Greenland and Antarctica are almost entirely covered with ice sheets that are up to 3500 m (11 500 ft) thick. Glaciers are usually divided into two groups – alpine glaciers, which form on mountain sides and more downward through valleys; and continental ice sheets, which spread out and cover large areas. Ask your question. The glaciers on the mountain slope that end in the middle before approaching the main river are known as mountain glaciers. There are two types of glaciers, continental and alpine. Ice flowing downslope follows the original topography and seeks the steepest path, similar to flowing water. There are two general types of glaciers: mountain glaciers and continental glaciers. Secondary School. In the case of continental ice sheets however, such as those found in Greenland and Antarctica, they radiate out from the areas of thicker inland ice to the thinner coastal ice, eventually breaking off (calving) into the ocean and becoming large icebergs. There are ice caps in Iceland and huge ice sheets in Greenland and Antarctica. They are also known as valley glaciers, and as you know are found on mountain tops above the snow line. For information about other types, see the articles ice and glacier.
A large body of glacial ice astride a mountain, mountain range, or volcano is termed an ice cap or ice field. 1. Geography. Introduction. Read More Glaciers are categorized by their morphology, thermal characteristics, and behavior. Glacial change. Valley glaciers cover much of a continent, while continental glaciers cover a small area of mountains. Glaciers also deposit sediments in characteristic landforms. Most alpine glaciers are located in the major mountain ranges of the world such as the Andes, Rockies, Alps, and Himalayas. Those ice masses are not necessarily associated with mountains. Glaciers. The accumulation zone begins in a bowl-shaped cirque, eventually it spills outs and flows downwards. Those ice masses are not necessarily associated with mountains. Glacier - Glacier - Mountain glaciers: In this discussion the term mountain glaciers includes all perennial ice masses other than the Antarctic and Greenland ice sheets. Join now. Introduction. Continental glaciers can also be divided into ice sheets and ice fields. They sculpt mountains, carve valleys, and move vast quantities of rock and sediment. Glaciers and Glacial Landforms. These are thick accumulations of ice that occupy a large geographical area.
ADVERTISEMENTS: Difference between Continental Glacier and Mountain Glacier are: Related posts: Short essay on the Definition of a glacier Short essay on the Rate of glacier movement What is the Characteristic Feature of Glaciers? Continental glaciers flow in all directions as they move, while valley glaciers move down slopes already cut by rivers. 5 points Difference between Continental glaciers and mountain Glaciers Ask for details ; Follow Report by … There are two types of glaciers, continental and alpine. Of the two main categories of glaciers, alpine glaciers are the most recognizable and well-known, and as far as the vast majority of casual observers concerned, the only type of glacier in existence. Alpine glaciers form on mountains and flow down mountain valleys. Continental glaciers cover large swaths of land and extend over 50,000 km, meanwhile valley glaciers are confined to mountains and don't exceed lengths of 100 km. Continental glaciers are continuous masses of ice that are much larger than alpine glaciers. Log in. Continental glaciers are also far thicker, they bury the land in up to thousands of meters of ice, completely transforming the landscape.