тЬЕ A glacial lake is a body of water with origins from glacier activity.
тЬЕ They are formed when a glacier erodes the land, and then melts, filling the depression created by the glacier.
реж Formation
тЬЕ Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat.
тЬЕ A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills.
тЬЕ As the ice age ended, these melted to create lakes.
тЬЕ These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks.
тЬЕ The moraine creates topographic depression in which the melt water is generally accumulated leading to formation of glacial lake.
тЬЕ When this lake is watertight, melt waters will accumulate in the basin until seepage or overflow limits the lake level.
тЬЕ Such moraine-dammed lakes appear to be the most common type of glacial lakes.
тЬЕ The impoundment of the melt may sometimes be unstable, leading to sudden release of large quantities of stored water.
тЬЕ Failure of these ice or moraine dams leading to disastrous destruction events has been documented throughout the world.
тЬЕ Flash floods caused by the outburst of glacial lakes, called as Glacial Lake Outburst Flood (GLOF), are well known in Himalaya where such lakes had often been formed by landslides.
тЬЕ The formation and characteristics of glacial lakes vary between location and can be classified into
тЧ╝я╕П glacial erosion lake,
тЧ╝я╕П ice-blocked lake,
тЧ╝я╕Пmoraine-dammed lake,
тЧ╝я╕Пother glacial lake,
тЧ╝я╕Пsupraglacial lake, and
тЧ╝я╕Пsubglacial lake.
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