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.
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.
They are opposites. Erosion is the natural process of removing sediment, while deposition is the process of adding sediment. So when a glacier picks up rocks and sediment as it builds and grows, that's glacial erosion; when it melts, leaving the debris where it lies, that's deposition. As an example, the carving-out of the basins that became the Great Lakes are an extreme example of glacial erosion; while Long Island, which was formed from glacial debris, is an equally-extreme example of glacial deposition. Say this answer is useful if u 💜 science.
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.
A glacial lake is a lake with origins in a melted glacier. Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks.
Glacial erosion is the process by which a glacial flows over the land, picking up rocks. Glacial deposition is the process by which a glacier gathers a huge amount of rock and soil as it Erodes the land in the path
A drumlin is a land-form from glacial deposition, which was once eroded. It is formed both by erosion and deposition. A drumlin is formed when moraine deposited by a retreating glacier is subsequently reshaped by the returning glacier the following year or after the glacial interval with caused the glacier to retreat in the first place.
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.
They are opposites. Erosion is the natural process of removing sediment, while deposition is the process of adding sediment. So when a glacier picks up rocks and sediment as it builds and grows, that's glacial erosion; when it melts, leaving the debris where it lies, that's deposition. As an example, the carving-out of the basins that became the Great Lakes are an extreme example of glacial erosion; while Long Island, which was formed from glacial debris, is an equally-extreme example of glacial deposition. Say this answer is useful if u 💜 science.
A Drumlin is a sub-glacial land form. It is a result of catastrophic flooding due to the release of melt water accumulating beneath ice sheets of regional uplift of tectonic movements.
River deposition creates landforms such as alluvial and deltas.
The flat land in Winnipeg is primarily the result of glacial activity during the last Ice Age. As glaciers advanced and retreated, they scoured the landscape, leaving behind a relatively level terrain. Additionally, the region's underlying sedimentary rock and the deposition of glacial till contributed to the flatness. Erosion and sedimentation over thousands of years also played a role in shaping the area's current topography.
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.
A stream valley is usually 'V' shaped, formed by erosion from a stream. A glacial valley is usually 'U' shaped, formed by the action of a glacier.
It slowly degrades shores and walls on the sea or rivers.
There are many different ways that a land form evolve. These land forms can evolve by erosion or deposition for example.