A slow melting glacier
The zone above the snowline on a glacier is called the accumulation zone. This is where snowfall exceeds melting, leading to an increase in glacier mass.
glacier
Meltwater streams formed by melting ice when a valley glacier stops advancing are called proglacial streams. These streams are commonly found at the terminus of a glacier where melting ice produces large volumes of water that flow down the valley.
A melting glacier gets smaller, but a growing glacier gets bigger.
When a melting glacier accumulates sand, gravel, and rocks, it forms a landform called a moraine. There are different types of moraines such as terminal, lateral, and medial moraines, depending on where they are deposited in relation to the glacier.
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.
When the glacier is formed the ice scratches the land. When the glacier recedes the ice will scar the earth. This is called glacial scarring.
A slow-moving river of ice is called a glacier. Glaciers form when snow accumulates and compresses into ice over time, flowing downhill under the force of gravity. Glaciers can carve out valleys, carry debris, and shape the landscape as they move.
She gave me her glacier eyes, so I left. The glacier is melting.
A slow-moving body of ice is called a glacier. Glaciers form over time as snow accumulates and compacts into ice. They can carve out valleys, shape the landscape, and contribute to rising sea levels as they melt.
The area that is melting faster than it is accumulating is the "Zone of Ablation." The very bottom end of a glacier is typically called its "foot."
These winding ridges of sand and small bits of gravel formed from the outwash of a melting glacier are called eskers. They are created when meltwater streams flowing beneath or within the ice deposit sediments as the glacier retreats. Eskers typically have a sinuous shape due to the flowing water underneath the glacier.