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Glacial Tectonic Interaction
Context: A change in the course of the Himalayan glacier has been observed by a group of scientists from Wadia Institute of Himalayan Geology, Dehradun which is an autonomous institute under the Department of Science and Technology, Government of India.
Important Observations:
This is for the first time that an abrupt change has occurred in the Himalayan glacier and the scientists believe that this is a consequence of climate and tectonics. The observation was made in the upper Kali Ganga valley in the Pithoragarh district of Uttarakhand.
The change in the course of the glacier is associated with the disaster that took place in Rishiganga.
The rock mass on which the glacier was placed became fragile because of weathering, percolation of meltwater in joints and cracks, freezing, thawing, snowfall, overloading. All these contribute to the mechanical disintegration of the glacier from the source rock.
Therefore the scientists found that the northeast moving glacier abruptly changed the direction towards the southeast due to climatic factors and tectonics.
The active fault on the glacier was confirmed by remote sensing and an old survey map.
Significance:
This study helps in understanding the factors that result in disastrous events in the Himalayan region.
It is inferred that not only the climatic factors but the glacial-tectonic interactions play a significant role in the evolution of new landforms.
A clear idea about the unique behaviour of glaciers has been offered by the study which can be essential in future studies related to glacial events and Himalayan disasters.
What is Glacitectonics?
The deformation involving folding and thrusting caused by a glacier or ice-sheet that forces into the existing sedimentary bedrock is known as Glacitectonics.
This phenomenon results in the dynamic nature of glaciers and ice sheets leading to their advancement, retreat, folding and faulting.

(a) Depicts past scenario and (b) depicts the present scenario – Image source: PIB
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