Erosion and Sedimentation

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Erosion and Sedimentation

Erosion in the context of soil and watershed conservation is the detachment and movement of soil particles by natural forces, primarily water and wind. More broadly, erosion is the process of wearing away rocks, geologic, and soil material via water, wind, or ice (e.g., glaciers). Erosion will transport materials after mechanical weathering has broken rock and geologic materials down into smaller, moveable pieces.

Sedimentation is the process in which particulate matter carried from its point of origin by either natural or human-enhanced processes is deposited elsewhere on land surfaces or in waterbodies. Sediment is a natural product of stream erosion; however, the sediment load may be increased by human practices. Such enhanced sources of sediment in a watershed include unvegetated streambanks and uncovered soil regions, including construction sites, deforested areas, and croplands.

Erosive Forces

Through different types of erosion, the Earth's surface is continually being reshaped. Landmasses are altered as waves and tides erode old lands while silt and other sediments deposited in waterbodies build up new lands. Over geologic time, some gullies become ravines and eventually valleys. More than 1,500 meters (5,000 feet) deep, the Grand Canyon in Arizona was produced by erosion over a 5-million-year timeframe.


Glaciers are important means of erosion over long periods of time. Although a glacier moves slowly, it eventually removes material from the surface over which it travels through processes such as plucking, abrasion, crushing, and fracturing. Rock fragments, located at the bottom and sides of moving ice masses, will grind and scour bedrock to eventually form the walls and floors of mountain valleys.


Wind can move sediment grains over long distances when they are carried through the air. Sediments also can be blown along expanses of land, such as beaches, mudflats, unvegetated cropland, or construction areas. Obstructions help reduce the wind's erosive capacity; hence, windblown sediment often is deposited at these locations.


Flowing water plays a major role in erosion by carrying away soils and other materials on the land surface. In general, there is a potential for water erosion where the land slope is at least 2 percent. The four types of water erosion of soil are sheet, rill, gully, and tunnel.

Sheet erosion is the uniform removal of soil without the development of visible water channels. It is the least apparent of the four erosion types. Rill erosion is soil removal through the cutting of many small, but conspicuous, channels. Gully erosion is the consequence of water that cuts down into the soil along the line of flow. Gullies develop more quickly in places like animal trails, plow furrows, and vehicle ruts.* Tunnel erosion may occur in soils with sublayers that have a greater tendency to transport flowing water than does the surface layer.

Along the seacoast, erosion of rocky coastal cliffs and sandy beaches results from the strong, unceasing action of currents and waves. Severe storms exacerbate the problem of sandy beach erosion. In many world regions, land and economic losses due to coastal erosion represents a serious problem.*

Stream Sedimentation

In the context of stream hydrology, sediment is inorganic and organic material that is transported by, suspended in, or deposited by streams. Sediment load, which is the quantity of sediment transported by a stream, is a function of stream discharge, soil and land-cover features, weather conditions, land-use activities, and many other factors. Sediment load carried by streams and rivers can be composed either of fine materials, mostly silts and clays, or larger materials such as sand.

Solid sediment load can be divided into two components on the basis of the mode of sediment transport: suspended sediment, and bedload sediment, each of which is produced by mechanical weathering processes, is clearly visible, and is able to settle out of water. Suspended sediment consists of silt-sized and clay-sized particles held in suspension by turbulence in flowing water. Bedload sediment consists of larger particles which slide, roll, or bounce along the streambed by the force of moving water. Dissolved load consists of inconspicuous material in solution moving downstream. It is produced by chemical weathering processes, and does not settle out of water.

Sediment yield is the total quantity of sediment transported from a watershed (drainage basin) at a given location in a given period of time. Low suspended sediment yields can be attributed to, among other factors, a region's low erosion rate. Permeable soils and low topographic relief, in general, help limit the availability of eroded material from within a watershed. Conversely, relatively impermeable soils and steep topography can yield high erosion rates and therefore greater sediment yield.

Accelerated Sedimentation.

Changes in land use, streamflow characteristics, and drainage patterns can alter the natural sedimentation rate. Historically, agriculture has been a main source of human-enhanced sediments in waterbodies. U.S. farming, for instance, accounts for an annual erosion loss of over 3 billion metric tons of soil.

The conversion of wetlands or woodlands to cropland can increase soil erosion and the associated sedimentation in streams, particularly when bare soil is exposed.* Windblown particles from bare soils also contribute to sedimentation problems. Activities such as dredging and channelization that increase stream slope and velocity can increase the stream's erosive capacity and sediment-transport capability. Construction projects within or adjacent to streams can contribute to sedimentation problems as they dislodge or expose soils and sediments.

Ecological and Economic Impacts

Excessive erosion can reduce the soil's inherent productivity, whereas the associated sedimentation can damage young plants and fill drainage ditches, lakes, and streams. Erosive processes can reduce farm income by decreasing crop yields and increasing maintenance costs for drainage systems. Additional erosion damages in both rural and urban areas include reduced property values, deteriorated water quality, and increased costs of removing sediment from roadways, roadside ditches, and surface-water supplies.

One of the principal causes of degraded water quality and aquatic habitat is the depositing of eroded soil sediment in waterbodies. Excessive amounts of sediment resulting from natural or human-induced causes can result in the destruction of aquatic habitat and a reduction in the diversity and abundance of aquatic life. Diversity and population size of fish species, mussels, and benthic (bottom-dwelling) macroinvertebrates associated with coarse substrates can be greatly reduced if the substrates are covered with sand and silt. Where sand or silt substrates have historically predominated, however, increased deposition may have little detrimental impact on benthic aquatic life.

Suspended sediment causes the water to be cloudy (turbid). Increased turbidity reduces light transmission (and hence photosynthesis ), thereby reducing the growth of algae and aquatic plants, which can adversely affect the entire aquatic ecosystem . Moreover, increased turbidity decreases the water's aesthetic appeal and the human enjoyment of recreational activities. If the river cross-section is sufficiently reduced by sediment buildup, sedimentation can increase downstream flooding. In addition, some metal ions , pesticides , and nutrients may adhere to sediment particles and be transported downstream.

Increased sediment in surface-water bodies (e.g., rivers, lakes, and reservoirs) may have an economic impact on public water systems that use them as a source of drinking water. High turbidity not only is aesthetically displeasing, but also interferes with disinfection of the water prior to it being pumped to customers. Communities whose water-supply source has become more turbid often invest millions of dollars to upgrade their treatment facilities in order to remove the increased sediment load.

Preventive Measures and Erosion Control

During the last 40 years of the twentieth century, nearly one-third of the world's arable land was lost to erosion, and topsoils continue to be lost at a nonsustainable rate (i.e., faster than it can be naturally restored). In the United States, the Midwest experiences some of the highest erosion rates, with some states losing between 7 and 10 tons of soil per acre annually.

Water quality can be protected by controlling and minimizing erosion. State and federal laws provide some consideration of erosion and sedimentation control along streams and lakes during flood control, drainage, highway, bridge, and other stream-related construction projects. A variety of programs administered by public and private agencies encompass research projects, education programs, technical assistance, regulatory measures, and cost-share financial assistance for erosion control.

Coordinated efforts by federal and state agricultural programs have been helping reduce the amount of soil erosion and sedimentation. Farmers now utilize a variety of conservation practices to reduce erosion and limit sedimentation, such as conservation tillage methods, use of conservation buffers and riparian habitat, and establishment of conservation easements. The Natural Resource Conservation Service, state and local conservation districts, and other organizations play critical roles in preserving cropland productivity and limiting adverse water quality impacts.

Preventive measure for reducing excessive sediment load in streams include:

  • Proper repair and maintenance of drainage ditches and levees;
  • Minimal disturbance of the streambanks;
  • Avoidance of structural disturbance of the river;
  • Reduction of sediment excesses arising from construction activities;
  • Application of artificial and natural means for preventing erosion; and
  • Use of proper land and water management practices on the water-shed.

These preventive measures are preferred over remedial measures, which include:

  • Construction of detention reservoirs, sedimentation ponds, or settling basins;
  • Development of side-channel flood-retention basins; and
  • Removal of deposited sediment by dredging.

see also Beaches; Coastal Ocean; Forest Hydrology; Land Use and Water Quality; Land-Use Planning; Pollution of Lakes and Streams; Pollution Sources: Point and Nonpoint; Runoff, Factors Affecting; Stream Channel Development; Stream Erosion and Landscape Development; Weathering of Rocks.

William Arthur Atkins


Tarbuck, Edward J., and Frederick K. Lutgens. The Earth: An Introduction to Physical Geology, 6th ed. New York: Prentice Hall, 1998.

Troeh, Frederick R., Roy L. Donahue, and J. Arthur Hobbs. Soil and Water Conservation. New York: Prentice Hall, 2000.

Internet Resources

The State of the Soil. Soil and Water Conservation Society. <>.

Water Erosion. Intermountain Resource Inventories, Inc. <>.

* See "Beaches" for a photograph of erosion damage to houses built on sandy ground.

* See "Forest Hydrology" for a photograph of rill and gully erosion on a burned slope.

* See "Land Use and Water Quality" for a photograph of an unvegetated streambank adjoining an agricultural field.

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