beacause alpine glaciers are bad for the enviromental energy called phleux that makes chemicals interact with each other smoothing the landscape
I only know that alpine glaciers can carve deep u-shaped valleys in the mountains.
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.
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.
When multiple glaciers start their downward flow from a single point, they create a valley glacier. This type of glacier forms as two or more alpine glaciers flow together and merge into a single larger glacier that moves down a valley. Valley glaciers can be quite large and have a significant impact on shaping the landscape.
Continental glaciers create a variety of landforms, including moraines, which are ridges of debris left behind as glaciers advance and retreat. They also form drumlins, which are streamlined hills shaped by glacial movement, and kettles, which are depressions that result from melting ice blocks. Additionally, continental glaciers can carve out large basins and fjords, reshaping the landscape significantly. These features reflect the dynamic processes of glacial erosion and deposition.
Alpine glaciers create distinctive features through processes of erosion and deposition. As glaciers move down mountainous terrain, they carve out U-shaped valleys and sharp peaks, known as horns, through abrasion and plucking of rock. Additionally, when glaciers melt, they deposit sediment in the form of moraines, which are ridges of debris left at the glacier's edge. These processes collectively shape the dramatic landscapes characteristic of alpine environments.
Both are made of compacted snow which recrystallizes into solid ice.They both make Striates or Grooves, shaping the landscape they move over.Both originate in high regions where the snowfall exceeds the amount of melt. This is called the zone of accumulation.Both are pulled down slopes with Gravity, as the immense weight of accumulated snow and ice can no longer support its own weight, and begins to flow outward.Both are an agent of Erosion as the flow of ice pushes, plucks and carries material from one place to another place.Both weather rock surfaces by reducing the size of the rock formations they flow over; this is due to abrasion, plucking and grinding of rock.Both carry Sediments and deposit them somewhere else.Both create Morraines, or accumulations of soil and rock where the glacier reaches its furthest point of advance in any direction.
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.
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.
Continental glaciers, which cover vast land areas, reshape the landscape by flattening it and creating features like fjords and drumlins through their immense weight and movement. In contrast, valley glaciers, confined to mountain valleys, carve deep U-shaped valleys and sharp peaks by eroding the terrain in a more localized manner. While both types of glaciers erode and deposit sediment, continental glaciers tend to have a broader, more uniform impact, whereas valley glaciers create more pronounced topographical features. This results in distinct geological landscapes influenced by the scale and flow patterns of each glacier type.
Continental glaciers, also known as ice sheets, cover vast areas of land and can reshape entire landscapes through their immense weight and movement, often resulting in a flat terrain and the formation of features like drumlins and eskers. In contrast, valley glaciers are smaller and confined to mountainous regions, carving U-shaped valleys and sharp peaks as they flow down slopes. While continental glaciers can create extensive plains and depressions, valley glaciers typically enhance topographic relief and create distinct landforms like cirques and aretes. Overall, the scale and movement patterns of these glaciers lead to different geomorphological impacts on the Earth's surface.