i dnt knw :(
It melts and leaves a canyon
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.
it all comes together.
Glacial till collects at the base and along the sides of a glacier, where it is deposited as the glacier moves and melts. This unsorted sediment consists of a mix of clay, silt, sand, gravel, and boulders. When the glacier retreats, it leaves behind this till, forming various landforms such as moraines, that are characterized by their heterogeneous composition. Additionally, till can also accumulate in front of the glacier, forming features like terminal moraines.
Materials bulldozed at the front of a glacier form what is known as a terminal moraine. This accumulation consists of debris that the glacier has plowed up and pushed forward as it advances. When the glacier retreats, it leaves behind this pile of sediment, which can vary in size and composition. Terminal moraines serve as important indicators of past glacial movement and can influence local ecosystems.
It melts and leaves a canyon
a glacier valley forms from the pieces of ice that the glacier leaves behind when it broken down thats all i realy know
Tomorrow
The retreating glacier leaves behind linear mounds of till (till being unsorted debris) and is known as moraine.
Because the food comes from the leaves...by kathlene claire,,,,,
Moraines are formed by the deposition of glacial debris as a glacier moves and erodes the land. As the glacier melts, it leaves behind ridges and mounds of unsorted sediment. The size and shape of a moraine can vary depending on the glacier's movement and the type of sediment deposited.
it all comes together.
The terminal moraine is the sediment deposition furthest from the source of the glacier. It is also known as an end moraine, however depending on recession or advancement of the glacier, the end moraine is not always the terminal moraine. Lateral moraines are lines of sediment deposited along the outer walls or boundaries of a glacier and can run from the top of the glacier down to its end.
Glacial till collects at the base and along the sides of a glacier, where it is deposited as the glacier moves and melts. This unsorted sediment consists of a mix of clay, silt, sand, gravel, and boulders. When the glacier retreats, it leaves behind this till, forming various landforms such as moraines, that are characterized by their heterogeneous composition. Additionally, till can also accumulate in front of the glacier, forming features like terminal moraines.
Materials bulldozed at the front of a glacier form what is known as a terminal moraine. This accumulation consists of debris that the glacier has plowed up and pushed forward as it advances. When the glacier retreats, it leaves behind this pile of sediment, which can vary in size and composition. Terminal moraines serve as important indicators of past glacial movement and can influence local ecosystems.
Glacial moraines are accumulations of rock, soil, and debris carried and deposited by a glacier. They form as the glacier flows, picking up material from the land surface and carrying it along. Once the glacier retreats, it leaves behind these deposits, creating distinctive ridges and mounds.
* Fryingpan Glacier * Nisqually Glacier * Paradise Glacier * Pyramid Glacier * Puyallup Glacier * South Tahoma Glacier * Tahoma Glacier * Success Glacier * Sarvent Glacier