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Continental glaciers and valley glaciers are both types of glaciers that form from accumulated snowfall. They both flow under the influence of gravity, albeit in different directions. While continental glaciers cover vast areas like an ice sheet, valley glaciers are confined to mountain valleys and flow down through them.
There are 2 main types of glaciers, Continental is one, they float away from central regions. The second is alpine or valley which are the glaciers that flow down the valley from the mountain.
Yosemite Valley is a California geologic feature that formed as a result of erosion by glaciers. The glaciers carved out the U-shaped valley, leaving behind steep granite walls and beautiful waterfalls. Other examples include the glacially-carved cirques and hanging valleys in the Sierra Nevada mountain range.
Valley glaciers are formed in high altitudes (e.g. mountains) and continental glaciers are formed in high latitudes (e.g. Greenland). Therefore, they both cover land areas but continental glaciers generally cover more area.
Glaciers are the main agents of erosion that create U-shaped valleys. As glaciers move downhill, they carve out the valley floor and sides through the process of abrasion and plucking. The unique U-shape is a characteristic feature of valleys that have been shaped by glaciers.
Valley glaciers are not associated with being found on the coastal regions. They are typically found in mountainous areas and their movement is influenced by gravity and topography.
Continental glaciers are thicker and larger. Valley glaciers are formed on mountains; continental glaciers are formed on flat land.
valley glaciers
It is valley and continental glaciers they are different because continental glaciers are the largest, and valley glaciers are on the top of mountain peaks.
Continental glaciers and valley glaciers are both types of glaciers that form from accumulated snowfall. They both flow under the influence of gravity, albeit in different directions. While continental glaciers cover vast areas like an ice sheet, valley glaciers are confined to mountain valleys and flow down through them.
There are 2 main types of glaciers, Continental is one, they float away from central regions. The second is alpine or valley which are the glaciers that flow down the valley from the mountain.
No. Valley glaciers are a few miles to a few tens of miles long. Continental glaciers are hundreds to thousands of miles long.
Valleys are formed by glaciers through a process called glacial erosion. As glaciers move, they pick up rocks and debris, which act as tools to scrape and carve the underlying bedrock. Over time, this erosion deepens and widens the valley, creating the distinctive U-shape commonly associated with glacial valleys.
Two kinds of glaciers are valley glaciers and ice sheets. Valley glaciers are long, narrow glaciers that form in mountain valleys, while ice sheets are vast, continent-sized glaciers that cover large land areas. The main difference is in their size and location, with valley glaciers typically being smaller and found in mountainous regions, while ice sheets are much larger and exist in polar regions.
Continental and Valley Glaciers.
its not mountain glaciers but its valley glaciers
valley glaciers