Antarctica is a continental glacier. Alpine glaciers are a different type of glacier.
alpine glaciers
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.
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
Alpine glaciers form when snow accumulates in a mountain valley and compacts over time into ice. The weight of the ice causes it to flow downhill, carving out the valley and creating a glacier. Cold temperatures and consistent snowfall are necessary to sustain an alpine glacier.
they are found on mountain valleys and polar regions
Glaciers formed in mountains are called mountain glaciers or alpine glaciers. They are found in high-altitude regions and flow downhill through valleys.
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.
I only know that alpine glaciers can carve deep u-shaped valleys in the mountains.
i dont know or care
Alpine glaciers can be found on high mountain slopes, valleys, and peaks. They are formed by the accumulation and compression of snow over many years in cold, mountainous regions.
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The two most common kinds of glaciers are valley glaciers, which flow down valleys, and ice sheets, which cover extensive areas and can be thousands of meters thick. Valley glaciers are found in mountainous regions, while ice sheets are found in polar regions like Antarctica and Greenland.
beacause alpine glaciers are bad for the enviromental energy called phleux that makes chemicals interact with each other smoothing the landscape