WhiteIndex

Earthquakes in Turkey, 1926–2026

107on the map
23M ≥ 7
7.8max M
Magnitude
1926
2026
Layers
WhiteIndex

Tap a circle or a line on the map to see the details

M 6 · 6.5 · 7 · 7.5 (outlined if M ≥ 7)
M 4.5 · 5.5 (smaller events, no outline)
Subduction zone / thrust belt (teeth on the overriding side)
Strike-slip fault / transform zone
Normal fault (graben boundary), ticks on the downthrown side
Diffuse or poorly mapped zone
Shaking intensity zones from USGS ShakeMap (MMI scale: IV, VI, VIII). Shown when you select an event.
zones (model) — a USGS model reconstruction (ShakeMap Atlas), not measurements
Historical events before 1926 (for context)

Fault lines are schematic, drawn from published reviews without precise georeferencing. Construction decisions require the MTA active fault map (General Directorate of Mineral Research and Exploration of Turkey), AFAD and Kandilli Observatory data, and site-specific engineering surveys.

All events of magnitude 4.5 and above in the USGS ComCat catalog within 35.5–42.5°N, 25.5–45°E, plus the region’s main active faults.

Main faults

Strongest events (M ≥ 7), 1926–2026

DateMDepth, kmLocation (USGS)Structure
1928-04-147.1109 km S of Stara Zagora, BulgariaBulgaria, outside the structures shown
1930-05-067.11510 km SSW of Salmās, IranNorth-western Iran (Salmas), outside the structures shown
1939-12-267.82020 km NNE of Erzincan, TurkeyNorth Anatolian Fault (Erzincan)
1942-12-2071013 km SE of Ayvacık, TurkeyNorth Anatolian Fault (Niksar–Erbaa)
1943-11-267.5206 km SSE of Ilgaz, TurkeyNorth Anatolian Fault (Tosya–Ladik)
1944-02-017.63010 km WNW of Orta, TurkeyNorth Anatolian Fault (Bolu–Gerede)
1948-02-097.31515 km NNW of Karpathos, GreeceHellenic Arc, Karpathos (by location)
1949-07-237.16159 km NNW of Karaburun, TurkeyWestern Anatolia, Karaburun Peninsula (by location)
1953-03-187.3107 km N of Gönen, TurkeyNorth-western Anatolia, Gönen (by location)
1956-07-097.72019 km SSE of Amorgós, GreeceSouthern Aegean, Amorgos (by location)
1957-04-247.13527 km SSE of Sarigerme, TurkeyHellenic Arc, off Fethiye (by location)
1957-04-257.33534 km S of Sarigerme, TurkeyHellenic Arc, off Fethiye (by location)
1957-05-267.092513 km SSW of Düzce, TurkeyNorth Anatolian Fault (Abant)
1967-07-227.2913.59 km E of Akyazı, TurkeyNorth Anatolian Fault (Mudurnu)
1970-03-287.2322.222 km NE of Gediz, TurkeySimav–Gediz faults (Gediz)
1976-11-247.33647 km S of Doğubayazıt, TurkeyÇaldıran Fault
1991-04-29717.222 km WNW of Java, GeorgiaGreater Caucasus, Racha (Georgia), outside the structures shown
1999-08-177.6174 km ESE of Derince, TurkeyNorth Anatolian Fault (İzmit)
1999-11-127.2108 km S of Düzce, TurkeyNorth Anatolian Fault (Düzce)
2011-10-237.11827 km NNE of Van, TurkeyThrust north of Van (by mechanism)
2020-10-3072113 km NNE of Néon Karlovásion, GreeceNormal fault north of Samos, Aegean Sea
2023-02-067.810Pazarcik earthquake, Kahramanmaras earthquake sequenceEast Anatolian Fault (Pazarcık)
2023-02-067.57.4Elbistan earthquake, Kahramanmaras earthquake sequenceÇardak–Sürgü zone (Elbistan)

Structure attribution is an interpretation based on epicentre location and the literature. Stated directly by sources: the 1939–1999 North Anatolian Fault sequence, 2023 (East Anatolian Fault and the Çardak–Sürgü zone), 1976 (Çaldıran Fault), 1970 (Gediz), 2011 (Van), 2020 (Samos). Click a row to show the event on the map.

USGS data as of 11 October 2026

Country analytical review →

Sources and method

Catalog. USGS ComCat, FDSN event web service: M ≥ 4.5, 1926-01-01 to 2026-10-11, 35.5–42.5°N, 25.5–45°E. 2,366 events in total: 107 of M ≥ 6, 861 of M 5–5.9 and 1,398 of M 4.5–4.9. Downloaded on 2026-10-11 directly from the USGS server and verified with checksums. For events below M 6, coordinates are rounded to 0.01° and magnitude to 0.1; place names were not kept. Some USGS place names had Turkish letters replaced by “?”; we restored them. Any event can be checked in the USGS search.

North Anatolian Fault and the 1939–1999 sequence. Wikipedia: North Anatolian Fault; 1939 Erzincan earthquake; 1999 İzmit earthquake.

East Anatolian Fault and 2023. Wikipedia: East Anatolian Fault; 2023 Turkey–Syria earthquakes.

Dead Sea Transform. Wikipedia: Dead Sea Transform.

Hellenic arc. Wikipedia: Hellenic arc.

Western Anatolia. Gediz Graben, Plymouth University: pearl.plymouth.ac.uk; Wikipedia: Büyük Menderes Graben; 1970 Gediz earthquake; 2020 Aegean Sea earthquake.

Bitlis–Zagros suture. Okay et al., Geology, “Arabia–Eurasia collision”: web.itu.edu.tr.

Eastern Turkey. 1976 Çaldıran–Muradiye earthquake; 2011 Van earthquake.

Historical events. 1509 Constantinople earthquake; 1912 Mürefte earthquake.

Coastlines. Natural Earth 1:10m (world-atlas 2.0.2 package); lakes are not shown separately.

Sources for the text

How earthquakes affect property prices

Seismic risk is one of the few factors that lowers property values for a long time and in a measurable way. This is not a forecast but a finding from markets where the risk has been officially mapped and prices can be tracked for years.

  • New Zealand. After the 2010–2011 earthquakes, land in Christchurch was classified by liquefaction risk. By the third year, homes in the highest-risk category had lost 17.7% of their value relative to neighbouring land, and the gap has held steady at around 13%.
  • California. When a plot is placed inside an official active fault zone, its value falls by 6.6% on average and its rent by 3.3%.
  • Tokyo. According to the official seismic hazard map, land in the riskiest zones is about 10% cheaper than in the safest ones.
  • Japan overall. Before major earthquakes, buyers barely priced in seismic risk. Afterwards, the discount in hazardous areas became noticeable and more than doubled.

What this means for a buyer

Three patterns repeat across all these markets.

  1. Prices react to visible risk. A discount appears once the risk is officially disclosed or the country has lived through a strong earthquake. Earlier risk maps of Christchurch that nobody paid attention to had no effect on prices.
  2. The building matters more than the country. Within the same city, the biggest discounts hit buildings constructed before current seismic codes, on weak soils or close to a fault. In Istanbul this has shown up in bank valuations since 2023.
  3. Commercial property is penalised harder. In Wellington, commercial buildings officially classified as earthquake-prone sell for 45% less on average.

For an investor, an earthquake map is therefore not geography but part of the valuation of a property. It shows how likely a shock that changes the price is, and in which parts of the country it is more likely.

What to check before buying in a seismic country

  • The year of construction and which edition of the seismic code the building was designed to.
  • The type of soil and the distance to active faults.
  • Earthquake insurance: whether it is mandatory and what it covers.
  • For high-rises, an independent structural report, not just the developer’s documents.

Earthquakes in Turkey and the property market

Between 1926 and 2026 the map window contains 107 earthquakes of magnitude 6 or more, 23 of them of magnitude 7 or more. The strongest was M 7.8.

After the earthquakes of 6 February 2023, the Istanbul market started to differentiate districts by risk. According to 139,913 bank valuations of homes, prices in low-risk districts rose about 4.8% more than in high-risk ones. In hazardous districts, homes built before the 2007 seismic code lose more value than newer ones.

Turkey has compulsory earthquake insurance for homes, known as DASK. The policy is checked when a sale is registered at the land registry, and a mortgage is not issued without it.

Questions and answers

Does seismic risk affect property prices?
Yes. Studies from Japan, California, New Zealand and Turkey show that housing in high seismic-risk zones is cheaper, and the gap widens after strong earthquakes.
How much cheaper is housing in earthquake-prone areas?
Between 2% and 18%, depending on the study. The gap is largest where the risk is officially mapped: 13–18% in Christchurch, about 10% in Tokyo and 6.6% in California.
What matters more — the country’s seismicity or the specific building?
The building. Within the same city, the biggest discounts hit buildings constructed before current codes and those on weak soils or near faults.
Where does the map data come from?
The USGS ComCat earthquake catalogue: all events of magnitude 4.5 and above from 1926 to 2026, downloaded on 11 October 2026. Faults are drawn schematically from published reviews.