Alpine glaciers, even though they move, are confined to mountain valleys, which in most instances had previously been a stream valley. Continental ice sheets exist on a much larger scale. These huge masses flow out in all directions from one or more centers of the land. They cover the entire continent, hence the name, and extend out toward the sea. Only two exist today: Greenland and Antarctica.
Alpine glaciers are smaller in size and are found in mountainous regions, while continental glaciers cover much larger areas of land. Alpine glaciers move down valleys, while continental glaciers flow outwards in all directions from a central ice dome. Alpine glaciers are influenced by local topography and weather conditions, while continental glaciers are influenced by global climate patterns. Alpine glaciers tend to have higher melt rates due to their lower elevation compared to continental glaciers. Alpine glaciers are more accessible for study and research compared to the remote and harsh environments of continental glaciers.
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.
The two main types of glaciers are alpine glaciers, which form in mountainous regions and flow down valleys, and ice sheets, which are massive continental glaciers that cover large areas of land. Alpine glaciers are smaller and more common, while ice sheets are much larger and thicker.
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.
Continental glaciers are large and cover vast areas, so their weight and movement over time smooth out the landscape. Alpine glaciers are smaller and flow down steep mountain slopes, carving out valleys and creating jagged peaks as they erode the rock beneath them.
i dont know or care
Antarctica is a continental glacier. Alpine glaciers are a different type of glacier.
Alpine glaciers are smaller in size and are found in mountainous regions, while continental glaciers cover much larger areas of land. Alpine glaciers move down valleys, while continental glaciers flow outwards in all directions from a central ice dome. Alpine glaciers are influenced by local topography and weather conditions, while continental glaciers are influenced by global climate patterns. Alpine glaciers tend to have higher melt rates due to their lower elevation compared to continental glaciers. Alpine glaciers are more accessible for study and research compared to the remote and harsh environments of continental 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.
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.
The two main types of glaciers are alpine glaciers, which form in mountainous regions and flow down valleys, and ice sheets, which are massive continental glaciers that cover large areas of land. Alpine glaciers are smaller and more common, while ice sheets are much larger and thicker.
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.
I only know that alpine glaciers can carve deep u-shaped valleys in the mountains.
One is bigger than the other one
Alpine glaciers leave behind U-shaped valleys, deep, high-altitude lakes and cliffs. Continental glaciers flow outwards scraping the landscape clean, making fairly flat lands and lakes
beacause alpine glaciers are bad for the enviromental energy called phleux that makes chemicals interact with each other smoothing the landscape
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.