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When wind slows down or meets an obstacle, it loses the energy needed to transport sediment and may deposit the material it was carrying. This process can lead to erosion around the obstacle where the wind's ability to move the sediment is diminished.
A sediment deposit called a windward slope forms when sediment is blown against an obstacle and settles behind it. This deposit is characterized by a gradual slope facing into the prevailing wind direction.
Glacial deposition is the process by which glaciers transport and deposit sediments, rocks, and other materials as they move. One example of glacial deposition is the formation of moraines, which are long ridges of material left behind by a glacier as it retreats.
Water can deposit sediment such as sand, silt, and clay. Wind can deposit smaller particles like sand and dust. Melting glaciers can deposit a mixture of rocks, sediments, and debris known as moraines.
A continental deposit of gravel and sand is typically created by the erosion and transportation of rock fragments by rivers, glaciers, or wind to a new location. These deposits can accumulate over time, forming layers of sediment that eventually solidify into sedimentary rocks like sandstone or conglomerate. They are important sources of building materials and may also contain valuable minerals or fossils.
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When an obstacle causes wind to slow down and deposit materials, the materials can pile up and eventually form a dune. Dunes are formed through the accumulation of sand or other sediments carried by the wind and deposited behind the obstacle, such as a rock or vegetation. Over time, these sediments build up, forming characteristic features of dune formations.
When an obstacle causes wind to slow down and deposit materials, it can create a landform known as a dune. Dunes are formed by the accumulation of sand or other sediments as they are carried by the wind and then deposited behind the obstacle. Over time, these deposits can pile up and shape the characteristic features of a dune.
deposition is incorrect, the answer is a sand dune
When wind slows down or meets an obstacle, it loses the energy needed to transport sediment and may deposit the material it was carrying. This process can lead to erosion around the obstacle where the wind's ability to move the sediment is diminished.
When blowing sand encounters an obstacle, it can deposit and accumulate on the leeward side, forming a mound or dune. This process is known as sand deposition or aeolian deposition. The deposited sand can eventually lead to the formation of various landforms such as sand dunes.
A stream deposits material when its velocity decreases, causing sediment to settle out of the water and accumulate on the streambed. This can occur when the stream widens, becomes shallower, or encounters an obstacle that slows its flow. The deposited material forms features like bars, deltas, and floodplains.
A sediment deposit called a windward slope forms when sediment is blown against an obstacle and settles behind it. This deposit is characterized by a gradual slope facing into the prevailing wind direction.
The obstacle is called a windbreak, which disrupts wind flow and causes particles to settle due to reduced wind speed. This process is known as wind deposition.
It's just known as an Eolian (wind-driven) deposit. It will result in the formation of a slope of varying degrees, depending on the friction of the material against itself. Greater friction will lead to a slope of greater angle.
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