glaciers modify a valley by its erotional features i.e. lateral cutting effect it turns v shaped valley into u shaped 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.
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.
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.
No. Valley glaciers are a few miles to a few tens of miles long. Continental glaciers are hundreds to thousands of miles long.
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
Valley Glaciers!