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Erosion

Erosion

The surface of the earth is continually being worn away by natural geologic processes. The displace­ment of this weathered material is called . Agents such as water, wind, ice, and gravity work to level the land surfaces of the earth across vast expanses of geologic time. The shapes of conti­nents constantly change as waves and tides cut into old land, while rivers deposit silt and build new land. Erosion eventually wears away moun­tains, but movements of the crust and volcanic activity raise new ones. Although erosion is gener­ally a slow and gradual process that occurs over thousands or millions of years, human activity greatly increases the rate of erosion on fertile land. Farming, mining, and industrial development are all ultimately destructive processes.

Types of Erosion

There are two major categories of erosion: geo­logic erosion and . Geologic erosion is initiated by the weathering of rock. Weathering can be caused by natural physical or chemical means. Heat from the sun may expand the upper­most layer of rock, causing cracking on the sur­face. Wind and rain then carry the particles away, completing the erosion process. In damp climates, minerals in the rock can react chemically with rainwater, causing the rock to gradually dissolve or decompose. Cold climates will cause water that has seeped into crevasses to freeze and expand, splitting rock at the surface. Roots of nearby plants may also grow into cracks and cause fur­ther breaking. Water is a very powerful erosional agent. Running water in streams and rivers not only wears away or dissolves rock but also can carry stones that cause further abrasion along the banks. Glaciers pick up and carry away all loose surface material. When the ice melts, only bare rock remains. Ocean currents and waves erode coastlines, sometimes carving into cliffs and other times depositing sandy beaches.

erosion on uninhabited, untouched land is balanced by soil formation. Soil is protected by natural vegetation. Trees, shrubs, and grasses serve as windbreaks and protect the soil from the force of the rain. Roots hold soil in place. Unfortunately, many human activities involve removing the vege­tation from the land. Agriculture, logging, con­struction, mining, and heavy animal grazing all greatly increase the rates of erosion. Some histori­ans believe that soil erosion is partially responsible for population shifts and the collapse of some civi­lizations throughout history. Ruins of cities with agricultural artifacts have been found in arid des­erts, demonstrating that farming was widespread in these areas in the distant past.

Rates of Erosion

Over geologic time, approximately the past 500 million years, there has been about 60 feet of ero­sion each million years. Currently, in areas of the United States being eroded by human agricultural activity, erosion is occurring at a calculated 1,500 feet per million years. The rate is even higher in other parts of the world. Soil formation varies, but it takes about 10,000 years for 1 foot of top­soil to form. Today, approximately 40% of the world’s agricultural land is seriously degraded, The resulting in lower productivity and poorer crop quality. Virtually all arable land is in use.

Slowing Erosion Rates

Erosion is recognized as a serious problem. Judicious farming practices can greatly reduce erosion rates. Less disruptive tilling methods are being developed. Leaving plant debris in fields after harvest protects the soil and provides shelter for the creatures that assist in soil formation. Strips of land planted with trees and shrubs are left between fields to form windbreaks. Perennial crops that leave root systems in the soil over the winter also hold the soil in place. Contour plow­ing and terracing the land also help limit erosion. Urban developers can plan green space and replant vegetation after the construction process is completed.

A certain amount of erosion is both natural and healthy for an ecosystem. However, the huge pop­ulation growth experienced in the past few centu­ries has put a great deal of stress on the surface of our planet. The availability of rich soil will be critical if we expect to feed future generations. There is unnecessary soil loss happening on every continent right now. Soil conservation programs can substantially reduce the loss of this basic, yet critical, resource. With careful planning, erosion can be minimized and the earth will remain a pro­ductive place for the generations to come.

Jill M. Church

See also Ecology; ; Glaciers; Sedimentation

Further Readings

Cattermole, P. J. (2000). Building planet Earth: Five billion years of earth history. Cambridge, UK: Cambridge University Press.

McNeill, J. R., & Winwarter, V. (2006). Soils and societies: Perspectives from environmental history. Isle of Harris, UK: White Horse Press.

Montgomery, D. R. (2007). Dirt: The erosion of civilizations. Berkeley: University of California Press.

Skinner, B. J., & Porter, S. C. (2004). Dynamic Earth: An introduction to physical geology. Hoboken, NJ: Wiley.

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Johannes Scotus Eriugena

Johannes Scotus Eriugena

Eschatology

Eschatology