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.