Glacial Lakes - Nepal
Visited October 2009
An emerging climate change driven threat for high-altitude communities is the flash flooding of valleys when glacial dams burst. Accelerated melting of glaciers is expanding their lakes and putting pressure on the earthen damns originally created by the glaciers.
On an expedition in Nepal in October 2009 I saw the effects of one such flooding event and also another glacial lake which is of great concern to local communities.
In 1998, a portion of the Sabai Glacier, a hanging glacier at the head of the Hinku Valley broke off and plunged into the lake below. The lake burst its dam and decimated the valley below - which we trekked up - for tens of kilometres.
At the base of Island Peak, glaciers, such as those coming off Lhotse, have been forming an enormous glacial lake at the rate of 74m of length per annum in recent years. Imja Tsho’s (Island Lake’s) head dam is not strong and if the dam bursts it will likely destroy much of the Khumbu Valley, the ‘tourist highway’ up into the Everest region. This would be a huge disaster for local communities and assumedly the Nepalese economy.