a glacier has a snowline at the same height as the wastage line.
A glacier snout is the terminus or end point of a glacier where ice and meltwater are released. It is where the glacier meets lower elevations and warmer temperatures, causing melting and ice loss. The snout can vary in shape and size depending on the glacier's dynamics.
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Valley glaciers are typically advancing when their terminus is pushing forward, causing the glacier to grow in size. Conversely, they are retreating if the terminus is melting or receding, leading to a decrease in glacier size. Monitoring changes in the glacier front position over time can help determine if it is advancing or retreating.
Depending on when it was formed, the size and speed it is moving it could be either an Avalanche or Glacier. If it is an incredibly old, slow moving, large, ice mass it is likely a Glacier; however if it is a quickly moving, small (relatively), ice mass it is an Avalanche.
a glacier has a snowline at the same height as the wastage line.
A glacier can not do any damage to earth and it depends on the size of the glacier if it is huge it may flood
Temperature influences glacier size.
Glaciers can vary in size, with the largest glacier in the world being the Lambert Glacier in Antarctica, which is over 60 miles wide and 250 miles long. The size of a glacier can be affected by factors such as its location, climate, and topography.
A glacier snout is the terminus or end point of a glacier where ice and meltwater are released. It is where the glacier meets lower elevations and warmer temperatures, causing melting and ice loss. The snout can vary in shape and size depending on the glacier's dynamics.
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The Lambert Glacier in Antarctica is the largest glacier on earth. Its roughly 40 000 sq km (25 000 sq mi) in size.
Valley glaciers are typically advancing when their terminus is pushing forward, causing the glacier to grow in size. Conversely, they are retreating if the terminus is melting or receding, leading to a decrease in glacier size. Monitoring changes in the glacier front position over time can help determine if it is advancing or retreating.
Its depends on the temperature in the area and Save the size of the glacier
A graph showing particle size (y-axis) versus distance from glacier source (x-axis) would best represent the range of particle sizes that can be carried by a glacier. The graph would show that larger particles are carried closer to the source of the glacier, while smaller particles are transported further away.