WhiteIndex

Earthquakes in Cyprus, 1926–2026

130on the map
0M ≥ 7
6.8max M
Magnitude
1926
2026
Layers
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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
Elevations of 500, 1,000 and 1,500 m and sea depths of 200, 1,000 and 2,000 m: darker means higher or deeper.
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
Diffuse or poorly mapped zone
Historical events before 1926 (for context)

Fault lines are schematic, drawn from published reviews without precise georeferencing. Construction decisions require Eurocode 8 with the Cyprus National Annex (CYS EN 1998-1, used in the south of the island since 2007; the north uses the Turkish seismic code), data from the Geological Survey Department of Cyprus (seismic network CQ) and site-specific engineering surveys.

All events of magnitude 4.5 and above in the USGS ComCat catalog within 33.5–36.3°N, 31–35.5°E, plus the main active structures.

Main faults

Strongest events (M ≥ 5.5), 1926–2026

DateMDepth, kmLocation (USGS)Structure
1927-06-055.821575 km SE of Tekirova, TurkeyWestern Cyprus Arc segment, Antalya Basin (by location)
1930-05-095.671526 km SSW of Koloni, CyprusCyprus Arc zone (by location)
1941-01-206.03154 km SSE of Lefkónoiko, CyprusCyprus Arc zone (by location)
1953-09-106.32209 km WSW of Paphos, CyprusCyprus Arc zone (by location)
1961-09-155.9306 km SSE of Xylofágou, CyprusCyprus Arc zone (by location)
1977-06-015.76755 km SW of Okurcalar, TurkeyWestern Cyprus Arc segment, Antalya Basin (by location)
1995-02-235.910Cyprus regionCyprus Arc zone (by location)
1996-10-096.83336 km SW of Paphos, CyprusNE–SW tear fault between the western and central segments of the Cyprus Arc
1996-10-095.73328 km SW of Paphos, CyprusCyprus Arc zone (by location)
1996-10-105.73330 km SW of Paphos, CyprusCyprus Arc zone (by location)
1997-01-135.73350 km SSW of Koloni, CyprusCyprus Arc zone (by location)
1999-05-255.61042 km SW of Paphos, CyprusCyprus Arc zone (by location)
1999-08-115.63310 km NNW of Páno Polemídia, CyprusCyprus Arc zone (by location)
2013-12-285.940.777 km SSW of Okurcalar, TurkeyWestern Cyprus Arc segment, Antalya Basin (by location)
2022-01-116.62148 km WNW of Pólis, CyprusCyprus Arc zone (by location)

Structure attribution is an interpretation based on epicentre location and the literature. Stated directly by sources: 9 October 1996, NE–SW tear fault between segments of the Cyprus Arc (Wdowinski et al. 2006). Click a row to show the event on the map.

USGS data as of 13 October 2026

Country analytical review →

Sources and method

Catalog. USGS ComCat, FDSN event web service: M ≥ 4.5, 1926-01-01 to 2026-10-13, 33.5–36.3°N, 31–35.5°E. 130 events in total: 4 of M ≥ 6, 45 of M 5–5.9 and 81 of M 4.5–4.9. Downloaded on 2026-10-13 directly from the USGS server and verified with a checksum. Coordinates and magnitudes are not rounded; place names are as given by USGS, with letters lost in a few USGS names restored (Gazipaşa, Kızkalesi, Yayladağı, Pégeia, Baniyas). Any event can be checked in the USGS search.

Strongest earthquakes. 1953 Paphos earthquake; 1995 Paphos earthquake; 2022 Cyprus earthquake; List of earthquakes in Cyprus; Financial Mirror, 11.01.2022; Cyprus Mail, 12.08.1999; Cyprus Mail, 13.11.2025.

Cyprus Arc, Eratosthenes Seamount, Latakia Ridge and Kyrenia Range. Cyprus Arc; Wdowinski et al. 2006, Geophysical Journal International; Aykut et al. 2025, Nature Communications; Özbey et al. 2024, BSGF; Eratosthenes Seamount; Latakia Ridge; Kyrenia Mountains.

Codes and monitoring. CYS, National Annex to CYS EN 1998-1; FDSN: Cyprus Broadband Seismological Network (CQ); Safkan 2012, 15th WCEE; UNFICYP: the buffer zone.

Historical events. 1222 Cyprus earthquake; Kourion; Cyprus in the Middle Ages; Salamis, Cyprus; Kyriakides et al. 2017.

Terrain and depths. AWS Terrain Tiles (Terrarium format, Mapzen; combines SRTM, GMTED2010, ETOPO1 and other datasets), zoom 8 (about 0.5 km). The data are smoothed and generalised to contours of 500, 1,000 and 1,500 m and depths of 200, 1,000 and 2,000 m; areas smaller than about 100 km² are not shown, so the Troodos summit (1,952 m) does not appear as a separate band.

Intensity zones and impacts. USGS ShakeMap: 1953 (iscgem891997, Atlas v4), 1995 (usp0006tdu, Atlas v4), 1996 (usp0007r4u, Atlas v4), 2022 (us7000gaqu, USGS v7); MMI IV and VI contours simplified to about 1 km (these events have no MMI VIII zone). These are ShakeMap model estimates; for 1953, 1995 and 1996 they are archival ShakeMap Atlas models based on the data available at the time. Losses: 1953 Paphos earthquake; The Cyprus Review 36(1); 1995 Paphos earthquake; List of earthquakes in Cyprus; 2022 Cyprus earthquake.

Coastlines and borders. Natural Earth 1:10m (world-atlas 2.0.2 package), simplified to about 0.3 km; islands smaller than about 2 km² are not shown. Natural Earth divides the island into the Republic of Cyprus, the northern part (areas in which the Government of the Republic of Cyprus does not exercise effective control), the UN buffer zone and the UK Sovereign Base Areas of Akrotiri and Dhekelia. The map shades the whole island in one colour and takes no position on questions of territorial status.

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 Cyprus and the property market

The map window also covers the sea south of Turkey and the coasts of Syria and Lebanon. Almost all seismicity here is linked to the Cyprus Arc, the boundary between the African and Anatolian plates. Between 1926 and 2026 the window recorded 4 earthquakes of magnitude 6 and above and none of magnitude 7 or above. The strongest was M 6.8, on 9 October 1996, south-west of Paphos.

The century's strongest events on the map are linked to the Paphos area. The Paphos earthquake of 10 September 1953 (Mw 6.3) killed 40 people, left about 4,000 homeless and completely destroyed five villages. In 1995, 50 houses were completely destroyed in the Paphos and Nicosia districts. The 2022 earthquake (M 6.6) caused only light damage to a few buildings.

In the south of the island, Eurocode 8 with the Cyprus National Annex (CYS EN 1998-1) has applied since 2007; in the north, Turkish seismic codes apply. So before buying, check the year of construction and which code the building was designed to. Our materials contain no data on how seismic risk is priced into housing in Cyprus, so the patterns from other markets described above serve as a guide.

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 13 October 2026. Faults are drawn schematically from published reviews.