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A flood caused by a glacial lake outburst flood on 13 December 1941 killed an estimated 1,800 people along its path in Peru, including many in the town of Huaraz. The cause was a block of ice that fell from a glacier in the Cordillera Blanca mountains into Lake Palcacocha. This event has been described as a historic inspiration for research ...
Alt, David (2001) Glacial Lake Missoula and Its Humongous Floods (Mountain Press, 2001. ISBN 978-0878424153). Norman B. Smyers and Roy M. Breckenridge (2003). "Glacial Lake Missoula, Clark Fork ice dam, and the floods outburst area: Northern Idaho and western Montana". In T. W. Swanson (ed.). Western Cordillera and adjacent areas. Geological ...
The lake measured about 7,770 square kilometres (3,000 sq mi) and contained about 2,100 cubic kilometres (500 cu mi) of water, half the volume of Lake Michigan. [1] The Glacial Lake Missoula National Natural Landmark is located about 110 kilometers (68 mi) northwest of Missoula, Montana, at the north end of the Camas Prairie Valley, just east ...
A 2020 glacial lake outburst flood in British Columbia, Canada, caused a tsunami of water about 330 feet (100 meters) high, but no one was hurt. A 2017 glacial outburst flood in Nepal, ...
More than 100 people are missing in India’s northeast after heavy rain caused a glacial lake to burst, leading to flash floods which ripped through the Himalayan state of Sikkim Wednesday ...
In geomorphology, an outburst flood—a type of megaflood—is a high-magnitude, low-frequency catastrophic flood involving the sudden release of a large quantity of water. [1] [2] During the last deglaciation, numerous glacial lake outburst floods were caused by the collapse of either ice sheets or glaciers that formed the dams of proglacial ...
The flooding began on Monday night after water spilled out from the glacial lake at Suicide Basin, which annually fills with rainwater and meltwater and is usually dammed by the retreating ...
Lake Agassiz (/ ˈ æ ɡ ə s i / AG-ə-see) was a large proglacial lake that existed in central North America during the late Pleistocene, fed by meltwater from the retreating Laurentide Ice Sheet at the end of the last glacial period.