Continental glaciers are larger and flow over vast regions, leading to erosion and smoothing of the landscape. Alpine glaciers are smaller and flow through steep mountain valleys, resulting in more specific and localized erosion that creates a rugged landscape with sharp peaks, cirques, and ridges.
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.
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.
Continental glaciers smooth the landscape because the immense weight and pressure of the ice sheets scrape and erode the underlying rocks and soil as they slowly move across the land. This process, known as glacial erosion, acts like sandpaper, grinding down the surface features and creating smooth, flat expanses of land. Additionally, the movement of the glacier can carry and deposit the eroded material, further reshaping the landscape.
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.
beacause alpine glaciers are bad for the enviromental energy called phleux that makes chemicals interact with each other smoothing the landscape
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
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.
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.
Antarctica is a continental glacier. Alpine glaciers are a different type of glacier.
i dont know or care
Do not
Continental glaciers smooth the landscape because the immense weight and pressure of the ice sheets scrape and erode the underlying rocks and soil as they slowly move across the land. This process, known as glacial erosion, acts like sandpaper, grinding down the surface features and creating smooth, flat expanses of land. Additionally, the movement of the glacier can carry and deposit the eroded material, further reshaping the landscape.
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.
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.