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.
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.
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.
A glacier that picks up debris and moves it to other places is called a "lateral moraine." This debris is typically picked up along the sides of the glacier as it moves, and is then deposited in new locations as the glacier advances or retreats.
A large pile of rock and debris left by a receding glacier is known as a moraine. Moraines can consist of different sizes of material, from clay and silt to boulders, and are typically deposited along the sides or at the terminus of a glacier.
The front of a glacier is called the terminus or terminus face. This is where the glacier ends and may be characterized by ice cliffs or a build-up of glacial debris.
an accumulation of boulders, stones, or other debris carried and deposited by a glacier.
Debris on a glacier can be found scattered on the glacier's surface, within crevasses, or concentrated at the glacier's margins. It can include rocks, sediment, and even man-made objects that have fallen or been carried onto the glacier.
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
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.
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.
the glacier picks up the sediments, rocks, till, debris, and soil and carries them along while the glacier moves and will eventually drop them.
A glacier that picks up debris and moves it to other places is called a "lateral moraine." This debris is typically picked up along the sides of the glacier as it moves, and is then deposited in new locations as the glacier advances or retreats.
The accumulation of unsorted rocky debris that is formed by a melting glacier is called a moraine. There are many large moraines throughout the northern parts of North America, Europe, and Asia.