Retreating valley glaciers often leave behind glacier lakes in front of or
within their melting tongues. Nearly all glaciers in this image of the Bhutan
Himalayas show lakes at their tongues. Once such a lake has formed, melting and
retreat of the glacier front accelerates because water transports heat much
more efficiently to the ice front than air can. The Bhutan Himalayas currently
host more than 2,500 glacier lakes. On October 7, 1994, the greenish lake to
the right in this image, Lugge Tsho, partially burst out. Though the impact in
this lightly populated area was minimal—12 houses were damaged, five water
mills washed away, and about 800 acres of land damaged—traces of the
subsequent debris flow down the valley remain visible seven years later in this
2001 image. The glacier tongue seen in the middle of the image, between the
blue and green lakes, shows clearly how small ponds forming on a melting
glacier tongue can rapidly grow and connect with one another to form large,
potentially hazardous lakes.