WhiteIndex

Earthquakes in Uzbekistan, 1926–2026

452on the map
8M ≥ 7
7.54max 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
Elevations of 500, 1,000, 2,000, 3,000 and 4,000 m: darker means higher.
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 Uzbekistan’s current code “Construction in seismic areas” (2.01.03-19) with the seismic-safety requirements updated in 2025, the seismic zoning map of the G. A. Mavlyanov Institute of Seismology and site-specific engineering surveys.

All events of magnitude 4.5 and above in the USGS ComCat catalog within 37.2–45.8°N, 55.8–73.2°E, plus the main active faults.

Main faults

Strongest events (M ≥ 7), 1926–2026

DateMDepth, kmLocation (USGS)Structure
1929-05-017.21040 km SSE of Baharly, TurkmenistanKopet Dag (by location)
1946-11-027.542534 km N of Kerben, KyrgyzstanChatkal Range, western Tien Shan (by location)
1948-10-057.151514 km N of Ashgabat, TurkmenistanKopet Dag (by location)
1949-07-107.52043 km ENE of Rasht, TajikistanNorthern Pamir front, Vakhsh thrust zone (by location)
1976-04-0873333 km NE of Gazli, UzbekistanGazli zone, Kyzylkum (by location)
1976-05-1771027 km N of Gazli, UzbekistanGazli zone, Kyzylkum (by location)
1984-03-19714.522 km NNW of Gazli, UzbekistanGazli zone, Kyzylkum (by location)
2015-12-077.222104 km W of Murghob, TajikistanPamir (by location)

Structure attribution is an interpretation based on epicentre location and the literature; fault traces are schematic. Click a row to show the event on the map.

USGS data as of 13 October 2026

Sources and method

Catalog. USGS ComCat, FDSN event web service: M ≥ 4.5, 1926-01-01 to 2026-10-13, 37.2–45.8°N, 55.8–73.2°E. 1,691 events in total: 44 of M ≥ 6 and 1,647 of M 4.5–5.9. Downloaded on 2026-10-13 directly from the USGS server and verified with checksums. Events of M ≥ 6 and the 1966 Tashkent earthquake are given at full precision with the USGS place name; for the rest, coordinates are rounded to 0.01° and magnitude to 0.1 (values of 5.95–5.99 are shown as 5.9), and place names were not kept. USGS dates the Tashkent earthquake 25 April 1966 in UTC (26 April, 05:23 local time) and places the epicentre 9 km NNW of Tashkent. Any event can be checked in the USGS search.

Strongest earthquakes. 1966 Tashkent earthquake; Настоящее время: Ташкентское землетрясение; NZSEE Bulletin 1977: Gazli; COSMOS: Gazli 1976; Christian Science Monitor, 1984; Bossu et al. 1996, BSSA; Plotnikova et al. 1996, PAGEOPH; 2011 Fergana Valley earthquake; 1946 Chatkal earthquake; 1948 Ashgabat earthquake; 1949 Khait earthquake.

Tien Shan, Talas–Fergana Fault, Pamir. Rizza et al. 2019, Tectonics: Talas–Fergana Fault; Dense GNSS profiles across the NW tip of the India–Asia collision (Pamir); List of earthquakes in Tajikistan.

Codes, monitoring, borders. E3S Web of Conferences 474 (2024): BRR 2.01.03-19; Anhor.uz, 18.11.2025; Kun.uz, 24.03.2023: MES list of settlements; Sokh District; Shohimardon; Vorukh.

Historical events. 1902 Andijan earthquake; 1907 Qaratog earthquake.

Terrain. AWS Terrain Tiles (Terrarium format, Mapzen; combines SRTM, GMTED2010, ETOPO1 and other datasets), zoom 6 (about 2 km). The data are smoothed and generalised to contours of 500, 1,000, 2,000, 3,000 and 4,000 m; areas smaller than about 700 km² are not shown.

Intensity zones and impacts. USGS ShakeMap: 1946 (iscgem898647, Atlas v4), 1948 (iscgem897583, Atlas v4), 1949 (iscgem896645, Atlas v4), 1976 (usp0000gcj, Atlas v4), 1984 (usp00022s5, Atlas v4), 2011 (usp000j560, Atlas v4); MMI IV, VI and VIII contours simplified to about 2 km. These are ShakeMap Atlas model estimates based on the data available at the time; USGS has no ShakeMap for the 1966 Tashkent earthquake. Losses: 1966 Tashkent earthquake; Настоящее время; 1946 Chatkal earthquake; 1948 Ashgabat earthquake; 1949 Khait earthquake; NZSEE 1977; CSM 1984; 2011 Fergana Valley earthquake.

Coastlines and borders. Natural Earth 1:10m (world-atlas 2.0.2 package), simplified to about 1 km; areas smaller than about 20 km² are not shown; the Aral Sea and other lakes are not shown separately. Borders follow Natural Earth and are approximate. The Fergana Valley contains enclaves: Sokh and Shohimardon (Uzbekistan) and Vorukh (Tajikistan); some boundaries are being settled under treaties of 2022–2025. The map takes no position on their legal 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 Uzbekistan and the property market

The map window covers all of Uzbekistan and neighbouring parts of Kazakhstan, Kyrgyzstan, Tajikistan, Turkmenistan and Afghanistan. Between 1926 and 2026 it recorded 44 earthquakes of magnitude 6 and above, 8 of them of magnitude 7 and above. The strongest was M 7.54, on 2 November 1946, in the Chatkal Range (Kyrgyzstan). The most active zones, the Pamirs and the mountains of Tajikistan, lie beyond Uzbekistan's borders.

For housing, what matters is not only magnitude but also where the focus lies and what the houses are built of. The Tashkent earthquake of 26 April 1966 was moderate, with a magnitude of about 5.1–5.3, but its focus lay 3–8 km directly beneath the city centre. Between 200,000 and 300,000 people were left homeless and 78,000–95,000 houses, mostly mud-brick, were destroyed. Gazli was hit by three M 7.0 earthquakes in 1976 and 1984; in 1984, according to Soviet press reports, even "earthquake-resistant" buildings collapsed because of poor construction quality. The 2011 Fergana Valley earthquake (M 6.1) damaged at least 800 houses.

A buyer in Uzbekistan should check not only the year of construction but also the materials and build quality. The code "Construction in seismic regions" (2.01.03-19) applies, with seismic safety requirements updated in 2025; the seismicity of a site is shown on the zoning map of the G. A. Mavlyanov Institute of Seismology. Our materials contain no data on how seismic risk is priced into housing in Uzbekistan, 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.