Alpine Glacier produce a variety of erosional features. These features are usually rounded or polished grooves made by the glacier's passing. The features are called arete, Circque, horn, tarn, u shaped valley, and hanging valleys.
The alpine glaciers are high in the mountains.
Antarctica is a continental glacier. Alpine glaciers are a different type of glacier.
The bottom of alpine glaciers are rugged or rough, so they create a rugged landscape. They move because when the bottom of them melt, the water produced allows it to slide. (they typically move downhill) From a science book "Earth's Changing Surface" by Holt Science & Technology.
There are two primary types of glaciers: alpine glaciers and continental glaciers. Alpine glaciers, found in mountainous regions, carve sharp, U-shaped valleys and create features like cirques and arêtes as they move down slopes. In contrast, continental glaciers, which cover vast land areas like Greenland and Antarctica, reshape the landscape on a much larger scale, flattening terrain and depositing thick layers of sediment, resulting in features like drumlins and moraines. While both types of glaciers erode and transport material, their impacts on the land differ significantly due to their sizes and environments.
Glaciers that create cirques on the sides of mountains are called cirque glaciers. These glaciers form in bowl-shaped depressions on the slopes of mountains and are responsible for eroding and shaping the characteristic amphitheater-like features known as cirques. Examples of cirque glaciers can be found in mountain ranges around the world, such as the Alps, Andes, and Himalayas.
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The alpine glaciers are high in the mountains.
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 are found in mountain valleys
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