because they they shaped history
because they they shaped history
It makes a u-shape
It makes a u-shape
a mountain range
A new mountain range will likely experience erosion due to weathering processes such as rain, wind, and glaciers, which will shape the landscape over time. The mountains may also undergo tectonic activity, causing earthquakes and volcanic eruptions. Over millions of years, the new mountain range will likely continue to change and evolve due to these natural processes.
Mount Aspiring is considered to be a classic horn shape, a terminal landform in mountain sculpting by glaciers.
The Matterhorn was primarily shaped by glacial erosion. The movement of glaciers over thousands of years carved and sculpted the distinctive pyramid shape of the mountain.
Yes, glaciers can profoundly shape mountains through the processes of erosion, transportation, and deposition of sediments. Glaciers carve out U-shaped valleys, create cirques and aretes, and deposit moraines, all of which contribute to the unique features of mountain landscapes. Additionally, the weight of glaciers can cause the Earth's crust to bend and uplift, influencing mountain formation.
A series of mountain is known as range; for example, the Indian Himalayan Range
A confined glacier is a glacier that is confined by topography. For example, a glacier that forms on a mountain. Continental glaciers, by contrast, are not affected. The glaciers on Antarctica and Greenland are continental glaciers. The glaciers at Glacier Bay National Park, or on a mountain are confined glaciers.
Mount Olympus is considered a fold mountain, which is the most common type of mountain. They get this name because the edges crumble when two plates collide while the mountain is being formed.
a mountain range