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unsorted deposition

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What do sediments tend to from when transported by water and wind?

Sediments transported by water and wind can form various sedimentary structures such as sand dunes, river deltas, beaches, and alluvial fans. These structures develop as the sediments settle and accumulate in response to the flow dynamics and energy of the transporting medium.


What sediments float in water?

Light materials such as sand, silt, and clay sediments tend to stay suspended in water and can float for a short period. Organic matter like plant debris and some types of algae can also float in water depending on their density and decomposition level. Oil and grease are other examples of sediments that can form a layer and float on the surface of water.


Which sediments float in the moving water?

Fine sediments like silt and clay tend to stay suspended in moving water because the turbulence keeps them from settling. Coarser sediments like sand and gravel require calmer conditions to settle out of the water column.


Where do Sediments tend to build up in the ocean?

Sediments build up in the Abyssal plain.


How are neritic sediments different form pelagic sediments?

Neritic sediments are found in shallow water close to the coast, while pelagic sediments are found in deep open ocean areas. Neritic sediments tend to be coarser and more influenced by terrestrial input, while pelagic sediments are finer and accumulate slowly over time.


Sediments tend to build up in the?

condimental shelf


What erosion agent typically deposited hills of unsorted sediments?

The erosion agent that typically deposits hills of unsorted sediments is glacial activity. As glaciers move, they carry a mixture of sediments, including clay, silt, sand, and larger rocks, without sorting them by size. When glaciers melt, they leave behind these unsorted deposits, known as till, which can form features such as drumlins or moraines. This process contrasts with other erosion agents like water or wind, which tend to sort sediments by size.


What are the steps that turn sediment into rock?

Sedimentary rocks are formed by the lithification (cementing, compacting, and hardening) of existing rock or the bones, shells, and pieces of formerly living things. Rocks are weathered and eroded into tiny particles which are then transported and deposited along with other pieces of rock called sediments. Sediments are cemented together and compacted and hardened over time by the weight and pressure of up to thousands of feet of additional sediments above them. Eventually, the sediments are lithified and become solid sedimentary rock. These sediments that come together are known as clastic sediments. Sediments usually sort themselves by the size of the particles during the deposition process so sedimentary rocks tend to contain similarly sized sedimentary particles. An alternative to clastic sediments are chemical sediments which are minerals in solution that harden. The most common chemical sedimentary rock is limestone, which is a biochemical product of calcium carbonate created by the parts of dead creatures. Approximately three-quarters of the earth's bedrock on the continents is sedimentary.


What do air masses that form over water tend to have more of than the ones that form over land?

Water vapor.


What cohesion is especially strong because water molecules tend to form?

hydrogen


Describe 2 proerties of an acid?

When mixed in pure water, acids form H+ ions. They also tend to be sour tasting. In contrast, bases form OH- and tend to be bitter.


Characteristics of sediments tansported by water and wind?

Sediments transported by water are typically rounded and well-sorted due to the continuous abrasion and sorting processes during transport. They can vary in size from fine silt to large boulders, depending on the energy of the water flow. In contrast, wind-transported sediments, such as sand, tend to be finer and more angular, as wind can only move smaller particles. Wind also results in unique features like ripples and dunes, shaped by the directional flow of air.