Post by : Mina Rahman
Recently, Tibet was jolted by two earthquakes, heightening worries regarding seismic safety. The first quake, registering a magnitude of 4.3, struck at a depth of 90 kilometers on January 14, 2026, at 12:27 PM IST, with coordinates 27.96° N latitude and 87.87° E longitude.
Earlier, on January 13, 2026, at 11:50 PM IST, a second quake of 3.8 magnitude occurred at a shallower depth of 10 kilometers, found at 30.49° N latitude and 81.25° E longitude.
Shallow seismic events, like the latter, pose increased risks due to their proximity to the surface, leading to stronger shaking and a higher potential for damage and loss of life.
The Tibetan Plateau is known for its seismic activity, as the Indian tectonic plate converges with the Eurasian plate. This interaction causes elevation of the land, forming the Himalayas and triggering frequent quakes.
Various fault systems sculpt the geology of the area. The northern region is primarily affected by strike-slip faulting, where tectonic plates move horizontally, while the south experiences east-west expansion with north-south normal faults. Research utilizing satellite data since the 1970s has uncovered multiple rifts formed between 4 to 8 million years ago.
Significant seismic events in Tibet occasionally reach magnitudes around 8.0 along strike-slip faults. Although normal fault quakes, such as the recent ones, are usually smaller but still impactful, previous tremors in the region have ranged from 5.9 to 7.1 in magnitude since 2008.
This latest seismic activity underscores the persistent tectonic forces that continue to shape Tibet's landscape, emphasizing the need for earthquake preparedness in this vulnerable area.
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