Collapse of rock mass may have caused Uttarakhand flash floods
What's the story
Initial observations by scientists of the Wadia Institute of Himalayan Geology (WIHG) suggest that a rock mass weakened over a period of time due to freezing and thawing of snow and led to the creation of a weak zone, triggering its collapse. This resulted in the formation of a temporary dam that eventually breached, causing the deadly floods in Uttarakhand's Chamoli district on Sunday.
Glaciers
Avalanche supposedly happened in the wee hours of Sunday
Kalachand Sain, Director of the WIHG, said the incident occurred adjacent to the Raunthi glacier. The area also has glaciers that feed the Rishi Ganga river, which ultimately joins the Dhauli Ganga. Sain said the avalanche must have taken place in the wee hours of Sunday while the temporary dam must have breached between 10-11 am.
Details
Two teams of glaciologists conducted a helicopter survey
Two teams comprising five glaciologists of the WIHG, an institute that studies the Himalayan environment and its geology, are at the site conducting observations. The teams carried out a helicopter survey of the area on Tuesday to find clues as to what led to the massive flash floods that swept everything on the way. So far, the flash floods have claimed 31 lives.
Observations
Area had witnessed precipitation in the preceding three days
Sain said, "Our observations suggest that the rock mass may have weakened due to freezing and thawing over a period of time. This sometimes leads to the development of a weak zone and fractures." The area also witnessed precipitation in the preceding three days, followed by clear weather on the day of the event, which caused a freezing and thawing effect.
Background
Huge rock and glacial ice masses moved down the valley
Sain said, "The event occurred due to a slide of a large rock mass beneath the hanging glacier at 5,600 meters above sea level." "It was observed that a huge rock and glacial ice masses collectively moved rapidly down the valley, taking away along with them all the snow and other loose material coming in their way," he added.
Fact
Steep slopes made the rock-and-snow avalanche worse
The steep slopes of the mountains in the region further increased the intensity of the crash. The stretch of the avalanche was about three kilometers with an average slope of 37 degrees, before reaching the Raunthi Nala/Gadhera floor at an altitude of about 3,600 meters. Thus, the rock-and-snow avalanche was able to entrain a vast amount of water and sediment.
Information
A supposed temporary water impoundment eventually breached
Sain said, "It seems that the materials blocked the water to the Raunthi Nala stream, causing a temporary water impoundment. The impounded water was eventually breached, which might have caused the catastrophic flash floods." Sain said that an initial report will be sent to the Department of Science and Technology (DST).