The accumulated influence of Climatic and tectonics have led to abrupt change in the main course of Himalayan Glacier, revealed a study conducted by Indian scientists.

A team of scientists from Wadia Institute of Himalayan Geology (WIHG) had studied an unnamed glacier in one of the less explored regions in the upper Kali Ganga valley (Uttarakhand) and found that the glacier had abruptly changed its main course.

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“It is for the first time that such change in course has been reported from a Himalayan glacier, and the researchers have attributed this to the accumulated influence of both climate and tectonics,” said a senior officer of the Ministry of Science and Technology.

“The abnormal behaviour of this unnamed glacier clearly suggests that not only is climate a controlling factor, but tectonics also plays an important role in glacial catchments,” the Scientists said in its study report.

“The recent disaster in Rishiganga is a latest example which suggests that the rock mass on which the glacier was sitting gradually became fragile (due to weathering, percolation of meltwater in joints, crevasses, freezing and thawing, snowfall, overloading, and gradually operating tectonic forces forcing rocks to mechanical disintegration) with due course of time and detached from the source rock,” the study stated.

It clearly suggests that the Himalaya is an active mountain range and highly fragile where tectonics and climate play a critical role, the scientists claimed. The WIHG (an autonomous institute under the Department of Science & Technology) scientists also found that the unnamed NE moving glacier had been abruptly truncated and forced to move towards SE.

Based on remote sensing and an old survey map, the study assessed that the glacier had been affected by active fault and climate change. Tectonic activity and change in climatic conditions had changed the course and morphology of this glacier, the Ministry said.

“An active fault produced a fault scarp that measures about 250 m in height with a northerly dip. The fault trace is 6.2 km in length and trends towards NW-SE,” the WIHG team observed.

The WIHG team also found that the 5 km long unnamed glacier, which covered around 4 km² area in Kuthi Yankti valley (Tributary of Kali River), has abruptly changed its main course.

It moved, truncated, and ultimately merged with the adjacent glacier named Sumzurkchanki as a result of tectonic forcing during the time between Last Glacial Maxima (19-24 ka) and Holocene. It is one of the unique behaviours of the glacier, and no such observation has so far been reported on this type of glacier kinematics, the Study claimed.

The study further indicated that climate is not the only factor that triggers disasters in the Himalaya, which is an active mountain range, but tectonics also plays an important role in glacial catchments.

The study would open doors for a new approach in glacier studies, particularly focused on the course change and evolution of new landforms formed by glacial-tectonic interplay.