4.3 Article

Cause and Process Mechanism of Rockslide Triggered Flood Event in Rishiganga and Dhauliganga River Valleys, Chamoli, Uttarakhand, India Using Satellite Remote Sensing and in situ Observations

Journal

JOURNAL OF THE INDIAN SOCIETY OF REMOTE SENSING
Volume 49, Issue 5, Pages 1011-1024

Publisher

SPRINGER
DOI: 10.1007/s12524-021-01360-3

Keywords

Rockslide; Flood; Himalaya; Remote sensing; Chamoli Uttarakhand

Funding

  1. Earth Observation and Applications & Disaster Management Support Service Program Office (EDPO)
  2. ISRO Head Quarters
  3. Institute of Seismological Research (ISR), DST, Govt. of Gujarat

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On February 7, 2021, a catastrophic flood occurred in the Chamoli district of Uttarakhand, triggered by a massive rockslide, impacting the catchments of Rishiganga and Dhauliganga valleys, causing significant damage. The rock and ice detached from Trishul mountain range swiftly moved downstream entraining snow, debris, and mud, creating water waves and washing away infrastructure. The event led to the formation of a dammed lake and mud marks reaching up to 80-150 m in height in the valley.
The catchments of Rishiganga and then Dhauliganga valleys in the Chamoli district of Uttarakhand were impacted by a catastrophic flood triggered due to a massive rockslide, caused by wedge failure on 7th February, 2021. It is estimated that the massive rockslide of similar to 23 million cubic meter volume containing base rock, deposited ice, and snow got detached from the northern slopes of the Trishul mountain range near Ronti Glacier and created a vertical fall of almost 1700 m before severely impacting the Ronti Gad valley located at 1.5 km downstream of Ronti Glacier snout. The huge detached mass of rock and ice (GLIMS ID: G079733E30381N) swiftly moved downstream through the glaciated valley entraining snow, debris, mud on its way, caused rapid fluidization, created massive water/slush waves, and washed away partially or completely the hydel power projects and bridges in its route. It is estimated that similar to 0.93 Peta Joules of potential energy led to the generation of a significant amount of kinetic and thermal energy, good enough to trigger above-mentioned processes. Post-event analysis of high-resolution satellite data shows flood water marks in the valley and on the rock outcrops reaching up to similar to 80-150 m height on the way to Raini Village. The mud and the slush produced through this process led to the formation of a dammed lake and temporarily blocked one of the tributaries of the Rishiganga joining from the northeast. This study provides an insight into the sequence of events as they unfolded, through multi-temporal satellite image analysis, aerial survey, seismological data in conjunction with various other geo-spatial and geo-visualization tools for unraveling the flood event that has happened on February 7, 2021. We also discuss the potential cause of rockslide and the process mechanism of this unique event, causing loss of lives and property besides widespread devastation.

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