Esker
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.
a glacier that stays in one spot ( stationary )answer 2 the above is OK, but these stationary ice fields are usually called ice plateaus. And they are plateaus because they don't move; otherwise they would be sloping. Actually they may have a very slight slope, but they will appear flat.
Kames. Many are found in areas of kettles and moraines.
The area of a glacier where losses of ice exceed the addition of snow is called the ablation zone. In this zone, melting, sublimation, and iceberg calving typically occur at a higher rate than snow accumulation. This can lead to glacier retreat and overall shrinking of the glacier.
eskers
A slow melting glacier
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.
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.
The rapid movement of a glacier is called a glacier surge. This sudden acceleration in movement can be caused by internal changes within the glacier, such as the release of stored meltwater or changes in the glacier's structure.
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.
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.
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."
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.
The water melting from a glacier is called the glacier melt. This water often supplies the water for some of the great rivers of the world, like the Ganges and the Yangtsee.
The unsorted rocky debris formed by a melting glacier is known as glacial till. This mixture of rock fragments of various sizes and shapes is deposited by the glacier as it retreats, with no specific order or arrangement. Glacial till can form different landforms, such as moraines or drumlins, depending on how it is deposited.
a glacier that stays in one spot ( stationary )answer 2 the above is OK, but these stationary ice fields are usually called ice plateaus. And they are plateaus because they don't move; otherwise they would be sloping. Actually they may have a very slight slope, but they will appear flat.
Kames. Many are found in areas of kettles and moraines.