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.
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.
glacier
Floating ice around a glacier, often in the form of icebergs or sea ice, acts as an insulating barrier that reduces heat exchange between the warmer ocean water and the glacier. This insulation helps to slow down the melting of the glacier's ice face where it meets the water. Additionally, the presence of floating ice can obstruct the flow of warmer currents, further protecting the glacier from accelerated melting. Consequently, this floating ice can significantly prolong the lifespan of the glacier.
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."