ice sheets, ice shelves, ice caps, ice streams and outlet glaciers, ice fields, mountain glaciers, valley glaciers, piedmont glaciers, cirque glaciers, hanging glaciers, tidewater glaciers. Figure \(\PageIndex{1}\): Glacier in the Bernese Alps. Continental glaciers are large ice sheets that cover relatively flat ground. These glaciers flow outward from where the greatest amount of snow and ice accumulate. Glacier ice covers about 11 percent of the world’s land area and would cause a world sea-level rise of about 90 metres (300 feet) if all existing ice melted. Continental glaciers are known as ice sheets. Glacier movement occurs in two ways; either retreating or advancing. Mountain glacier: Glaciers formed in the high mountainous regions, and flow out of the icefield. Alpine glaciers form in mountainous areas either at high elevations or near cool and wet coastal areas like the Olympic Peninsula of Washington. The two main types are the Alpine and the Continental glacier, but there are other types too. Alpine glaciers form in mountainous areas either at high elevations or near cool and wet coastal areas like the Olympic Peninsula of Washington. Alpine or valley glaciers flow downhill through mountains along existing valleys. There are 2 main types of glaciers, Continental is one, they float away from central regions. The downhill movement of the glacier causes chopping and remolding of the landscape, which explains the gorgeous landscaping sceneries on mountains. Alpine glaciers The second is alpine or valley which are the glaciers that flow down the valley from the mountain. Glaciers occur in all parts of the world and at almost all latitudes. There are two general types of glaciers – alpine glaciers and ice sheets. TYPES OF GLACIERS There are two main types of glaciers — alpine or valley glaciers, and ice sheets or continental glaciers. List and briefly distinguish among four types of glaciers. A glacier (US: / ˈ ɡ l eɪ ʃ ər / or UK: / ˈ ɡ l æ s i ər, ˈ ɡ l eɪ s i ər /) is a persistent body of dense ice that is constantly moving under its own weight. They are found in Alaska, Arctic, Canada, Andes, and Himalaya. However, these movements of glacier pretty much depend on where the cone-like nose is facing. valley glaciers or continental glaciers (ice sheets) types of glaciers. Sea ice is often mistaken as glacial ice, as for example, the relatively persistent ice that covers the North Pole region. The two types of glaciers include continental and alpine glaciers. Glaciers are mainly classified according to their formation. References; Figure \(\PageIndex{1}\): Glacier in the Bernese Alps. Ice sheets are glaciers that cover large regions and consist of masses of ice that flow out in all directions from one or more snow-accumulation centers. 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