Valley glaciers flow down mountain slopes... so they flow down. I finally found this answer in a book.
No. Valley glaciers are found in high mountain valleys. Continental glaciers, also called ice sheets, move across vast expanses of land regardless of terrain.
These are glaciers.
Heaps of earth moved by glaciers are called moraines. These are composed of a mixture of rocks, sediment, and debris that are picked up and transported by glaciers as they move and are then deposited as the glacier melts.
Yes, they move down slope under their own weight.
they move very slowly down a mountain
Valley glaciers flow down mountain slopes... so they flow down. I finally found this answer in a book.
No. Valley glaciers are found in high mountain valleys. Continental glaciers, also called ice sheets, move across vast expanses of land regardless of terrain.
No. The Alps are a mountain range in Europe. Glaciers are large masses of ice that move slowly due to their weight. Glaciers are commonly found in mountain ranges such as the Alps/
These are glaciers.
Heaps of earth moved by glaciers are called moraines. These are composed of a mixture of rocks, sediment, and debris that are picked up and transported by glaciers as they move and are then deposited as the glacier melts.
A glacier is a massive river of ice, rocks, and soil that moves slowly down a mountain due to gravity. Glaciers form from the gradual accumulation and compaction of snow over time.
Yes, they move down slope under their own weight.
One main difference is that continental glaciers are much larger in size and cover vast areas of land or even entire continents, while valley glaciers are smaller and confined to mountain valleys or depressions. Continental glaciers flow out in all directions from a central region, whereas valley glaciers flow down valleys due to gravity.
Glaciers move slowly.
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.
Glaciers move due to a combination of gravity and pressure. As snow accumulates, it compresses into ice which then flows under its own weight. The basal sliding of the glacier also helps in its movement.