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A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased ...
Talkin Tarn is a glacial lake and country park near Brampton, Cumbria, England. [1] The lake is in a kettle hole , formed 10,000 years ago by mass glacial action. [ 2 ] Situated just 20 minutes from Carlisle by road, or a short train journey via Brampton Junction , this is a popular venue for families and local people.
Lake Nipissing; 8,400 – 5,500 YBP formed as the water bodies in the Superior and Huron basins merged across Sault Ste. Marie around 8,400 YBP and then merged with the Michigan basin around 7,800. [1] Lake Stanley-Hough; 8,700 YBP, the water levels had risen to connect both Lake Stanley and Lake Hough into a single body of water. [1]
Lake Matheson formed between two moraine terraces left by the rapid retreat of Fox Glacier / Te Moeka o Tuawe 14,000 years ago, at the end of the last glacial period. The retreating glacier left behind a valley and a huge slab of ice insulated by a deep layer of moraine gravel, which gradually melted and collapsed to form the lake bed. [ 1 ]
The glacial origin of the Kettle Mucubají is evident because of the visible footprint left by the Mucubají ravine tens of thousands of years ago. This ravine was created by the action of a receding glacier, which was also sealed by an accumulation of unconsolidated glacial debris created by the lake. [1]
Lake Kankakee was a prehistoric lake during the Wisconsin glacial epoch of the Pleistocene Era. The lake formed during the period, when the Michigan and Saginaw lobes of the Laurentian glacier had receded back to the Valparaiso and Kalamazoo moraines. While the glacial advance became stagnant, the summer runoff formed a large lake covered parts ...
Years of heavy rainfall and snowmelt call forth the ghost of the lake, however, haunting the residents with damaging floodwaters. This happened in 1983 and 1997 -- both years that experienced very ...
Lake Maumee was a proglacial lake and an ancestor of present-day Lake Erie. It formed about 17,500 calendar years, or 14,000 Radiocarbon Years Before Present (RCYBP) as the Huron-Erie Lobe of the Laurentide Ice Sheet retreated at the end of the Wisconsin glaciation .