Valley Glaciers!
valley glaciers
valley glaciers
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.
One is bigger than the other one
Advancing glaciers are glaciers that are moving forward and expanding, while retreating glaciers are glaciers that are melting and shrinking. Stationary glaciers are glaciers that are not currently advancing or retreating, maintaining a relatively stable position.
Modern day footballs are actually more elongated, oval shaped then the original round ones.
Alpine glaciers form in mountainous regions and are confined within valleys or cirques, while continental glaciers are large ice sheets that cover vast land areas. Alpine glaciers are typically smaller and more fragmented compared to the continuous ice sheets of continental glaciers.
These long narrow glaciers are called valley glaciers. They form when snow accumulates in a valley and slowly turns into ice, flowing downhill under the force of gravity. Valley glaciers are often found between mountains in regions like the Alps and the Andes.
Sex love and peace
What is the difference between standard theory and extended standard theory?
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.