Do not
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.
Sharp pyramid-shaped peaks formed by alpine glaciers are called "horns." These features occur when multiple glaciers erode a mountain from different sides, creating steep, pointed summits. The most famous example is the Matterhorn in the Swiss Alps. Horns are typically characterized by their rugged, jagged profiles, resulting from the intense glacial activity.
The bowl-shaped hollow from which alpine glaciers originate is called a "cirque." Formed by the processes of erosion and weathering, a cirque is typically situated on the side of a mountain and is characterized by steep walls and a flat bottom. As snow accumulates in this hollow, it compacts into ice, eventually leading to glacial movement down the mountainside. Cirques play a crucial role in the development of alpine glaciers and the surrounding landscape.
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 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
That would be called a Fjord.
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.
An area that has been recently glaciated is most likely to display features such as U-shaped valleys, which are formed as glaciers carve through the landscape. Additionally, one might observe moraines, which are accumulations of debris deposited by glaciers, and fjords, which are deep, narrow inlets created when glaciers retreat. Other features include exposed bedrock and kettle lakes, formed by melting ice blocks.
Cirques. They are the bowl-shaped depressions formed by the erosion of glaciers in the upper parts of alpine valleys.