Search results
Results from the WOW.Com Content Network
Lake Tekapo, New Zealand. A moraine-dammed lake, occurs when the terminal moraine has prevented some meltwater from leaving the valley. When a glacier retreats, there is a space left over between the retreating glacier and the piece that stayed intact which holds leftover debris . Meltwater from both glaciers seep into this space creating a ...
Lake Algonquin is an example of a proglacial lake that existed in east-central North America at the time of the last ice age. Parts of the former lake are now Lake Huron, Georgian Bay, Lake Superior, Lake Michigan and inland portions of northern Michigan. [1] Examples in Great Britain include Lake Lapworth, Lake Harrison and Lake Pickering.
Moraine-dammed lakes occur when glacial debris dam a stream (or snow runoff). Jackson Lake and Jenny Lake in Grand Teton National Park are examples of moraine-dammed lakes, though Jackson Lake is enhanced by a man-made dam. Kettle lake: Depression, formed by a block of ice separated from the main glacier, in which the lake forms; Tarn: A lake ...
Moraine-dammed lake – Type of lake formed by glaciation; Terminal moraine – Type of moraine that forms at the terminal of a glacier; Rogen moraine – Landform of ridges deposited by a glacier or ice sheet transverse to ice flow; Kame; Moraine examples. Dogger Bank – Large sandbank in the North Sea; Kettle Moraine – Large moraine in ...
South Lhonak Lake is a glacial-moraine-dammed lake, located in Sikkim's far northwestern region. [2] It is one of the fastest expanding lakes in the Sikkim Himalaya region, and one of the 14 potentially dangerous lakes susceptible to Glacial lake outburst flood (GLOFs).
The 21-square-kilometre (8.1 sq mi) lake would have been part of the saltwater Larviksfjorden, had it not been dammed by an end moraine left by the latest ice age. That moraine is about 1 kilometre (0.62 mi) wide, separating the lake from the sea. There is a short river that runs through the moraine which drains the lake into the fjord. The ...
[12] [16] Studies show that moraine-dammed lakes, which are attributed to the melting of snowcaps and increased rainfall, are also giving rise to lake outbursts and subsequent flash flooding. [citation needed] The Mandakini region is seismically and ecologically fragile due to its position along a collision zone.
Below the glacier, water had been accumulating, dammed back by the moraine, and formed a lake some 250 m (820 ft) long and 150 m (492 ft) wide. Its depth was 15 to 20 m (49 to 66 ft), depending on the time of year. [2] The water in the lake mostly accumulated from rainfall and melting snow in its catchment area.