Under land 297 kilometer from Nagqu in China, a shallow and significant MAG-5.1 earthquake occurred in the night of Saturday May 23rd, 2026.
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Earthquake Summary
The earthquake struck on land in China, 297 kilometer (185 mi) northwest of Nagqu in Tibet. The center of this earthquake had a very shallow depth of 10 km. Shallow earthquakes usually have a larger impact than earthquakes deep in the earth.
| Date and Time: | May 23, 2026 01:16 (Shanghai Time) - May 22, 2026 17:16 Universal Time. |
|---|---|
| Location: | 297 km NW of Nagqu, Tibet, China. Coordinates 33°36'30"N 90°8'49"E. |
| Map: | ![]() Map of area around epicenter. Click to open in Google Maps. |
| Magnitude: | MAG 5.1 Detected by 133 stations. Maximum Error Range ±0.049 . |
| Depth: | 10 km (6 mi) A very shallow depth. |
| Tsunami Risk: | Tsunami very unlikely While this was a shallow earthquake, it appears to have occurred under land with a magnitude not strong enough to cause tsunami's. Always stay cautious - More info here. |
Nearby towns and cities
This earthquake may have been felt in China . Located 297 kilometer (185 mi) northwest of the epicenter of this earthquake, Nagqu (Tibet, China) is the nearest significant population center.
Overview of nearby places
| Distance | Place |
|---|---|
| 297 km (185 mi) SE from epicenter |
Nagqu Tibet, China. |
Risk of aftershocks?
This earthquake did not have any significant foreshocks nor aftershocks occurring within 100km (62 mi) of its epicenter.
The risk of aftershocks decreases rapidly over time. Usually, aftershocks are at least one order of magnitude lower than a main shock.
The chance that a significant earthquake like this one is followed by an even larger earthquake is not so large. On average, scientists estimate a 94% chance that a major earthquake will not be followed by an even larger one. It is still adviced to be aware of this risk
Read: How to Stay Safe during an Earthquake (cdc.gov).Earthquakes like this are common in the region
Earthquakes of this strength occur quite regularly in the region. This is the strongest earthquake to hit since January 6th, 2025, when a 5.2 magnitude earthquake hit 290 km (180 mi) further west. An even stronger magnitude 5.7 earthquake struck on August 14th, 2022.
In total, 8 earthquakes with a magnitude of 5.1 or higher have been registered within 300km (186 mi) of this epicenter in the past 10 years. This comes down to an average of once every year.
Tsunami very unlikely
While MAG-6.5+ earthquakes may cause tsunami's, it appears that the epicenter of this earthquake hit under land. In addition, the reported depth is deeper than 100km, making the risk of a tsunami even less likely. However always stay cautious and monitor advice from local authorities.
Tsunami Risk Factors
| Factor | Under Sea? | MAG-6.5 or stronger? | Shallow depth? |
|---|---|---|---|
| Explanation | Almost all tsunami's are caused by earthquakes with their epicenter under sea or very near the sea. However stay cautious in coastal areas as earthquakes on land may cause landslides into sea, potentially still causing a local tsunami. | Under MAG 6.5: Very unlikely to cause a tsunami. MAG 6.5 to 7.5: Destructive tsunami's do occur, but are uncommon. Likely to observe small sea level changes. MAG 7.6+: Earthquakes with these magnitudes might produce destructive tsunami's. |
Most destructive tsunami's are caused by shallow earthquakes with a depth between 0 and 100km under the surface of the earth. Deeper tsunami's are unlikely to displace to ocean floor. |
| This Earthquake | Not this earthquake. This earthquake appears to have struck on land far from any coast. |
Not this earthquake. This earthquake had a magnitude of 5.1. Earthquakes of this strength are unlikely to trigger a tsunami. |
This earthquake occurred at a depth of of 10 km (6 mi). Earthquakes this shallow could trigger a tsunami. |
Sources
Last updated 22/05/26 20:58 (). As more information on this earthquake becomes available this article will be updated. This article is automatically composed based on data originating from multiple sources.

