the layers deposit is because the acid rain break them apart
When flood waters deposit sediment, they can create a landform called a floodplain. Floodplains are flat, low-lying areas of land adjacent to rivers or streams that are prone to flooding. Over time, repeated flooding can build up layers of sediment, enriching the soil and creating fertile farmland.
Water deposits sediment through a process called sedimentation where particles carried by the water settle on the bottom of a water body. This can happen when the velocity of the water decreases, allowing the particles to drop out of suspension. Over time, sediment can accumulate and form layers on the bottom.
Gravity causes layers of sediment to be horizontal because as sediment deposits, it settles evenly due to gravity pulling the particles downwards. Over time, as more sediment accumulates, the weight of the new layers causes the underlying layers to compact and settle into a horizontal orientation.
The squeezing of layers of sediment is called compaction. This process reduces the volume of sediment and removes water between particles, resulting in the formation of sedimentary rocks.
Since the following options are not stated a person will not know which would most likely be covered with thick turbidite layers. Including this information would allow a person to know the right answer.
the crust will cool to form metamorphic rock
Doesa glacier deposit sediment whenit freezes
Loess deposits is form when sediment that is finer than sand, such as particles of clay and silt, is deposited into layers far from its source.
When flood waters deposit sediment, they can create a landform called a floodplain. Floodplains are flat, low-lying areas of land adjacent to rivers or streams that are prone to flooding. Over time, repeated flooding can build up layers of sediment, enriching the soil and creating fertile farmland.
A glacier deposits sediment when it melts or retreats, losing its ability to carry the material it has accumulated. As the ice melts, the sediment, known as till, is released and settles in layers, forming various landforms such as moraines, drumlins, or outwash plains. Additionally, when glaciers calve into the ocean or lakes, they can also deposit sediments directly into these bodies of water.
A sediment pile up underwater is known as a sediment deposit or accumulation, where particles settle out of suspension to form layers of sediment on the seabed. Over time, this process can create sedimentary rocks and contribute to the formation of underwater landforms like submarine canyons or seamounts.
Glaciers can deposit sediment through processes known as till and outwash. Till is unsorted sediment that is deposited directly by the glacier as it melts, forming features like moraines. Outwash occurs when meltwater from the glacier carries sediment away from the glacier's terminus, depositing it in sorted layers further downstream. Both processes contribute to the landscape and geological features shaped by glacial activity.
Its deposits sediment by picking the sediment up which is called plucking.(weathering)
When the wind starts to slow down it starts to deposit sand or other sediment.
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Water deposits sediment through a process called sedimentation where particles carried by the water settle on the bottom of a water body. This can happen when the velocity of the water decreases, allowing the particles to drop out of suspension. Over time, sediment can accumulate and form layers on the bottom.
Rivers, streams, glaciers, and wind are four agents responsible for depositing sediment in the water. These agents transport eroded material and deposit it in bodies of water, contributing to the formation of sediment layers.