Cirque glaciers.
Mountains formed by magma that reaches the Earth's surface are called volcanoes.
Continental glaciers and valley glaciers are both types of glaciers that form from accumulated snowfall. They both flow under the influence of gravity, albeit in different directions. While continental glaciers cover vast areas like an ice sheet, valley glaciers are confined to mountain valleys and flow down through them.
Sharp pyramid-shaped peaks formed by alpine glaciers are called horn glaciers. Horn glaciers are created when three or more cirque glaciers erode a mountain from different sides, leaving behind a sharp-edged peak. Famous examples include the Matterhorn in the Alps.
These long narrow glaciers are called valley glaciers. They form when snow accumulates in a valley and slowly turns into ice, flowing downhill under the force of gravity. Valley glaciers are often found between mountains in regions like the Alps and the Andes.
Plateau mountains are formed through the uplifting and tilting of large sections of the Earth's crust. This uplift can be caused by tectonic forces, such as the collision of continental plates, or by volcanic activity. Over time, erosion processes, such as glaciers and rivers, shape the plateau mountains into their distinctive flat-topped appearance.
Continental glaciers are thicker and larger. Valley glaciers are formed on mountains; continental glaciers are formed on flat land.
mountain glaciers
Rocks/Mountains.
That would be called a Fjord.
A low land between hills or mountains is called a valley. Valleys are typically formed through erosion by rivers or glaciers over time. They often have fertile soil and are important for agriculture and settlement.
Glaciers don't 'hit' anything, they are formed by thousands of years of snowfall that doesn't melt and thus compacts and stays in place on high, cold mountains, moving very slowly downwards. There are glaciers on some of the mountains in the Andes.
The low land between two mountains is called a valley. It is a low-lying area surrounded by higher ground such as mountains or hills. Valleys are often formed by the erosion of rivers or glaciers over time.
A low lying land between hills or mountains is called a valley
Glaciers formed during the ice age when earth was so cold that water in the coldest places just became frozen mountains, called icebergs.
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.
The fjords are surrounded by rugged mountains. We can find them on the shoreline in Labrador. They are formed by glaciers that sculpted the valley's from a <<v>> shape to a <<u>> shape.
Mountains formed by magma that reaches the Earth's surface are called volcanoes.