Science
Huge earthquake 2,500 years ago rerouted the Ganges River, study suggests
A huge earthquake that shook southern Asia 2,500 years ago abruptly changed the course of the Ganges River, new research suggests.
The earthquake was previously unknown to Science, but researchers spotted clues of its immense force buried in the landscape near Dhaka, the capital of Bangladesh. The team revealed its findings in a study published Monday (June 17) in the journal Nature Communications. The quake likely reached magnitude 7.5 or 8 and was so powerful it rerouted the main stem of the Ganges — despite the displaced section of river being more than 110 miles (180 kilometers) away from the quake's epicenter.
Rapid river-course changes are called avulsions. Researchers have previously documented avulsions caused by seismic activity, but "I don't think we have ever seen such a big one anywhere," study co-author Michael Steckler, a geophysicist and research professor at the Lamont-Doherty Earth Observatory of the Columbia Climate School in New York, said in a statement.
The Ganges is one of the largest rivers in the world, flowing for about 1,600 miles (2,500 km). It starts in the Himalayas, on the border between India and China, and then flows east through India to Bangladesh, where it merges with other major rivers, including the Brahmaputra and the Meghna. The combined waterways fan out to form the largest river delta on Earth and empty out into the Bay of Bengal.
Related: Why do earthquakes happen far away from plate boundaries?
Like other rivers that flow through big deltas, the Ganges can change its own course — without help from an earthquake — by carrying sediments that gradually accumulate on the riverbed. Eventually, enough sediment builds up in one spot to grow taller than the surrounding landscape, at which point the river spills over and carves out a new path for itself.
While this process occurs over several years or decades, an earthquake could potentially reroute a river more or less instantaneously, Steckler said.
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