A cirque is the top of a glacier valley.
Glaciers that create cirques on the sides of mountains are called cirque glaciers. These glaciers form in bowl-shaped depressions on the slopes of mountains and are responsible for eroding and shaping the characteristic amphitheater-like features known as cirques. Examples of cirque glaciers can be found in mountain ranges around the world, such as the Alps, Andes, and Himalayas.
valley glaciers
Cirques are the rounded basins carved into the sides of mountains by valley glaciers. They are typically characterized by steep walls and a bowl-like shape. The process of glacial erosion forming cirques is known as plucking and abrasion.
Glaciers grind into mountains by eroding the cirques at their heads. If a mountain has cirques all around it, it is called a horn
True. Glaciers erode the base of mountains into basins called cirques through a process known as glacial erosion. This results in the formation of amphitheater-like depressions at the base of mountains.
Moraine
Cirques are formed
valley glaciers
Steep-sided, half-bowl shaped recesses carved into mountains at the heads of glacial valleys. The Fjords: Steep cliffs, acting as ocean inlets. Horn peaks: Where cirques intersect. Terminal moraines: Piles of rocks. Crevasses: Cracks in glaciers
A cirque is a bowl-shaped, steep-sided glacier-carved valley found high in the mountains. It is formed by the erosive action of a glacier as it moves downhill, carving out the landscape. Cirques often contain small lakes called tarns.
When three or more cirques erode into a mountain summit, they form a horn. This distinctive landform is characterized by steep, sharp peaks, often seen in famous mountains like the Matterhorn in the Swiss Alps.
Waterfalls on the sides of mountains reveal much about hydrology.