When multiple glaciers start their downward flow from a single point, they create a land feature known as a "paternoster lake" if they form a series of small lakes, or a "glacial cirque" if they carve out a bowl-shaped depression. This formation is typically characterized by steep cliffs and a rugged terrain shaped by the erosive power of the glaciers. The converging flow can also lead to the development of a "horn" or "arete" if the surrounding peaks are shaped by glaciers.
When multiple glaciers flow downward from a single point, they create a feature known as a "piedmont glacier." This occurs when the glaciers spread out and merge as they move into a broader lowland area, often resulting in a lobe-like formation. Piedmont glaciers can significantly reshape the landscape by eroding and depositing sediments as they advance and retreat.
THey create chichks of glaich and loves of rods
When tectonic plates push the crust downward, the land feature that forms is called a "trough" or "rift." This process can create valleys or basins where the land is depressed between higher elevations. In some cases, this can also contribute to the formation of geological features like pull-apart basins or oceanic trenches.
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.
valley glaciers
When multiple glaciers flow downward from a single point, they create a feature known as a "piedmont glacier." This occurs when the glaciers spread out and merge as they move into a broader lowland area, often resulting in a lobe-like formation. Piedmont glaciers can significantly reshape the landscape by eroding and depositing sediments as they advance and retreat.
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.
valley glaciers
Glaciers are the main agents of erosion that create U-shaped valleys. As glaciers move downhill, they carve out the valley floor and sides through the process of abrasion and plucking. The unique U-shape is a characteristic feature of valleys that have been shaped by glaciers.
You don't. Inheritance is a feature of object oriented programming languages. C is not object oriented.
THey create chichks of glaich and loves of rods
When tectonic plates push the crust downward, the land feature that forms is called a "trough" or "rift." This process can create valleys or basins where the land is depressed between higher elevations. In some cases, this can also contribute to the formation of geological features like pull-apart basins or oceanic trenches.
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.
they made by glaciers melting
I only know that alpine glaciers can carve deep u-shaped valleys in the mountains.
yes
valley glaciers