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A Cirque
A tarn (or corrie loch) is a mountain lake or pool, formed in a cirque excavated by a glacier.
a cirque is a steep-walled semicircular basin in a mountain (carved by a glacier)
A deep and steep bowl-like depression produced by glacier erosion is called a cirque. The word "cirque" is a French word for "arena". A cirque is also known as a corrie.
A glacial cirque is formed when a glacier erodes the headwall of a valley through processes like plucking and abrasion. As the glacier moves downhill, it creates a bowl-shaped depression with steep walls. After the glacier retreats, the cirque may fill with water, forming a tarn or glacial lake.
A ' Tarn' is a mountain lake or pool formed in a cirque excavated by a glacier.
A cirque is a glacial landform that resembles an armchair. It is a bowl-shaped hollow with steep sides formed at the head of a glacier where ice erosion and plucking have occurred.
Emmons Glacier is the largest glacier on Mount Rainier and is located within a cirque, which is a bowl-shaped hollow at the head of a valley. This cirque, known as Emmons Cirque, was carved out by glacial activity over thousands of years.
What can happen when the glacier melts in a cirque
What can happen when the glacier melts in a cirque
In cross-section: A 'U' shaped valley is formed from glacial erosion. A 'V' shaped valley is formed by river erosion.
The Cirque is the name given to the bowl shaped depression were the valley glaciers usually begins. A glacier basically refers to a terminus that usually ends in a body of water.