China Earthquakes

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Recent Earthquakes in China

China’s earthquake activity is spread across a vast and geologically complicated country. Many earthquakes occur in Tibet, Xinjiang, Qinghai, Gansu, Sichuan and Yunnan, but damaging events have also struck the northern plains, central China and areas that appear relatively quiet on a modern earthquake map.

This page displays the latest available China earthquakes of magnitude 1.5 and above. The earthquake list, interactive map and statistics update when the page loads or refreshes. For activity beyond China, visit the Asia earthquake map or view the latest earthquakes worldwide.

Each coloured circle represents an earthquake location. Select a marker to see its magnitude, reported location, UTC time and depth. The controls allow you to view earthquakes recorded during the last hour, 24 hours, 7 days or 30 days.

China earthquakes (map loads with JavaScript).

Map coverage: This page covers mainland China, including Tibet or Xizang, Xinjiang, Inner Mongolia and Hainan, together with earthquakes assigned to recognised Chinese border regions. Taiwan is excluded because it has a separate earthquake map. Events close to international borders may be included or excluded according to their coordinates and the geographic name assigned by the reporting network.

China’s Deadliest and Most Powerful Earthquakes

China has one of the world’s longest written records of destructive earthquakes. This is a selected chronology rather than a complete catalogue, concentrating on earthquakes notable for their magnitude, loss of life or lasting consequences. Magnitudes assigned to early earthquakes are reconstructions, while historical population losses may include displacement and deaths from exposure, famine or disease after the initial disaster.

• 2025 Dingri earthquake, Tibet: A shallow earthquake struck the Shigatse region on 7 January. Chinese authorities measured it at magnitude 6.8, while international calculations placed it at magnitude 7.1. At least 126 people died, 188 were injured and more than 1,000 homes were damaged. Freezing temperatures and the high altitude complicated rescue and shelter operations. Reuters reported the official figures and conditions in the affected region.
• 2024 Uqturpan earthquake, Xinjiang: The magnitude 7.1 earthquake struck a remote part of western Xinjiang near the Kyrgyzstan border on 23 January. Three people died, homes collapsed and thousands of residents were displaced in severe winter conditions. Its relatively limited death toll reflected the sparse population around the epicentre rather than a lack of destructive shaking. The Associated Press documented the damage and emergency response.
• 2023 Jishishan earthquake, Gansu and Qinghai: A shallow magnitude 6.2 earthquake struck shortly before midnight on 18 December. The disaster killed 149 people, left two others missing at the end of the search period and destroyed more than 14,000 homes. Soft sediments, vulnerable rural buildings and freezing temperatures increased its consequences. Reuters reported the confirmed losses and findings from local authorities.
• 2022 Luding earthquake, Sichuan: The magnitude 6.8 earthquake struck mountainous western Sichuan on 5 September. Ninety-three people died and 25 remained missing, with landslides responsible for a large proportion of the deaths. Roads, communications and access to isolated settlements were severely disrupted. PreventionWeb examines the exceptional landslide impact.
• 2014 Ludian earthquake, Yunnan: Although its magnitude was approximately 6.5, the earthquake devastated a mountainous part of Yunnan. It killed 617 people, injured more than 3,000, destroyed over 60,000 homes and forced nearly 230,000 residents to relocate. Reuters includes the Ludian disaster in its chronology of China’s deadliest recent earthquakes.
• 2013 Lushan earthquake, Sichuan: The magnitude 7.0 earthquake struck close to the southern end of the fault system involved in the 2008 Wenchuan disaster. It killed 196 people, injured thousands and affected more than two million residents. The World Bank discusses the Lushan earthquake in relation to earthquake warning and risk reduction.
• 2010 Yushu earthquake, Qinghai: A magnitude 7.1 earthquake devastated Yushu County on the Tibetan Plateau. At least 2,698 people died, hundreds remained missing and much of the town of Gyêgu was destroyed. The altitude, cold weather and remoteness created additional difficulties for rescuers and survivors. The confirmed figures are included in Reuters’ review of destructive Chinese earthquakes.
• 2008 Wenchuan earthquake, Sichuan: The magnitude 7.9 to 8.0 earthquake ruptured a long section of the Longmenshan fault system between the Tibetan Plateau and the Sichuan Basin. More than 69,000 people died and almost 18,000 remained missing. Entire towns were destroyed, while landslides buried communities, blocked rivers and created unstable earthquake lakes.
• 1976 Tangshan earthquake: A magnitude 7.8 earthquake struck the industrial city of Tangshan in Hebei Province before dawn on 28 July. Official figures record more than 242,000 deaths and approximately 164,000 serious injuries, making it one of the deadliest earthquakes of the twentieth century. Reuters reported the official figures during the disaster’s fiftieth-anniversary commemoration.
• 1950 Assam–Tibet earthquake: This magnitude 8.6 earthquake occurred near the eastern end of the Himalayas and caused severe destruction in southeastern Tibet and northeastern India. It triggered enormous landslides, blocked rivers and altered parts of the mountain landscape. It remains one of the largest instrumentally recorded continental earthquakes. A peer-reviewed study examines its magnitude and extensive surface rupture.
• 1920 Haiyuan earthquake: Approximately 230 kilometres of the Haiyuan Fault ruptured across what is now Ningxia and neighbouring Gansu. Building collapses, landslides and the failure of homes excavated into loess slopes contributed to an enormous death toll. A modern reassessment calculated a moment magnitude of approximately 7.9, lower than some earlier estimates. The peer-reviewed AGU study explains how the earthquake’s magnitude was recalculated.
• 1556 Huaxian earthquake, Shaanxi: This earthquake devastated communities throughout the Wei River Valley during the Ming dynasty. The commonly repeated figure of 830,000 represents a reduction recorded in the regional population and should not be interpreted as a precise count of people killed immediately by the shaking. Collapsing buildings, landslides and the failure of homes cut into loess cliffs were followed by exposure, famine and disease. Research presented by the University of Oxford examines the earthquake’s source and explains why its magnitude remains uncertain.

Why Does China Have So Many Earthquakes?

China doesn’t sit neatly on one plate boundary. Instead, much of its earthquake activity is produced by stresses travelling through the continent from several directions. The most important influence is the continuing collision between the Indian and Eurasian plates, which built the Himalayas, raised the Tibetan Plateau and continues to deform western China.

The collision doesn’t stop at the Himalayan mountain front. Thickened crust beneath Tibet is shortened, stretched and pushed around stronger blocks of continental crust. Movement becomes concentrated along faults separating these blocks, allowing earthquakes to occur more than a thousand kilometres from the main plate boundary.

This helps explain an important feature of China’s earthquake map. The country’s most active regions are generally in the west and southwest, but some of its deadliest historical earthquakes occurred farther east in places such as Shaanxi, Shanxi, Hebei and the North China Plain.

Researchers have mapped thousands of structures capable of accommodating this deformation. The open-access China Active Faults Database brings together national and regional fault surveys conducted over more than two decades.

China’s Main Earthquake Zones

China’s seismic activity doesn’t form one continuous belt. It is divided among mountain ranges, plateaus, rift systems and major strike-slip faults, each behaving differently.

• Tibet and the Himalayan margin: The Indian Plate is pushing beneath Eurasia, thickening the crust and raising the Tibetan Plateau. Southern Tibet is also stretching from east to west, producing north–south rifts and normal faults. The 2025 Dingri earthquake showed that a region created by continental collision can experience strong extensional earthquakes as well as compression.
• Xinjiang and the Tian Shan: Earthquakes occur around the Tian Shan, Pamir and the edges of the Tarim Basin. The Tian Shan lies far north of the direct India–Eurasia boundary, yet it is still being compressed and uplifted. Research into the 2024 Wushi earthquake shows how collision-related stress reaches this distant mountain system.
• Qinghai, Gansu and Ningxia: The northeastern Tibetan Plateau contains the Kunlun, Haiyuan, Qilian and related fault systems. Large strike-slip and thrust earthquakes occur as crustal blocks move around the plateau’s northeastern edge.
• Sichuan and Yunnan: This is one of mainland China’s most persistently active regions. Important structures include the Longmenshan, Xianshuihe, Anninghe, Zemuhe and Red River fault systems. The belts form part of a broad zone transferring deformation from eastern Tibet toward southern China and Southeast Asia.
• The Longmenshan margin: The Longmen Mountains rise sharply where the Tibetan Plateau meets the comparatively rigid Sichuan Basin. Compression and sideways movement are accommodated by a series of faults along this boundary. The 2008 Wenchuan earthquake ruptured part of this system.
• The Shanxi and Weihe rifts: North and east of the Ordos Block, active faults bound a chain of sediment-filled basins. These faults have produced major historical earthquakes, including the devastating 1556 Huaxian earthquake in the Wei River Valley.
• North China and the Bohai region: Faults beneath the North China Plain and around the Bohai Sea have produced destructive intraplate earthquakes. Tangshan lies in this broader setting. The region may appear quieter than western China during an ordinary month, but quiet periods don’t erase its long-term hazard.

The North–South Seismic Belt

Chinese seismologists often refer to a broad north–south seismic belt running through or near Ningxia, eastern Gansu, eastern Qinghai, western Sichuan and Yunnan. It isn’t a single fault. It is a wide zone containing numerous faults and boundaries between crustal blocks along the eastern side of the Tibetan Plateau.

Several of China’s best-known earthquakes have occurred within this wider belt, including the 1920 Haiyuan, 2008 Wenchuan, 2013 Lushan, 2014 Ludian and 2022 Luding earthquakes. The same general region also experiences numerous smaller earthquakes that reveal continuing movement even when no major rupture is underway.

Why Tibet Can Have Both Thrust and Normal-Fault Earthquakes

It can sound contradictory to say that Tibet is being compressed while parts of the plateau are also pulling apart. Both processes can happen at the same time. India’s northward movement thickens and shortens the crust, but the elevated plateau can also spread sideways under its own weight.

This produces large strike-slip faults, compressed margins and north–south rifts within the plateau. The January 2025 Dingri earthquake occurred on a normal fault associated with one of these rift systems. A study of the Dingri rupture identified a surface rupture approximately 25 to 32 kilometres long and vertical movement reaching several metres in places.

The event is a useful reminder that a plate-collision zone isn’t squeezed in only one direction. The crust can shorten, rotate, escape sideways and extend locally as the entire region adjusts.

Earthquake Depth in China

Most earthquakes beneath mainland China begin within the continental crust and are classified as shallow. Shallow earthquakes generally start within about 70 kilometres of the surface, although many damaging Chinese earthquakes have been much shallower than that.

Depth matters because seismic waves from a shallow earthquake travel a shorter distance before reaching towns, roads and buildings. A moderate earthquake only a few kilometres underground can therefore produce severe local shaking, especially if its epicentre is close to a populated area.

China doesn’t have the long, dipping zones of very deep earthquakes seen beneath Japan, Indonesia or the Philippines. Those events occur inside oceanic plates descending at subduction zones. Mainland China’s earthquakes are largely generated by faults within thick continental crust.

Why Landslides and Loess Can Make the Damage Worse

Many of China’s active faults cross steep mountains, deep valleys or areas covered by loess. Loess is a fine, wind-deposited sediment that can form thick, steep-sided landscapes across northern and northwestern China. It can support homes and farmland under ordinary conditions but may collapse, slide or liquefy during strong shaking.

The 1920 Haiyuan earthquake triggered thousands of landslides across the Loess Plateau. More recently, the 2023 Jishishan earthquake caused saturated loess to liquefy and move through Jintian Village as a fast-moving landslide and mudflow. A scientific investigation of the Jintian event describes how the river-terrace sediments failed during the earthquake.

Mountain earthquakes create a different chain of hazards. Rockfalls and landslides may bury buildings, cut roads and block rivers. The 2008 Wenchuan earthquake created numerous landslide dams, forcing emergency crews to deal with the risk of sudden flooding as water accumulated behind unstable debris. NASA satellite imagery documented some of these blocked valleys after the earthquake.

Why Magnitude Isn’t the Same as Earthquake Intensity

Magnitude measures the overall size of an earthquake at its source. Intensity describes how strongly the ground shook at a particular place and what effects occurred there. One earthquake has a single preferred magnitude from each reporting agency, but it produces many different intensities across the affected area.

A shallow earthquake close to a town can produce severe local intensity even if its magnitude is moderate. A much larger earthquake in an isolated part of Tibet or Xinjiang may expose fewer people to destructive shaking. Building design, distance from the fault, soil conditions, topography and landslides all affect the eventual damage.

Why Chinese and International Agencies May Report Different Magnitudes

You may see one magnitude reported by the China Earthquake Networks Center and another in an international catalogue. That doesn’t necessarily mean either agency has made a mistake.

Agencies may use different seismic stations, waveform measurements and magnitude scales. Local or surface-wave calculations can be produced quickly from regional observations, while moment magnitude estimates use longer-period seismic data to estimate the physical size of the rupture. Preliminary figures can also be revised as more information becomes available.

The 2025 Dingri earthquake is a good example. Chinese authorities reported magnitude 6.8, while the USGS calculated moment magnitude 7.1. The 2008 Wenchuan earthquake is commonly described as magnitude 8.0 in Chinese records and magnitude 7.9 by the USGS. These are different measurements of the same earthquakes, not evidence that an additional event occurred.

China’s Long History of Earthquake Detection

China’s relationship with earthquake monitoring began long before electronic instruments. In AD 132, the scholar Zhang Heng described an early seismoscope that used a pendulum-operated mechanism inside a decorated bronze vessel. When shaking triggered the device, a ball reportedly dropped from a dragon’s mouth into a metal toad below, indicating the direction from which the seismic waves had arrived.

The device couldn’t measure magnitude or predict an earthquake, but it was intended to show that a distant earthquake had occurred. The Science Museum Group holds a model of Zhang Heng’s seismoscope, while the USGS describes it as the earliest known seismoscope.

The Haicheng Prediction and What It Really Means

China is also associated with one of earthquake science’s most debated stories. In February 1975, communities around Haicheng in Liaoning Province were evacuated before a destructive earthquake. The event is often presented as the first successful prediction of a major earthquake.

Later investigations found that an unusually strong foreshock sequence played a crucial role in the warnings and evacuations. Most large earthquakes don’t produce such clear foreshocks, and the deadly Tangshan earthquake arrived without a comparable warning the following year.

The USGS review of earthquake prediction notes that the Haicheng action was based mainly on its pronounced foreshock sequence. It shouldn’t be treated as proof that individual earthquakes can now be reliably predicted days in advance.

How China Monitors Earthquakes Today

The China Earthquake Networks Center operates and coordinates national earthquake monitoring, processes seismic data and publishes rapid earthquake information. Provincial networks and research institutes add more detailed regional observations, while international stations help refine the locations and magnitudes of larger events.

China completed a nationwide earthquake early-warning project in 2024. According to the Chinese government’s description of the early-warning network, its stations support rapid earthquake detection and warnings for populated areas and important infrastructure.

Early warning isn’t prediction. The earthquake has already begun when the system detects the first, faster seismic waves. A warning may arrive before the stronger shaking reaches locations farther from the epicentre, potentially allowing trains to slow, machinery to stop and people to take protective action. Communities very close to the fault may receive little or no warning.

Why Small-Earthquake Counts Vary Across China

The map accepts earthquakes of magnitude 1.5 and above when they’re available, but earthquakes of that size aren’t recorded equally across every province. Dense local networks can locate small earthquakes that distant instruments would miss, while remote deserts, plateaus and mountain ranges may have fewer nearby stations.

The map data comes from the ANSS Comprehensive Earthquake Catalog, which combines information from contributing seismic networks. Coverage of larger worldwide earthquakes is more consistent than coverage of small local events. A difference in counts between Sichuan, Tibet and eastern China may therefore reflect both genuine seismic activity and differences in detection or catalogue availability.

Earthquake Risk in China

Western China has the country’s most obvious concentration of modern seismic activity, but earthquake risk depends on more than the number of dots appearing on a recent map. Population, building strength, fault proximity and ground conditions are equally important.

Mountain communities in Sichuan, Yunnan, Tibet, Qinghai and Xinjiang may be exposed to landslides, damaged bridges and blocked roads. Loess regions can experience collapsing slopes and ground failure. Sediment-filled basins may amplify shaking, while older masonry, adobe or poorly reinforced buildings are more vulnerable than well-maintained structures designed for seismic forces.

Scientists can identify active faults, estimate long-term hazard and calculate aftershock probabilities, but they cannot reliably predict the exact time, place and magnitude of a future earthquake. Claims that a particular Chinese city is about to experience a major earthquake should be checked against official seismic and emergency authorities.

What to Do During an Earthquake

If you feel strong shaking, Drop, Cover and Hold On. Drop to your hands and knees, take cover beneath a sturdy table or desk if one is nearby, and hold on until the shaking stops. Keep away from windows, unsecured furniture and objects that could fall.

Don’t run outside while the ground is shaking. If you’re already outdoors, move away from buildings, walls, signs and power lines. In mountainous areas, remain alert for rockfalls and landslides. After the main earthquake, expect aftershocks and follow instructions from local authorities.

Read our earthquake safety guide, earthquake preparedness checklist and explanation of the earthquake magnitude scale.

🗺️ Related Earthquake Maps

Asia overview:
Asia Earthquakes

Neighbouring earthquake regions:
South Asia Earthquakes | Hindu Kush Earthquakes | Taiwan Earthquakes

Other active parts of Asia:
Japan Earthquakes | Philippines Earthquakes | Indonesia Earthquakes | Kamchatka and Kuril Islands Earthquakes