Loess (, , , or ) is an aeolian sediment formed by the accumulation of wind-blown silt, typically in the 20–50 micrometre size range, and lesser and variable amounts of sand and clay that are loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs.

The word loess, with connotations of origin by wind-deposited accumulation, is of German origin and means “loose.” It was first applied to Rhine River valley loess about 1821.

Properties

Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non-stratified and often calcareous. Loess grains are angular with little polishing or rounding and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil.

Loess deposits may become very thick; more than a hundred meters in areas of China and the Midwestern United States. It generally occurs as a blanket deposit that covers areas of hundreds of square kilometers and tens of meters thick.

Loess often stands in either steep or vertical faces. Because the grains are angular, loess will often stand in banks for many years without slumping. This soil has a characteristic called vertical cleavage which makes it easily excavated to form cave dwellings, a popular method of making human habitations in some parts of China. Loess will erode very readily.

In several areas of the world, loess ridges have formed that are aligned with the prevailing winds during the last glacial maximum. These are called paha ridges in America and greda ridges in Europe. The form of these loess dunes has been explained by a combination of wind and tundra conditions.

Etymology

''Loess'' comes from the German ''Löss'' or ''Löß'', and ultimately from Alemannic ''lösch'' meaning ''loose'' as named by peasants and masons along the Rhine Valley.

Formation

Periglacial Loess

Periglacial (Glacial) loess is derived from the floodplains of glacial braided rivers that carried large volumes of glacial meltwater and sediments from the annual melting of continental icesheets and mountain icecaps during the summer. During the fall and winter, when melting of the icesheets and icecaps ceased, the flow of meltwater down these rivers either ceased or was greatly reduced. As a consequence, large parts of the formerly submerged and unvegetated floodplains of these braided rivers dried out and were exposed to the wind. Because these floodplains consist of sediment containing a high content of glacially ground flour-like silt and clay, they were highly susceptible to winnowing of their silts and clays by the wind. Once entrained by the wind, particles were then deposited downwind. The loess deposits found along both sides of the Mississippi River Alluvial Valley are a classic example of periglacial loess.

Non-glacial

Non-glacial loess can originate from deserts, dune fields, playa lakes, and volcanic ash.

Some types of nonglacial loess are:

Volcanic loess in Ecuador and Argentina.

Tropical loess in Argentina, Brazil and Uruguay.

Gypsum loess in Spain.

Trade wind loess in Venezuela and Brazil

Anticyclonic loess in Argentina.

The thick Chinese loess deposits are non-glacial loess having been blown in from deserts in northern China. The loess covering the Great Plains of Nebraska, Kansas, and Colorado is non-glacial desert loess. Non-glacial desert loess is also found in Australia. and Africa

Fertility

Loess tends to develop into highly rich soils. Under appropriate climatic conditions it is some of the most agriculturally productive terrain in the world.

Soils underlain by loess tend to be excessively drained. The fine grains weather rapidly due to their large surface area making soils derived from loess very rich. One theory states that the fertility of loess soils is due largely to electron exchange capacity (the ability of plants to absorb nutrients from the soil) and porosity (the air-filled space in the soil). The fertility of Loess is not due to organic matter content, which tends to be rather low unlike tropical soils, which derive their fertility almost wholly from organic matter.

Even well managed loess farmland can experience dramatic erosion of well over 2.5 kg per square meter per year. Although in geological time loess has an incredible rate of erosion, in a more human time scale loess is durable and resistant to maltreatment. In China loess deposits along the Yellow River have been farmed and have produced phenomenal yields for over one thousand years. A large amount of the credit for this goes to the farmers; Chinese farmers were the first to practice active erosion control. The largest deposit of loess in the United States, the Loess Hills along the border of Iowa and Nebraska, has survived intensive farming and poor farming practices. For almost 150 years this loess deposit was farmed with mouldboard ploughs and fall tilled, both intensely erosive. At times it suffered erosion rates of over 10 kilograms per square meter per year. Today this loess deposit is worked as low till or no till in all areas and is aggressively terraced.

Sites

The Loess Hills of Iowa owe their fertility to the prairie topsoils built by 10,000 years of post-glacial accumulation of organic-rich humus as a consequence of a persistent grassland biome. When the valuable A-horizon topsoil is eroded or degraded, the underlying loess soil is infertile, and requires the addition of fertilizer in order to support agriculture.

The loess along the Mississippi River near Vicksburg, Mississippi consist of three layers. The ''Peoria Loess'', ''Sicily Island Loess'', and ''Crowley's Ridge Loess'' accumulated at different periods of time during the Pleistocene. Ancient soils, called paleosols, have developed in the top of the Sicily Island Loess and Crowley's Ridge Loess. The lowermost loess, the Crowley's Ridge Loess, accumulated during the late Illinoian Stage. The middle loess, Sicily Island Loess, accumulated during early Wisconsin Stage. The uppermost loess, the Peoria Loess, in which the modern soil has developed, accumulated during the late Wisconsin Stage. Animal remains include terrestrial gastropods and mastodons.

Loess soil forms sharp hills east of the Mississippi River and Yazoo River in western Mississippi north and south of Vicksburg. These deposits are more than 30 m thick (comparable to those in Iowa) immediately above the river valleys, to which they are sub-parallel, and thin to trace thickness within 40 km to the east. Streams and gulleys are incised very deeply and sharply between the linear loess ridges making topography very important in the conduct of military operations for the Vicksburg Campaign.

The Palouse Hills of eastern Washington and northern Idaho is a fertile agricultural region based on loess deposits.

Glacial loess from the Matanuska Glacier blown into Matanuska Valley created the fertile soil conditions that motivated the Matanuska Colony resettlement experiment in Alaska during the Great Depression.

The Loess Plateau (simplified Chinese: 黄土高原; traditional Chinese: 黃土高原; pinyin: huángtǔ gāoyuán), also known as the Huangtu Plateau, is a plateau that covers an area of some 640,000 km² in the upper and middle of China's Yellow River and China proper. The soil of this region has been called the "most highly erodible soil on earth". The Loess Plateau and its dusty soil cover almost all of Shanxi, Shaanxi, and Gansu provinces, the Ningxia Hui Autonomous Region, and parts of others.

Hungary has several areas that are covered by loess. At locations such as Dunaújváros and Balatonakarattya, loess walls are exposed as loess reefs. Similar formations exist in Romania (Wallachian Plain) and in Bulgaria on the south bank of the Danube.

Central Belgium is covered by thick loess stacks. Neanderthal artifacts were found within the soils between the loess layers of the Veldwezelt-Hezerwater.

Crowley's Ridge in Arkansas is a natural loess accumulation point.

See also

Loam

References

External links

2006, ''The Secret of China’s Vast Loess Plateau'' Suburban Emergency Management Project, Chicago, Illinois.

2007, ''New European Loess Map.'' Helmholtz Centre for Environmental Research, Leipzig, Germany.

''Glacial Deposits: Loess and Till.'' Illinois State Museum, Springfield, Illinois.

Briedis. C.A., 2006, ''Loess Thickness Map (of Illinois).'' Illinois State Geological Survey, Champaign, Illinois.

Gill, T.E., A. Warren, and J.E. Stout, 2008, ''The Bibliography of Aeolian Research.'' Cropping Systems Research Laboratory, U.S. Department of Agriculture, Lubbock, Texas.

Heinrich, P.V., 2008, ''Loess map of Louisiana.'', Public Information Series. no. 12, Louisiana Geological Survey, Baton Rouge, Louisiana.

Prior, J.C., and D.J. Quade, nd, ''The Loess Hills: A Geologic View.'' Iowa Geological Survey, Department of Natural Resources, Iowa City, Iowa.

U.S. Geological Survey, 1999, ''Geology of the Loess Hills, Iowa''

U.S. Geological Survey, 2006, ''Eolian History of North America'' Why is loess important to study?

''The Loess Hills of Western Iowa''

''The Loess Hills of Roztocze''

Category:Pedology Category:German loanwords Category:Glaciology Category:Sedimentary rocks Category:Sediments Category:Types of soil Category:Aeolian landforms

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