Cirque Glacier, also called corrie glacier, is a type of glacier that forms in a bowl-like depression on the side of a mountain. There are several synonyms for this term, including mountain glacier, valley glacier, and alpine glacier. Mollier Glacier and Neve Glacier are also types of cirque glaciers. These glaciers are characterized by their steep sides, often found in areas with high snowfall, and can be found in many regions of the world, including the Alps, Rocky Mountains, and Himalayas. These glaciers are important indicators of climate change, as their melting can contribute to rising sea levels and affect ecosystems downstream.