After the 2005 earthquake in Pakistan, studies indicated that the Himalayas rose by about 2 to 3 meters in certain areas. This uplift was a result of tectonic movements associated with the collision of the Indian and Eurasian plates. The earthquake’s magnitude and the resulting stress on the Earth's crust contributed to this geological change. Overall, the uplift is part of the ongoing geological processes in this seismically active region.
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