Gravity, mostly. The great weight of the ice moves slowly down the valley.
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.
Deglaciation is not a feature associated with valley glaciers. Valley glaciers form in mountainous regions due to the accumulation and compaction of snow, creating a flowing mass of ice within a valley. Features associated with valley glaciers include cirques, arêtes, and moraines.
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.
Two types of glaciers are valley glaciers, which flow down valleys, and ice sheets, which cover large land areas. Valley glaciers are narrower and are found in mountainous regions, while ice sheets are massive and cover extensive areas.
Valley glaciers flow down mountain slopes... so they flow down. I finally found this answer in a book.
A continental glacier can move in all directions and a valley glacier can move in a surge. :)
Continental and valley glaciers both develop in regions where there is constant snowfall and freezing temperatures throughout the year. Both types of glaciers move at a very slow pace.
canyon valley and glaciers bro
That's what causes them to move.
A long narrow glacier that forms between mountains is called a valley glacier. These glaciers flow down valleys, eroding the surrounding landscape as they move. Valley glaciers are common in mountainous regions around the world.
Continental glaciers are thicker and larger. Valley glaciers are formed on mountains; continental glaciers are formed on flat land.
valley glaciers
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.
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.