Glacial Lake Iroquois was a prehistoric proglacial lake that existed at the end of the last ice age approximately 13,000 years ago. The lake was essentially an enlargement of the present Lake Ontario that formed because the St. Lawrence River downstream from the lake was blocked by the ice sheet near the present Thousand Islands.The level of the lake was approximately 30 m …

Lake Agassiz was a large glacial lake in central North America.Fed by glacial meltwater at the end of the last glacial period, its area was larger than all of the modern Great Lakes combined.. First postulated in 1823 by William H. Keating, it was named by Warren Upham in 1879 after Louis Agassiz, when Upham recognized that the lake was formed by glacial action.

The Last Glacial Period (LGP), also known colloquially as the last ice age or simply ice age, occurred from the end of the Eemian to the end of the Younger Dryas, encompassing the period c. 115,000 – c. 11,700 years ago. The LGP is part of a larger sequence of glacial and interglacial periods known as the Quaternary glaciation which started around 2,588,000 years ago and is …

Lake Missoula was a prehistoric proglacial lake in western Montana that existed periodically at the end of the last ice age between 15,000 and 13,000 years ago. 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.. The Glacial Lake Missoula National Natural …

A glacial lake outburst flood (GLOF) is a type of outburst flood caused by the failure of a dam containing a glacial lake.An event similar to a GLOF, where a body of water contained by a glacier melts or overflows the glacier, is called a jökulhlaup.The dam can consist of glacier ice or a terminal moraine.Failure can happen due to erosion, a buildup of water pressure, an avalanche …

Lake Louise (named Ho-run-num-nay (Lake of the Little Fishes) by the Stoney Nakota First Nations people) is a glacial lake within Banff National Park in Alberta, Canada.It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway ().. Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen …

Lake Minnewanka (/ ˌ m ɪ n ə ˈ w ɑː ŋ k ə /) ("Water of the Spirits" in Nakoda) is a glacial lake located in the eastern area of Banff National Park in Canada, about five kilometres (3.1 miles) northeast of the Banff townsite. The lake is 21 km (13 mi) long and 142 m (466 ft) deep, making it the 2nd longest lake in the mountain parks of the Canadian Rockies (the result of a power dam ...

Hydrography. Okanagan Lake is called a fjord lake as it has been carved out by repeated glaciations. Although the lake contains numerous lacustrine terraces, it is not uncommon for the lake to be 100 metres (328 ft) deep only 10 metres (11 yd) offshore. Major inflows include Mission, Vernon, Trout, Penticton, Equesis, Kelowna, Peachland and Powers Creeks.

Ganoga Lake is a natural spring-fed lake just west of Pennsylvania Route 487 in southern Colley Township in southeastern Sullivan County, Pennsylvania. It is near the meeting point of Sullivan, Columbia and Luzerne counties, and is less than 0.4 miles (0.6 km) northwest of Ricketts Glen State Park. Ganoga Lake is on the Allegheny Plateau at an elevation of 2,260 feet (690 m).

The word is derived from the Old Norse word tjörn ("a small mountain lake without tributaries") meaning pond. In parts of Northern England - predominantly Cumbria but also areas of North Lancashire and North Yorkshire - 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn).