A small lake in a cirque is called a tarn. This type of lake forms in a glacial cirque, which is a bowl-shaped depression carved out by a glacier. Tarns are often found at the base of a cirque or in the floor of the depression.
A ' Tarn' is a mountain lake or pool formed in a cirque excavated by a glacier.
A tarn (or corrie loch) is a mountain lake or pool, formed in a cirque excavated by a glacier.
Cirque erosion results in the formation of bowl-shaped depressions at the head of a valley glacier. Deposition can occur when the glacier melts, depositing sediment and creating a small lake called a tarn in the cirque basin.
a cirque is a steep-walled semicircular basin in a mountain (carved by a glacier)
A cliff, a mountain, a ravine, a gorge, glacial valley, an arête, a cirque, a tarn. an escarpment are some possibilities.
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 small, steep-banked mountain lake, formed when a glacier advancing down a slope scoops material out of the ground in a "cirque" at the base of the slope. (Essentially, it continues downward into the ground before moving horizontally again.) When the glacier melts, the depression can fill with water, and is refilled by melting snow unless it becomes filled by silt.
Michael Tarn is 5' 8".
Tan Tarn How was born in 1960.
Gary Tarn was born in 1962.
Nathaniel Tarn was born in 1928.