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Backpackers cross a massive sheet of naled in Alaska.Smaller sheets of naled-like ice form when a river overflows, the top layer of the floodwater freezes, and then the floodwater recedes.
A sheet-like layered mass of ice formed in freezing temperatures from the freezing of successive flows of ground water over previously formed layers of ice.
1978, Frederick J. Sanger, Peter J. Hyde, Permafrost: Second International Conference, July 13-28, 1973 : USSR Contribution, National Academies, →ISBN, page 392:
The geographic distribution of naleds in Trans-Baikal does not confirm the view of certain researchers to the effect that naleds are typical only of the regions where permafrost occurs.
