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Earthquake of magnitude 4.3 strikes Tibet

By ANI | Updated: August 26, 2025 08:15 IST

Tibet, August 26 : An earthquake of magnitude 4.3 struck Tibet on Tuesday, a statement by the National Center ...

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Tibet, August 26 : An earthquake of magnitude 4.3 struck Tibet on Tuesday, a statement by the National Center for Seismology (NCS) said.

As per the NCS, the earthquake struck at a depth of 180km.

In a post on X, the NCS said, "EQ of M: 4.3, On: 26/08/2025 07:34:01 IST, Lat: 30.06 N, Long: 84.41 E, Depth: 180 Km, Location: Tibet."

https://x.com/NCS_Earthquake/status/1960163991855976947

Earlier on August 24, an earthquake of magnitude 3.4 struck Tibet at a depth of 98km.

In a post on X, NCS said, "EQ of M: 3.4, On: 24/08/2025 14:11:02 IST, Lat: 28.09 N, Long: 88.08 E, Depth: 98 Km, Location: Tibet."

https://x.com/NCS_Earthquake/status/1959546222710239465

The Tibetan Plateau is known for its seismic activity due to tectonic plate collisions.

Tibet and Nepal lie on a major geological fault line where the Indian tectonic plate pushes up into the Eurasian plate, and earthquakes are a regular occurrence as a result of it. The region is seismically active due to tectonic uplifts that can grow strong enough to change the heights of the Himalayas' peaks.

The Tibetan plateau attains its high elevation due to crustal thickening caused by the collision of the Indian tectonic plate with the Eurasian plate, creating the Himalayas. Faulting within the plateau is associated with strike-slip and normal mechanisms. The plateau extends in an east-west direction evidenced by north-south striking grabens, strike-slip faulting and GPS data.

In the northern region, strike-slip faulting constitutes the dominant style of tectonics while in the south, the dominant tectonic domain is east-west extension on north-south trending normal faults.

Seven north-south trending rifts and normal faults were first discovered in southern Tibet during the late 1970s and early 1980s using satellite imagery. They began formation when extension occurred some 4 to 8 million years ago.

The largest earthquakes in Tibet, with magnitudes of 8.0 or similar, occur along strike-slip faults. Normal faulting earthquakes are smaller in magnitudes; in 2008, five normal faulting earthquakes with magnitudes of 5.9 to 7.1 occurred in various locations across the plateau.

Disclaimer: This post has been auto-published from an agency feed without any modifications to the text and has not been reviewed by an editor

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