by either, pushing it further into the ground by top forces. or pushing around it because it has already got a rooted path to the ground. however if you mean how can they move objects and make it look like the have left them, then it is simply picking and plucking!
Answer:
Ice may look like solid (and feel like it when you fall) but it acts as a liquid under many conditions. When pressed against an object it melts a bit and flows out of the way. In the classic physics experiment a wire is stretched over a block of ice and pulled down with two weights. The wire passes through the ice with the ice melting on the downward side and reforming on the upper side.Technically this is referred to as "Regelation", the phenomenon of melting under pressure and freezing again when the pressure is reduced.
yes glaciers can flow they are much like water exept well solid XD always lolcat123
Yes, glaciers are made of solid water. Glaciers form when snow accumulates over time and undergoes compaction and recrystallization, turning into ice. The weight of the accumulated ice causes it to flow slowly downhill, resulting in the formation of glaciers.
Topographic features such as valleys, ridges, and slopes significantly influence the flow of glaciers. Steep slopes can accelerate flow due to gravity, while valleys can funnel and direct the glacier's movement. Additionally, the presence of obstacles like mountains can create stress points, causing the glacier to deform and extend in specific directions. Overall, the interplay between elevation changes and landscape contours plays a crucial role in determining the flow patterns of glaciers.
The term used to describe the movement of a glacier around small obstacles at its base is called "plucking." This process involves the glacier lifting and carrying rocks and debris as it flows over and around obstacles.
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.
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.
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.
A solid does not flow easily.
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.