Alpine glaciers form when snow piles up after a while they begin to build up eventually making an alpine glacier.
The alpine glaciers are high in the mountains.
Antarctica is a continental glacier. Alpine glaciers are a different type of glacier.
alpine glaciers
Valley glaciers form when ice and snow accumulate in a mountain valley due to the accumulation of snow exceeding the rate of melting. Over time, the ice flows downhill, shaping the valley and creating a distinct U-shaped profile.
One type of Alpine glacier is a cirque glacier, which forms in a bowl-shaped depression on the side of a mountain. These glaciers are typically small and may be found at the head of a valley or on a mountainside.
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.
The alpine glaciers are high in the mountains.
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.
Glaciers formed in mountains are called mountain glaciers or alpine glaciers. They are found in high-altitude regions and flow downhill through valleys.
They form at high places and when snow piles up after a while they begin to build up eventually making an alpine glacier.
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.
I only know that alpine glaciers can carve deep u-shaped valleys in the mountains.
i dont know or care
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.
Alpine glaciers are found in mountain valleys
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