Bottom and side?
The debris left behind by a melting glacier is called "moraine." Moraines consist of a mixture of soil, rocks, and sediment that the glacier has eroded and transported. They are typically found at the edges or terminus of the glacier, forming ridges or piles that mark the glacier's former extent.
still flows and carries debris to the end of the glacier
The debris on top of a glacier, often referred to as "glacial till," accumulates through processes such as erosion and weathering of surrounding rock and soil. As glaciers move, they scrape the landscape, picking up and transporting this material. Additionally, debris can be deposited on the glacier's surface from rockfalls or landslides occurring on steep mountain slopes nearby. Over time, this debris becomes embedded in the glacier as it advances and retreats.
Ridges that form along the sides of glacial valleys as a glacier melts are called moraines. Specifically, lateral moraines are found along the edges of a glacier, while terminal moraines accumulate at the glacier's end. These features are composed of debris and sediment that the glacier has transported and deposited as it advances and retreats.
Glacial debris gets incorporated into the glacier as it flows over the landscape, picking up rocks, sediment, and other materials. These materials are then transported within the glacier towards its base due to the movement of the ice. Once the glacier reaches a warmer area or melts, the debris is deposited on the ground or in bodies of water, leaving behind evidence of the glacier's path.
Terminal moraines are ridges of glacial debris deposited at the furthest point reached by a glacier. They mark the end of a glacier's advance and can be seen as a line of debris and rocks left behind as the glacier melts and retreats. These moraines are called "terminal" because they are found at the glacier’s terminus.
The debris left behind by a melting glacier is called "moraine." Moraines consist of a mixture of soil, rocks, and sediment that the glacier has eroded and transported. They are typically found at the edges or terminus of the glacier, forming ridges or piles that mark the glacier's former extent.
Moraines are found along the edges, flanks, and in the middle of glaciers. They are formed from debris and rocks that have been transported and deposited by the glacier's movement. Lateral moraines form along the sides, medial moraines run down the center, and terminal moraines are found at the glacier's terminus.
The unsorted rocky debris formed by a melting glacier is known as glacial till. This mixture of rock fragments of various sizes and shapes is deposited by the glacier as it retreats, with no specific order or arrangement. Glacial till can form different landforms, such as moraines or drumlins, depending on how it is deposited.
it's a valley glacier, it moves slowly carrying debris and melted snow.
Ridges of rock debris that form in front of a glacier are called terminal moraines at the point that the glacier stops moving ahead.
Terminal moraine: a ridge of glacial debris deposited at the furthest advance of a glacier. Lateral moraine: debris deposited along the sides of a glacier. Medial moraine: a ridge of debris formed where two glaciers merge. Recessional moraine: ridges of debris left behind as a glacier retreats.
still flows and carries debris to the end of the glacier
still flows and carries debris to the end of the glacier
A short answer:Glacier debris, or more properly called glacial debris,would be made up of bits of rock that were deposited by a glacier after it had melted away.A longer answer:Glacial debris is produced by the action of glaciers. As you probably know, glaciers are massive sheets of ice that advance and recede depending on the amount of snow that they get and the climate in the area. Because they are made of ice, they are very strong and able to pick up rocks of all sizes, from large boulders to small specks of sand.As glaciers creep along the landscape, they often pick up these pieces of rock and transport them as the glacier advances. When the glacier melts, these pieces of rock are left behind as glacial debris.
The debris on top of a glacier, often referred to as "glacial till," accumulates through processes such as erosion and weathering of surrounding rock and soil. As glaciers move, they scrape the landscape, picking up and transporting this material. Additionally, debris can be deposited on the glacier's surface from rockfalls or landslides occurring on steep mountain slopes nearby. Over time, this debris becomes embedded in the glacier as it advances and retreats.
Ridges that form along the sides of glacial valleys as a glacier melts are called moraines. Specifically, lateral moraines are found along the edges of a glacier, while terminal moraines accumulate at the glacier's end. These features are composed of debris and sediment that the glacier has transported and deposited as it advances and retreats.