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.