An esker is a glacial landform that is created by deposition. Eskers are long, winding ridges of sand and gravel left behind by streams within or under glaciers. They form as the glacier melts and recedes, leaving behind sediment deposited by the flowing water.
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Glacial erosion shapes the land by scraping and polishing the surface, creating features like U-shaped valleys and cirques. Glacial deposition occurs when the ice melts and deposits the sediments it carried, forming landforms like moraines and drumlins. Together, these processes have significantly shaped the Earth's landscape over millions of years.
Glacial erosion refers to the process where glaciers wear away the land by scraping and gouging the surface, while glacial deposition is the process where glaciers deposit materials like rocks, sediments, and other debris that they pick up as they move. Erosion creates features like U-shaped valleys and cirques, while deposition creates features like moraines and drumlins.
glacial deposition and glacial erosion
Glacial plains are formed by the deposition of sediments carried by glaciers as they advance and retreat. When glaciers move, they pick up rocks, soil, and other materials, which are then deposited when the glacier melts. Over time, these deposited materials accumulate to create flat, wide expanses of land known as glacial plains.
Glacial lakes are primarily caused by deposition. As glaciers move, they erode the land beneath them and create depressions where meltwater collects, forming glacial lakes. The deposition of sediment carried by the glacier contributes to the formation and shape of the lake.