Scientists have found that the Himalayas are not uniform and assume different physical and mechcal properties in different directions - a property present in crystals called sotropy which could result in significantly large earthquake events in the Himalayas.
The northwestern region of India, an area covering Garhwal and Himachal Pradesh, has been hit by four destructive moderate to great earthquakes since the beginning of the 20th century -- the Kangra earthquake of 1905, the Kinnaur earthquake of 1975, the Uttarkashi earthquake of 1991, and the Chamoli earthquake of 1999.
A Science and Technology Ministry release said that these seismic activities mfest large-scale subsurface deformation and weak zones, underlining the need for deeper insights into the ongoing deformation beneath these tectonically unstable zones.
Researchers from Wadia Institute of Himalayan Geology (WIHG), Dehradun and the Indian Institute of Technology Kharagpur used the data from WIHG to show that the northwest Himalayan region exhibits a peculiar characteristic present in crystals.
The release said the joint study using seismic waves from 167 earthquakes recorded by 20 broadband seismic stations deployed in the Western Himalaya suggested that the major contribution of the sotropy is mainly because the strain induced by the Indo-Eurasia collision (going on since 50 million years) and deformation due to the collision is found to be larger in the crust than in the upper mantle.
It has been recently published in 2020 in the Journal 'Lithosphere (GSA)', the release said.
"The inhomogeneity along the Himalayas influences the stressing rate because of variation in the geometry of the Main Himalayan Thrust (MHT) system, and it controls the rupture size during the earthquake," the release said.
It said this lack of homogenous physical and mechcal properties of the Himalayas could help explore new perspectives about deformations taking place at the Himalaya-Tibet crustal belt involved in the formation of the Himalayan mountains.
( With inputs from ANI )
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