Earthquakes in Turkey

North-western Turkey, the county's most densely populated region and industrial heartland, has been struck by two massive earthquakes in less than three months in 1999. The first, on 17 August 1999 at 03:02 local, measured 7.4 on the Richter scale and lasted 45 seconds. Izmit, an industrial city of than-1,2 million in western Turkey, was nearest the epicenter. The official death toll stands at 17,480, with some 44,000 people injured, nearly 300,000 homes either damaged or collapsed and more than 40,000 business premises similarly affected. On the day of the catastrophe, the Turkish government declared a state of emergency and requested international assistance. The International Federation immediately launched an appeal, and many foreign rescue teams were deployed to help local rescue teams on ground.

The disaster was followed by more than 1,300 aftershocks, culminating in the second quake - which shook Düzce and Kaynasli in the north-western province of Bolu, some 100 kilometers (63 miles) to the east of Izmit for 30 seconds - at 18:57 on 12 November 1999 and rated 7.2 on the Richter scale. The jolt was felt both in Istanbul (some 260 km to the west) and Ankara, the nation's capital, 300 km to the east.

Another big earthquake hit the city of Bingöl, Eastern part of Turkey, on 1st of May 2003, killing 176 people (mostly elementary school kids sleeping in their dormitory). The quake came at 03:27 local time lasting for about 17 seconds with a Richter scale of 6.4.

Then on 23rd of October 2011, a 7,2 magnitude earthquake hit the province of Van and its district Ercis in Eastern Anatolia at 13:41 local time, killing 644 people.

On 24th of January 2020, a 6,8 magnitude earthquake hit the provinces of Elazig and Malatya at 20:55 local time, killing 38 people and injuring over 1600.

On 30th of October 2020, a 6,6 magnitude (some sources say 6,9-7,0) earthquake in the Aegean Sea hit Izmir and surroundings, killing 114 people and injuring over a thousand. The quake even caused a tsunami in Sigacik (ancient Teos) town.

Last major earthquakes occured on 6th of February 2023 in Kahramanmaras and Hatay provinces, southeastern Turkey. These were 7,7 and 7,6 magnitude quakes, killing over 50 thousand people.

You can click for the latest earthquakes in Turkey based on:
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Data provided by Kandilli Observatory of Bogazici University in Istanbul
Latest Earthquake Map
Map provided by AFAD - Emergency Management Authority of Turkey
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Earthquake faults in Turkey

Izmit - Golcuk Quake

17 August 1999

The Izmit earthquake occurred at 03:02 local time, and was centered at 40.702° N., 29.987° E., which places the epicenter about 11 kilometers (7 miles) southeast of the city of Izmit. This location indicates that the earthquake occurred on the northernmost strand of the North Anatolian fault system. The earthquake originated at a depth of 17 kilometers (about 10.5 miles) and caused right-lateral strike-slip movement on the fault. Preliminary field reports confirm this type of motion on the fault, and initial field observations indicate that the earthquake produced at least 60 kilometers (37 miles) of surface rupture and right-lateral offsets as large as 2.7 meters (9 feet).

The earthquake likely occurred on a branch of the North Anatolian fault. Although this is the largest earthquake in the epicenter region in this century, the region of the earthquake has a long history of destructive earthquakes. In 1967, a magnitude 7.1 earthquake caused extensive damage along the North Anatolian fault just east of the current shock.

The 900 km-long North Anatolian fault has many characteristics similar to California's San Andreas fault. These two faults are right-lateral, strike-slip faults having similar lengths and similar long-term rates of movement. If a person is looking across a right-lateral, strike-slip fault during such an earthquake, that person would see the opposite side move to the right.

The North Anatolian fault has produced seven large (MS) 7.0 earthquakes in the period from 1939 through 1999. These earthquakes have ruptured the fault progressively from east to west. Following are data for the seven large earthquakes that have progressively ruptured the North Anatolian fault:

  • 1939 December 26. Magnitude (MS) 7.9 - 8.0. 30,000 deaths. Fault length about 360 km. Initiated the eastward migration of significant earthquakes on the North Anatolian fault. (Termed the 1939 Erzincan earthquake)
  • 1942 December 20. Magnitude (MS) 7.1. Fault length about 50 km. (Termed the 1942 Erbaa earthquake)
  • 1943 November 26. Magnitude (MS) 7.6. Fault length about 280 km. (Termed the 1943 Tosya earthquake)
  • 1944 February 01. Magnitude (MS) 7.3. Fault length about 165 km. (Termed the 1944 Bolu-Gerede earthquake)
  • 1957 May 26. Magnitude (MS) about 7. Fault length about 30 km. (Termed the 1957 Abant earthquake)
  • 1967 July 22. Magnitude (MS) 7.1. Fault length about 80 km. (Termed the 1967 Mudurnu Valley earthquake)
  • 1999 August 17. Magnitude (MS) 7.8; MW 7.4-7.5)

Earthquakes on the North Anatolian fault are caused by the northwards motion of the Arabian plate against the Eurasian plate, squeezing the small Turkish micro plate westwards. Also, compression in this region is due to the northwards motion of the African plate, which produces subduction at the Cyprus and Hellenic arcs. The small Turkish micro plate is bounded on the east by the East Anatolian fault zone (EAFZ), on the north by the North Anatolian fault zone (NAFZ), on the west by a diffuse zone of deformation surrounding the greater Aegean region, and on the south by the Hellenic and Cyprus arcs.

Düzce Quake

12 November 1999

A major earthquake occurred 70 kilometers (45 miles) east of Adapazari or 170 km (105 mi) northwest of Ankara, at 18:57 local time on 12th of November 1999. A magnitude of 7.2 was computed for this earthquake. This earthquake is located about 110 km (70 miles) east of the magnitude 7.4 main shock on August 17 which killed over 17,000 people and injured another 50,000 around Izmit.

Casualty figures from this last earthquake stand around 845 confirmed dead and around 5,000 injured. The destruction in Bolu and Düzce was widespread, with the total affected population between 150,000 and 180,000. Some assessments indicated that over 18 thousand buildings have been heavily damaged and the Government has estimated the financial cost of the quake at 10 billion US dollars. Industrial facilities in the area have stopped their production due to power shortages and some have suffered major material damage.

During the morning of 17 November two major aftershocks (4.9 at 02h00 and 5.0 at 10h10) were felt in the provincial capital of Bolu bringing more fear and despair to the population as damaged buildings collapsed. About 24,000 families (80% of the town's population) were homeless. The local crisis centre in Bolu called upon rescue and humanitarian workers in Düzce for help in the middle of the night. The Prime Minister's Crisis Center (PMCC) urgently sent 10,000 tents for the affected area. Temporary houses were constructed as well.

Besides Bolu and Düzce, the neighboring districts of Kaynasli (70% of the town is considered to be destroyed), Akcakoca, Cumayeri, Gümüsova, Yigilca and Gölkaya have been affected. With night-time temperatures dropping as low as minus two degrees Celsius, the majority of the region's population remained outdoors either because their homes were damaged or for fear of entering buildings even though many appeared structurally sound. Population movements away from the region were also increasing on a daily basis. According to the PMCC, 1,000 prefabricated houses constructed in Düzce for victims of the August earthquake were been immediately reassigned to the locality.

Meanwhile, many hospital facilities in the affected area were damaged and were no longer functioning. Field facilities surrounding the hospital buildings were set up immediately after the quake, with volunteer doctors and nurses coming from nearby towns to treat the injured. Severe cases were referred to hospitals both in Ankara and Istanbul. All schools in Düzce and Kaynasli were closed due to damage and they continued to teach in winterized tents or temporary buildings.

State crisis centers established in Düzce and Bolu, coordinating search and rescue teams from all over the world. Some 12,000 rescue workers came to the area and the total number of people pulled alive from collapsed buildings is estimated at 300. Rescue activities were ceased after some period giving way to the process of debris removal.

Van - Ercis Quake

23 October 2011

Another major earthquake hit Eastern Turkey, the province of Van and its district Ercis, on 23rd of October 2011, at 13:41 local time. A magnitude of 7.2 was computed for this earthquake and lasted less than 30 seconds. Hundreds of aftershocks were recorded, some being as large as 5,7 in magnitude causing some more damage.

Many buldings have collapsed during the earthquake in the city center and in Ercis town, as well as in its villages. The death toll has reached 644 people with over two thousand injured. Several rescue teams have immediately arrived on the spot to carry out their mission, a total of 222 residents were pulled out alive off the debris. Temporary tents and other equipments have been sent to the area. The officials are trying to replace tents with hard containers as soon as possible in order to ease the winter conditions, and then new homes were constructed within a couple of years.

Kahramanmaras - Hatay Quake

6 January 2023

On 6th of February 2023, two major earthquakes hit many provinces in southeastern Turkey. First one came at 04:17 AM with a magnitude of 7.7 in Pazarcik - Kahramanmaras province and lasted 70 seconds, then the second quake at 13:24 with a magnitude of 7.6 in Elbistan and lasted 35 seconds. These two powerful quakes leveled many cities in the region, as well as in Syria, being felt also in Lebanon, Iraq, Jordan, Israel and Egypt. The provinces affected were Kahramanmaras, Hatay, Malatya, Gaziantep, Osmaniye, Adana, Diyarbakir, Sanliurfa, Adiyaman, Kilis, and Elazig, the first two suffering the most of the damage. Besides many aftershocks in the following weeks, some being even at magnitude of 6, on 20th of February at 20:04 other two big earthquakes hit the same region, in Defne and Samandag districts of Antakya, during which many of the damaged buildings from the first quakes were collapsed.

After the first shock at the beginnig, help was rushed to the quake-hit region. Besides many local Search and Rescue (SAR) teams, over 9 thousand SAR personnel from about 90 countries came to help in the upcoming days in order to save lives from the rubbles, all working under the coordination of AFAD, Disaster and Emergency Management. Tents and container cities are established, field hospitals are settled, schools are closed. State of emergency was announced in this area for 3 months.

Because of the size and its damage, these quakes are considered as the worst disaster of the century. Also, it's the deadliest quake in the history of Turkey: over 50 thousand deaths announced officially, and over 122 thousand injured. It's also the second deadliest quake disaster in the world, after Haiti in 2010 which killed 220 thousand.

This area in Turkey covers around 350.000 square kilometers (140.000 square miles) which is equal to the total area of Germany. The tragedy affected 14 million people, around 16% of the total population. The cost of the damage to the economy is estimated to be over 105 billion US dollars.

The Richter Magnitude Scale

Seismic waves are the vibrations from earthquakes that travel through the Earth; they are recorded on instruments called seismographs. Seismographs record a zigzag trace that shows the varying amplitude of ground oscillations beneath the instrument. Sensitive seismographs, which greatly magnify these ground motions, can detect strong earthquakes from sources anywhere in the world. The time, locations, and magnitude of an earthquake can be determined from the data recorded by seismograph stations.

The Richter magnitude scale was developed in 1935 by Charles F. Richter of the California Institute of Technology as a mathematical device to compare the size of earthquakes. The magnitude of an earthquake is determined from the logarithm of the amplitude of waves recorded by seismographs. Adjustments are included for the variation in the distance between the various seismographs and the epicenter of the earthquakes. On the Richter Scale, magnitude is expressed in whole numbers and decimal fractions. For example, a magnitude 5.3 might be computed for a moderate earthquake, and a strong earthquake might be rated as magnitude 6.3. Because of the logarithmic basis of the scale, each whole number increase in magnitude represents a tenfold increase in measured amplitude; as an estimate of energy, each whole number step in the magnitude scale corresponds to the release of about 31 times more energy than the amount associated with the preceding whole number value.

At first, the Richter Scale could be applied only to the records from instruments of identical manufacture. Now, instruments are carefully calibrated with respect to each other. Thus, magnitude can be computed from the record of any calibrated seismograph.

Earthquakes with magnitude of about 2.0 or less are usually call micro earthquakes; they are not commonly felt by people and are generally recorded only on local seismographs. Events with magnitudes of about 4.5 or greater - there are several thousand such shocks annually - are strong enough to be recorded by sensitive seismographs all over the world. Great earthquakes, such as the 1964 Good Friday earthquake in Alaska, have magnitudes of 8.0 or higher. On the average, one earthquake of such size occurs somewhere in the world each year. Although the Richter Scale has no upper limit, the largest known shocks have had magnitudes in the 8.8 to 8.9 range. Recently, another scale called the moment magnitude scale has been devised for more precise study of great earthquakes. The Richter Scale is not used to express damage. An earthquake in a densely populated area which results in many deaths and considerable damage may have the same magnitude as a shock in a remote area that does nothing more than frighten the wildlife. Large-magnitude earthquakes that occur beneath the oceans may not even be felt by humans.

Source: This Information was provided by USGS - National Earthquake Information Center

Earthquakes in Turkey that caused 10,000 or more deaths

Source Date Lat  Lon  Mag  Deaths General area
NG(2) 342 36.2 36.1   40,000? Antakya (Antioch)
NG(2)  565 36.2 36.1   30,000? Antakya
ITU 688 38.4 27.2 7.0(ISK) 20,000 Izmir
NG(120) 847 36.2 36.1   20,000 Antakya
ITU 1268 39.8 40.4   15,000 Erzincan-Erzurum
NG(2,7,55) 1268 37.5 35.5   60,000? NE of Adana
ITU 1458 39.9 40.4   30,000 Erzincan-Erzurum
ITU,NG(51,73) 1509, Sep 14 40.7 29.3 7.0(ISK) 13,000 Istanbul
ITU,NG(2,51) 1653, Feb 23 38.2 28.2 7.5(ISK) 2,500-15,000 East of Izmir
ITU,NG(2,5b) 1688, Jul 12 38.4 26.9 7.5(ISK) 15,000-20,000 Izmir
NG(99) 1859, Jun 02 39.9 41.3 6.4(ISK) 15,000 Erzurum
ITU,NG(55,99) 1883, Oct 15 38.3 26.2 7.0(ISK) 15,000 West of Izmir
ITU,NG(2,3,138) 1939, Dec 26 39.5 38.5 7.9(ISK) 30,000 Erzincan
ITU 1999, Aug 17 40.7 30.0 7.8(MAG) 17,480 Izmit-Golcuk
AFAD 2023, Feb 6     7.7(MAG) 50,000+ Kahramanmaras-Hatay

Notes: It is possible that there is really only one quake in 1268. Turkish sources do not list the event near Adana. Also, NG(2) seems to have very large casualty figures that are not included with Turkish sources. Therefore, a question mark has been added after the values.


  • ISK: Earthquake catalog of Kandilli Observatory, Bogazici University, Istanbul, supplied by NOAA/NGDC (Meyers and Von Hake), Boulder CO, 1985.
  • ITU: K. Ergin, U. Guclu and Z. Uz, A Catalog of Earthquakes for Turkey and Surrounding Area (11 AD to 1964 AD), Technical University of Istanbul, Faculty of Mining Engineering, 1967.
  • AFAD: Earthquake Risk Map by AFAD, Department of Disasters and Emergency Management, 2018.
  • NG(n): R. Ganse and J. Nelson, Catalog of Significant Earthquakes 2000 BC - 1979 Including Quantitative Casualties and Damage, NOAA/NGDC Report SE-27, Boulder CO, 1981. The number in parentheses is from their references table, as listed below:
    • 2: Lomnitz, Global Tectonics and Earthquake Risk, 1974.
    • 3: Bath, Introduction to Seismology, 1978.
    • 5b: (there is no source 5b -- probably should be 55?).
    • 7: Meyers and von Hake, Earthquake data file summary, 1976.
    • 51: Munchener Ruckversicherungs-Gesellschaft, World Map of Natural Hazards, 1978.
    • 55: Milne, Catalogue of Destructive Earthquakes, 1911.
    • 73: U.S. Congress, Great Earthquakes, 1888.
    • 99: Karnik, Seismicity of the European Area, 1971.
    • 120: Alsinawi and Galih, Historical Seismicity of Iraq, 1978.
    • 138: Ambraseys, Middle East A Reappraisal of Seismicity, 1978.