There are two primary types of glaciers: Continental: Ice sheets are dome-shaped glaciers that flow away from a central region and are largely unaffected by underlying topography (e.g., Greenland and Antarctic ice sheets); Alpine or valley: glaciers in mountains that flow down valleys. From their high elevation origins, alpine and cirque glaciers may flow into ice falls or valley glaciers, or they may terminate in the mountains. Glaciers are located all around the world but behave similarly no matter where they are- from the Andes to the Alps, Greenland to Africa, glaciers move and grow in the same circumstances and leave the same results behind. Differences: Location; Alpine glaciers are only found on mountain tops but continental glaciers are only found at the earth's poles regardless of elevation. If a mountain glacier increases in size and begins to flow down the valley, it is then described as a valley glacier. Glaciers that flow out of ice sheets, icefields or ice caps are called outlet glaciers. The other major glacier type is ice sheets (also called continental … If a mountain glacier increases in size and begins to flow down the valley, it is then described as a valley glacier. Types of glaciers. alpine glacier. They are called "cirque glaciers" if they originate in small bowls with steep headwalls (cirques). There are two general types of glaciers – alpine glaciers and ice sheets. The glacial erosional and depositional features visible on the surface of the Earth today serve as proof of the above fact. Valley. Small alpine and cirque glaciers can sometimes be found nestled beneath the highest peaks in Parks in the western contiguous United States today. Snowflakes are the hexagonal water crystals. How do they form? Continental Glaciers. Alpine Glaciers. There are two primary types of glaciers: Continental: Ice sheets are dome-shaped glaciers that flow away from a central region and are largely unaffected by underlying topography (e.g., Greenland and Antarctic ice sheets); Alpine or valley: glaciers in mountains that flow down valleys. glacier which occupies the lowland at a mountain front. Latitude, topography, and global and regional climate patterns are important controls on the distribution and size of these glaciers. Glaciers that flow out of ice sheets, icefields or ice caps are called outlet glaciers. Alpine glaciers are further classified by their shape as well as the surface they flow onto. Valley glaciers are common in the mountain ranges of the United States and Canada. (ie: Greenland) An alpine glacier are typically found in high altitudes (ie: mountain valleys) Differences? Other factors that affect the velocity of a glacier include the roughness of the rock surface (friction), the amount of meltwater, and the weight of the glacier. The two main types of glaciers are alpine glaciers and continental glaciers. Terms in this set (9) Cirque. This is a list of glaciers existing in the United States, currently or in recent centuries.These glaciers are located in nine states, all in the Rocky Mountains or farther west. The other category is continental glaciers, also known as ice sheets. The flow of outlet glaciers is affected by the landscape, travelling through valleys and exposed rock. The other major glacier type is ice sheets (also called continental … Continental glaciers are also known as ice sheets because their form and flow are not significantly affected by underlying geographic formations. glacier which occupies a mountain valley. Similarities Features of Alpine Piedmont glaciers are the forwardmost extension of valley glaciers and form where the ice emerges at the front of the mountain range. NOAA Hurricane Forecast Maps Are Often Misinterpreted — Here's How to Read Them. There are several types of glaciers that fall into two main categories. glacier which occupies a mountain valley. The two main types of glaciers are continental glaciers and alpine glaciers. The majority of alpine glaciation is the result of the repeated advance and retreat of valley glaciers. Glaciers are constantly moving due to their own weight, and this movement over land creates landforms over many centuries, moving very slowly. A cirque is a bowl-shaped hollow found high up on the side of a mountain. Alpine glaciers form in mountainous areas either at high elevations or near cool and wet coastal areas like the Olympic Peninsula of Washington. 17.1 Types of Glaciers There are two main types of glaciers: continental glaciers and alpine glaciers. Continental glaciers can also be divided into ice sheets and ice fields. reservoir (besides the oceans) which holds the greatest amount of water. Most alpine glaciers are located in the major mountain ranges of the world such as the Andes, Rockies, Alps, and Himalayas. At the time that this digital image was made, the glacier's terminus was blocking the entrance to Russell Fiord. This is a list of glaciers existing in the United States, currently or in recent centuries.These glaciers are located in nine states, all in the Rocky Mountains or farther west. Although the uppermost layer of a glacier is brittle, the ice beneath behaves as a plastic substance that flows slowly (Figure 17.6). 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