yes glaciers can flow they are much like water exept well solid XD
always lolcat123
They difference between them is where there flow. Continental glaciers are enormous ice sheets, and are found in Greenland and Antarctica. Alpine glaciers form in mountain valleys.
Glaciers formed in mountains are called mountain glaciers or alpine glaciers. They are found in high-altitude regions and flow downhill through valleys.
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.
When multiple glaciers start their downward flow from a single point, they create a valley glacier. This type of glacier forms as two or more alpine glaciers flow together and merge into a single larger glacier that moves down a valley. Valley glaciers can be quite large and have a significant impact on shaping the landscape.
Valley glaciers flow down mountain slopes... so they flow down. I finally found this answer in a book.
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.
glaciers move slowly but when theres alot of rain the water and the glaciers move faster
Glaciers flow due to the force of gravity pulling them downhill. Factors that influence their movement include the slope of the terrain, the thickness of the ice, and the presence of meltwater at the base of the glacier.
It shows the movement of people, goods, ideas, animals, or glaciers.
Lava flow maybe, it is the exact opposite in my oppinion.
Valley glaciers are pieces of ice that flow down in the bottoms of steep valleys. These are found down between the bases of mountains.
Glaciers. Glaciers are large masses of ice that flow slowly over land, shaping the land through processes like erosion and deposition.