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Glaciers formed in mountains are called mountain glaciers or alpine glaciers. They are found in high-altitude regions and flow downhill through valleys.
An alpine glacier is a glacier that FORMED on a mountain. It doesn't have to BE on a mountain, just formed on one.
Alpine glaciers are found in mountain valleys
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.
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.
That would be called a Fjord.
Glaciers are ice sheets. There are 2 kinds of glaciers: alpine glaciers and continental glaciers. Alpine glaciers are formed when valleys above the snow line fill with ice and snow. Snow is compacted and gradually begins to flow downhill due to gravity. -Cham11
Upper Teesdale, located in the north of England, was formed by the action of glaciers during the last Ice Age. The movement of these glaciers over millions of years carved out the landscape and shaped the valley. The Tees River further sculpted the area, creating the unique features seen in Upper Teesdale today.
Central Park in Manhattan was formed primarily as a result of glacial deposition during the last ice age. The park's landscape features, such as its hills, valleys, and rock formations, were sculpted by the movement of glaciers and the debris they left behind.
Cirques. They are the bowl-shaped depressions formed by the erosion of glaciers in the upper parts of alpine valleys.
The bowl-shaped hollow from which alpine glaciers originate is called a cirque. Cirques are formed through the erosive action of ice and snow as they accumulate and flow down mountain slopes, carving out a steep, amphitheater-like depression. These features are typically located at high elevations and serve as the initial site for glacier formation before the ice moves downhill into valleys.
A mountain landscape is formed through processes like tectonic plate movement, volcanic activity, and erosion. Tectonic plates colliding or pulling apart can create mountain ranges, while volcanic activity can form individual peaks. Erosion from factors like wind, water, and glaciers shapes the landscape over time, creating the distinct features we see in mountains.