Glaciers that become unstable and experience exceptionally high
advance rates are called surging glaciers. Sometimes their surge
history gets "stored" in so-called looped moraines. Here, the
glacier in the middle shows deformed ("looped") moraines, in
contrast to the "straight" moraines in the glacier to the left.
These loops appeared when distinct surges in the tributary glacier
(lower left in image) pushing into the main glacier deformed and
transported its ice and debris cover, thereby storing the surge
history. If a glacier surge leads to a rapid advance of the
affected glacier, it may override and dam rivers too quickly to
allow for slow drainage of the dammed river. A dangerous lake can
develop and a corresponding flood hazard threaten people and
infrastructure down-valley.