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.
Alpine glaciers create several distinctive features, including U-shaped valleys, cirques, and moraines. U-shaped valleys are formed as glaciers carve through mountainous terrain, eroding the sides and base to create a broad, flat valley floor. Cirques are bowl-shaped depressions formed at the head of a glacier, where ice accumulates and scours the rock beneath it. Moraines are accumulations of debris, such as rocks and sediment, that are pushed along and deposited by the glacier as it moves and melts.
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.
Two significant physical features of the Midwest created by glaciers are the Great Lakes and the numerous moraines. The Great Lakes were formed by the retreat of glaciers that carved out large basins, which later filled with water. Moraines, which are accumulations of debris deposited by glaciers, shape the landscape and can be seen as ridges or hills across the region. These glacial features have greatly influenced the ecology and economy of the Midwest.
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.