Turkey
1999 İzmit earthquake
UTC time1999-08-17 00:01:38
ISC event1655218
USGS-ANSSComCat
Local date17 August 1999 (1999-08-17)
Local time03:01
Duration37 seconds[1]
Magnitude7.6 Mw[2][3]
Depth15.0 km (9.3 mi)[2]
Epicenter40°44′53″N 29°51′50″E / 40.748°N 29.864°E / 40.748; 29.864Coordinates: 40°44′53″N 29°51′50″E / 40.748°N 29.864°E / 40.748; 29.864
FaultNorth Anatolian Fault
TypeStrike-slip[1]
Areas affectedTurkey
Total damage3–8.5 billion USD[3]
Max. intensityX (Extreme)[4]
Peak acceleration0.45 g[5]
Tsunami2.52 m (8.3 ft)[3]
Casualties17,127–18,373 dead[6][7]
43,953-48,901 injured[6][7]
5,840 missing[7]

On the 17th of August, 1999 at 3:01 AM local time, a catastrophic magnitude 7.6 earthquake struck the Kocaeli Province of Turkey, causing monumental damage and 17,127–18,373 casualties.[7] Named for the quakes proximity to the northeastern city of Izmit, the earthquake is also commonly referred to as the August 17 Earthquake or the1999 Gölcük Earthquake.[8] The earthquake occurred on 00:01 UTC at a shallow depth of 15 km. A maximum Mercalli intensity of X (Extreme) was observed, marking this event as one of the most destructive earthquakes in the history of the region. The earthquake lasted for 37 seconds, causing seismic damage and becoming widely remembered as one of the deadliest natural disasters in modern Turkish history.

The 1999 earthquake was part of a 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.[9]

Tectonic setting

The North Anatolian Fault Zone (NAFZ), which the quake occurred on is a 1200-km-long dextral (right-lateral) strike-slip fault zone, expanding from the Gulf of Saros to Karlıova that formed around 13 to 11 Ma ago in the eastern part of Anatolia and moved towards the west. The fault later reached the Marmara Sea at around 200 ka ago, despite the shear-related movement in a rather broad zone which had already started in late Miocene.[10]

The fault zone has a diverse geomorphological structure, is seismically active and currently stands as one of the world's most major and active strike-slip fault, having an entire group of ruptures being produced as large as 8.0 in 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, lively seismicity could still be seen in that timespan. The 20th century earthquake record has been interpreted as where every earthquake concentrates the stress at the western tips of the ruptured areas leading to westward migration of larger earthquakes. The August 17 and November 12, 1999 events have loaded the Marmara segment of the fault, noted since the 1999 earthquakes and another major, magnitude 7.6 or larger event is expected in the next half-century with a probability of 50% on this segment. Currently, the deformation of the rocks by stress in the Marmara Sea region is asymmetric. This is conditioned by the geology of the region and it is believed that this is the case for most of the North Anatolian Fault Zone.[10]

Earthquake

An interferogram image of the rupture caused by the earthquake

The 17 August 1999 earthquake was the 7th in a sequence of westward-migrating quake sequence on the North Anatolian Fault. This earthquake sequence began in 1939 and ruptured along a 1000-km part of the fault zone, with horizontal displacements of up to 7.5 m.[5]

The waveform showing the peak ground acceleration recorded by a station in Ambarlı, Avcılar district, Istanbul

The maximum observed ground motion was 0.45g. The earthquake lasted 35–45 seconds according to various sources. The closest cities damaged or affected by the earthquake were Izmit, Gölcük, Yalova, and Adapazarı, all located near the eastern end of the Marmara Sea, within the Gulf of Izmit. 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 70 km away from the epicenter. Despite the distance, it killed about 1,000 people in the district. The preliminary magnitude of the earthquake was 7.4 by the U.S. Geological Survey (USGS) and by the Kandilli Observatory, which operate in this country. The earthquake caused a surface rupture which consists of 4 segments; Hersek/Karamürsel–Gölcük, Izmit–Lake Sapanca, Lake Sapanca–Akyazı, Akyazı–Gölyaka and Gölyaka–Düzce segments which in total, had length of more than 125 km. All the segments are separated by pull-apart stepovers of 1 to 4 km 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 5.2 m. 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 Izmit, and the Çınarcık area. At Değirmendere, which is 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 300 m long and 100 m wide, as a result a 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.[5]

Data was used from 7 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 and 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 which also proves that the main characteristic of the quake is dextral strike-slip.[11]

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.[12]

Impacts

See also: Earthquake engineering
USGS ShakeMap showing the intensity of the event

There was destruction caused in Yalova as a result of the earthquake, as well as hundreds killed and many buildings collapsed. Despite the earthquake being felt very strong there, the cause of most of the damage is suspected to be the induced liquefaction in the area. Since the area's mostly made of Quaternary alluvial soil which means it's rather prone to liquefaction, has around 200 drilling sites and boreholes and has many streams or rivers nearby, severe liquefaction was induced and recorded.[13]

Destruction in Istanbul was concentrated in the Avcılar district to the west of the city. Avcılar was built on relatively weak ground, mainly composed of poorly consolidated Cenozoic sedimentary rocks, which makes this district vulnerable to any earthquake.[14]

Damage from the Izmit earthquake

An official Turkish estimate of 19 October 1999 placed the toll at 17,127 killed and 43,953 injured, but many sources suggest the actual figure may have been closer to 45,000 dead and a similar number injured.[6][7] Reports from September 1999 show that 120,000 poorly engineered houses were damaged beyond repair[15] and approximately 20,000 buildings collapsed, resulting in more than 250,000 people becoming homeless after the earthquake.[16] 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.[17] Direct cost of damages is estimated at $6.5 billion US dollars, but secondary costs could exceed $20 billion.[18] In 2010, the research branch of the Grand National Assembly of Turkey released a report stating the amount of casualties as 18,373. In the same report, they have stated that there have been 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 were distributed and 147,120 people were placed into the prefab homes.[19]

There was extensive damage to several bridges and other structures on the Trans-European Motorway (European route E80), including 20 viaducts, 5 tunnels, and some overpasses. Damage ranged from spalling concrete to total deck collapse.[20]

Oil refinery fire

The Tüpraş refinery, where the fire occurred

The earthquake sparked a disastrous 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, results of the quake, nullified attempts at extinguishing the fire. Aircraft were called in to douse the flames with foam. The fire spread over the next few days, warranting the evacuation of the area within three miles of the refinery. The fire was declared under control five days later after claiming at least seventeen tanks and untold amounts of complex piping.[21]

Due to the fire, people within 2 to 3 miles near the refinery needed to evacuate even though some areas were still in the process of search and rescue of people under collapsed buildings.[22]

Tsunami

Many field studies were made about the tsunami that was caused by the 1999 Izmit earthquake in the region, especially in the Gulf of Izmit. Along the northern coast of the gulf, in the basin between Hereke and Tüpraş Petroleum Refinery, the tsunami was like a leading depression wave. The run-up wave heights in this area ranged from 1.5 to 2.6 m, and the waves later decreased to high water levels. The first row of waves arrived on the north coast of the gulf 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 tide carried mussels into buildings and damaged doors and windows. At Körfez, the inland inundation from the waves distance ranged up to 35 m. There were clear watermarks on the walls of buildings including the police station in Hereke, and at a restaurant near Körfez. Locals reported that 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, tide run-up heights were measured in the range of 0.8 to 2.5 m. The tsunami was recorded as a leading depression wave to the west of Kavaklı up to Güzelyalı as well. There, the wave was noticed by locals right after the earthquake. There was severe coastal subsidence as well as slumping of a park near Değirmendere. The subsided area was 250 m along the shore and 70 m perpendicular to shore. The same area included two piers, a hotel, a restaurant, a cafe and several trees. The sea was seen receding by locals about 150 m in less than 2 minutes on the coast near Değirmendere. When the sea came back, it inundated up to 35 m inland, as shown by the mussels and dead fish left in the flooded areas.[23]

The tsunami additionally caused damage to the naval base nearby.[24] The tsunami killed 155 people.[25]

Response

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.

A team of Korean volunteers and locals helping with rescue operations

The following table shows the breakdown of rescue teams by country in the affected locations:

Location Foreign Search and Rescue Teams From:
Gölcük, Kocaeli Hungary, Israel, France, South Korea, Belgium, Russia
Yalova Germany, Hungary, Israel, Poland,[26] United Kingdom, France, Japan, Austria, Romania, South Korea
Avcılar, Istanbul Greece, Germany
İzmit, Kocaeli Russia, Hungary, France, Germany, Austria, Switzerland, United States, Iceland, South Korea
Sakarya Bulgaria, Egypt, Germany, Spain
Düzce Poland,[26] United Kingdom
Bayrampaşa, Istanbul Italy
Kartal, Istanbul Azerbaijan

Search and Rescue Effort as of 19 August 1999. Source: USAID[27]

In total, rescue teams from twelve countries assisted in the rescue effort.

A rescue dog in action

Greece was the first nation to pledge aid and support to hard-stricken Turkey. Within hours of the earthquake, the Greek Ministry of Foreign Affairs contacted their counterparts in Turkey, and the minister sent his personal envoys to Turkey. The Ministry of Public Orders sent in a rescue team of 24 people and 2 trained rescue dogs, as well as fire-extinguishing planes to help with putting out the fire in the Tüpraş Oil refinery.[28]

Oil Spill Response Limited were activated by BP to deploy from the United Kingdom to the Tüpraş Refinery where their responders successfully contained the previously uncontrolled discharge of oil from the site into the sea.[29]

The U.K. 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.[30]

The US President Bill Clinton later visited Istanbul and İzmit to examine the level of destruction and meet with the survivors.[31]

Future risk

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 150-km long submarine seismic gap below the Sea of Marmara could point out to a future, 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.[32]

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 a long way off. The observation of a seismic gap in vicinity to 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 Izmit 1999 rupture and southeast of Istanbul's city center is highlighting the location of likely rupture points for the pending Marmara earthquake. It also limits the maximum size of future events along the whole Marmara seismic gap in case of cascade behavior. Knowing this, the need of a regional earthquake early warning system for Istanbul and surroundings could be justified. The aseismic part of the Princes' Islands segment could represent a potential and likely high-slip area in a future, large earthquake. Fault characterization is likewise very relevant to determine the directivity of earthquake waves approaching Istanbul. Recently made modelling of potential impacts to Istanbul from different scenarios have shown to improve the estimation of hazards the seismic gaps pose. In a similar way, more improved and dense seismic monitoring is expected from on-going efforts to install an underground (borehole-based) seismograph network in the eastern Sea of Marmara region.[32]

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 disaster which could possibly cause thousands of casualties and severe damage. Following the large earthquake in 1999, there was a great urgency 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.[33]

Gallery

  • A flooded Kavaklı Beach in Gölcük and a local passenger ferry in the background

    A flooded Kavaklı Beach in Gölcük and a local passenger ferry in the background

  • A tsunami wave causing minor surge

    A tsunami wave causing minor surge

  • A fault scarp as a result of the earthquake

    A fault scarp as a result of the earthquake

  • A fault's surface rupture right on a pasture in Sakarya

    A fault's surface rupture right on a pasture in Sakarya

  • A collapsed building

    A collapsed building

  • Destroyed buildings along a street

    Destroyed buildings along a street

  • A school class where the fault rupture went right under it

    A school class where the fault rupture went right under it

See also

References

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  2. ^ a b ISC (2014), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 1.05, International Seismological Centre
  3. ^ a b c USGS (September 4, 2009), PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey
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  11. ^ Orgulu, G.; Aktar, M. (2001). "Regional Moment Tensor Inversion for Strong Aftershocks of the August 17, 1999 Izmit Earthquake (Mw =7.4)". Geophysical Research Letters. 28 (2): 371–374. doi:10.1029/2000gl011991. S2CID 128751123.
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  28. ^ Greek and International Aid to Turkey
  29. ^ Girgin S. (2011). "The natech events during the 17 August 1999 Kocaeli earthquake: aftermath and lessons learned". Natural Hazards and Earth System Sciences. 11 (4): 1129–1140. Bibcode:2011NHESS..11.1129G. doi:10.5194/nhess-11-1129-2011.
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  33. ^ "Preparing for the Big One: Learning from Disaster in Turkey". World Bank. Retrieved 2021-11-30.

External links

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