Himalayan hard rocks may up flood risk: Study

Himalayan hard rocks may up flood risk: Study
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Highlights

Earthquakes and landslides in the Himalayas - that lead to large volume of hard rocks being dumped into rivers - can increase flood risk up to hundreds of kilometres downstream, potentially affecting millions of people in India and neighbouring countries, a new study warns. 

​London: Earthquakes and landslides in the Himalayas - that lead to large volume of hard rocks being dumped into rivers - can increase flood risk up to hundreds of kilometres downstream, potentially affecting millions of people in India and neighbouring countries, a new study warns.

The findings could help researchers improve flood risk maps for the Ganga Plain, a low-lying region covering parts of India, Nepal and Pakistan - one of Earth's most densely populated areas.

The study, by researchers at the University of Edinburgh in the UK could also provide fresh insight into the long-term impacts of earthquakes and storms in the region. Until now, little was known about how landslides in the Himalaya may affect flood risk downstream on the Ganga Plain.

For the first time, scientists have traced the path of rocks washed down from the Himalayan mountains onto the Plain.

They found that large landslides in the southern, lower elevation ranges of the Himalaya are more likely to increase flood risk than those in the high mountains further north.

Rocks in the south are extremely hard and travel only a short distance - less than 20 kilometres - to reach the Plain. This means much of this rock - such as quartzite - reaches the Plain as gravel or pebbles, which can build up in rivers, altering the natural path of the water, the team says.

Rocks from more northerly regions of the Himalaya tend to be softer, and the team found they often travel at least 100 km to reach the Plain.

These types of rock - including limestone and gneiss - are gradually broken down into sand which, unlike gravel and pebbles, is dispersed widely as it travels downstream.

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