Endogenetic and Exogenetic Forces and Evolution of Landforms: Some Terms

Endogenetic forces are forces resulting from dynamic processes operating beneath the crust of the Earth. They cause:

  • Diastrophism: Lifting of a large part of the crust in elevation
  • Orogeny: Folding, warping, faulting in the crust which may occur as a result of diastrophism.
  • Volcanism: a process whereby molten rock material from beneath the crust pushes through the crust and builds up the surface of the earth.
  • Exogenetic forces are the forces that work from outside the earth.Landforms (often plains or minor landforms) created from forces outside the earth which act upon the surface and change it.
    • Weathering: the breaking down of rock by chemical and/or mechanical means into smaller particles in preparation for the next two forces.
    • Erosion: the removal of weathered materials from higher elevations by moving water, wind, moving ice, and/or gravity.
    • Deposition: the build up of weathered materials at lower elevations once the force of gravity cannot be overcome by an agent of erosion.

Mountain

Landform that rises prominently above its surroundings, generally exhibiting steep slopes, a relatively confined summit area, and considerable local relief. Mountains generally are understood to be larger than hills, but the term has no standardized geological meaning. Very rarely do mountains occur individually. In most cases, they are found in elongated ranges or chains.

Hill

A usually rounded natural elevation of land lower than a mountain – lower in altitude and having less local relief. It has very little level land surface; however, it is usually much less steep than a mountain.

Plateau

A usually extensive land area having a relatively level surface raised sharply above adjacent land on at least one side sometimes referred to as a tableland.  The steep surface where it rises sharply above the adjacent land is called an escarpment

 Plain

Any relatively level area of the Earth’s surface exhibiting gentle slopes and small local relief. Plains vary widely in size. The smallest occupy only a few hectares, whereas the largest cover hundreds of thousands of square kilometers.The majority of the world’s most extensive plains were formed as a result of the dominance of erosional and depositional processes over tectonic activity—e.g., uplift or subsidence of the Earth’s crust.

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Agricultural Regions of North America

North America benefits greatly from its fertile soils, plentiful freshwater, oil and mineral deposits, and forests. With a strong domestic and export economy focused on this abundant array of natural resources, North America has become one of the most developed regions in the world.

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From the freezing Arctic to the tropical jungles of Central America, North America enjoys more climate variation than any other continent. Almost every type of ecosystem is represented somewhere on the continent, from coral reefs in the Caribbean to the ice sheet in Greenland. These differences contribute to variety of agricultural industries in North America, which are often divided by climate zone: tropical zone, subtropical zone, cool temperate zone, and dry zone.

In the tropical zones of North America, farmers grow oranges, sugar cane, coffee, cocoa, and bananas. These crops grow on coastal plains and humid mountain slopes. Cotton and hemp are cultivated in the warmer and drier intermediate climate zone. These crops are important exports for Central American countries.

Fruits, vegetables, cotton, and tobacco are predominant in the warm, subtropical zones of northern Mexico and the United States. Important agricultural areas in this zone include the Rio Grande Valley (citrus fruits) in the U.S. state of Texas and Mexico, Californias Central Valley (fruits and vegetables), the Gulf Coastal Plain (vegetables), and the sandy valleys of the Appalachians (cotton and tobacco). These areas enjoy the benefit from ample rain and warm air currents.

North American crops include grains, legumes, fruits, vegetables, and plants for clothing and other nonfood uses. The system of businesses associated with agricultural production in an industrialized society is integral part of modern agriculture and the interrelationship works quite well in North America.

In North America, agriculture generally has become mechanized and heavily dependent upon an integrated system of supporting agribusinesses, although traditional practices continue in Mexico. In the United States and Canada, most farmers and ranchers depend heavily upon technology, although groups such as the Amish have rejected automation and continue to use animal power for traction.

Most farmers practice monoculture, relying upon a single crop for their primary income, and have expanded to very large acreages in order to take advantage of economies of scale. Such farms are referred to in terms of the primary crop, for example, a dairy farm, a cattle ranch, or a wheat farm. Some small farms are run by part-time farmers who also have other occupations.

Agricultural Belts

The Dairy Belt, Corn Belt, and Wheat Belt are three agricultural areas in the continents cool temperate zones.

Dairy animals, including cows, goats, and sheep, feed on the hay and hardy small grains that thrive in New England and the Great Lakes-St. Lawrence region along the Atlantic coast. This is the Dairy Belt.

The Corn Belt, located between the Ohio River and the lower Missouri River, receives ample water and strong summer sun, ideal for corn and soybeans.

 West of the Corn Belt, the Wheat Belt stretches from the U.S. state of Kansas through the Canadian Prairie Provinces of Alberta, Saskatchewan, and Manitoba. This vast area of the Great Plains allows wheat to be cultivated in both winter and spring.

Dry zones, common in the southwestern U.S. and northern Mexico, are ideally suited for livestock ranching. Ranches with thousands of cattle are common in this region. Traditionally, livestock fed on locally grown fodder such as prairie grasses. However, irrigation for fruit and cotton farming has drained water supplies in the region. Native grasses cannot nourish the huge herds of livestock kept by ranchers. Cattle, sheep, hogs, and other livestock are less likely to graze than to eat corn-based feed. In fact, most of the corn grown in the Corn Belt is feeder corn used for livestock feed.

Corn Belt

The Corn Belt is a region of the Midwestern United States where corn (maize) has, since the 1850s, been the predominant crop, replacing the native tall grasses. By 1950, 99% of the corn was grown from hybrids. Most corn is fed to livestock, especially hogs and poultry. In recent decades soybeans have grown in importance. The U.S. produces 40% of the world crop.

Geography of corn belt

Geographic definitions of the region vary. Typically, it is defined to include: Iowa, Illinois, Indiana, southern Michigan, western Ohio, eastern Nebraska, eastern Kansas, southern Minnesota and parts of Missouri. As of 2008, the top four corn-producing states were Iowa, Illinois, Nebraska and Minnesota, together accounting for more than half of the corn grown in the United States.The Corn Belt also sometimes is defined to include parts of South Dakota, North Dakota,Indiana, Ohio, Wisconsin, Michigan, and Kentucky. The region is characterized by relatively level land and deep, fertile soils, high in organic matter.[

More generally, “Corn Belt” represents the most intensively agricultural region of the Midwest, connoting a lifestyle based on ownership of family farms, with supporting small towns and powerful farm organizations that lobbied to obtain higher prices.

History of corn belt

In the era from 1860 to 1970, new agricultural technology transformed the Corn Belt from a mixed crop-and-livestock farming area to a highly specialized cash-grain farming area. While the landscape was substantially modified, the family farm remained the standard form. Its acreage doubled, as farmers bought out their neighbors (who then moved to nearby towns). After 1970 increased crop and meat production required an export outlet, but global recession and a strong dollar reduced exports, depressed prices below costs of production, and created serious problems even for the best farm managers.

Vice President Henry A. Wallace, a politician and pioneer of hybrid seeds, declared in 1956 that the Corn Belt developed the “most productive agricultural civilization the world has ever seen”.

Wheat Belt

Wheat Belt, the part of the North American Great Plains where wheat is the dominant crop. The belt extends along a north-south axis for more than 1,500 miles (2,400 km) from central Alberta, Can., to central Texas, U.S. It is subdivided into winter wheat and spring wheat areas. The southern area, where hard red winter wheat is grown, includes parts of the states of Kansas, Oklahoma, Texas, Nebraska, and Colorado. This area is hot and dry in summer and is thus well suited to winter wheat, which is planted in fall, when it draws on moisture provided by autumn rains. Cattle often graze on the young wheat. As the summer heat hits, the wheat ripens and is harvested in July. Hard red spring wheat is grown in parts of Montana, North Dakota, South Dakota, and Minnesota and in the Canadian provinces of Alberta, Saskatchewan, and Manitoba, where the climate is more severe and the winters are too cold for winter wheat. Thus, the wheat is planted in spring and takes advantage of the long summer days of this high-latitude area to mature by fall.

Source(s):

http://nationalgeographic.org/encyclopedia/north-america-resources/

http://lifeofplant.blogspot.in/2011/03/north-american-agriculture.html

First map from Notes of Professor Abdul Munir

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It is Children’s Day: Do You Remember?

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It is another children’s Day (we celebrate Nehru’s Birthday as Children’s Day). As India is in the midst of cash chase, I wonder anyone remembers it. Come let us care about our future in the midst of this mad chase. Further, These days the Gullaks of children are helping the elders. Their dream chest is helping to run home.

soon it will be your turn to fulfill their dreams.

 

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Some Interesting Facts About California

  • Following James Marshall’s discovery of gold at Sutter’s Mill in Coloma in 1848, California’s population leaped from 14,000 to 250,000 in only four years. Between 1850 and 1859, miners extracted 28,280,711 fine ounces of gold.
  • California has the largest economy in the United States and, in 1997, was the first state to reach the trillion-dollar benchmark in gross state product. In 2012, California was ranked the ninth largest economy in the world.
  • California grows more than 3.3 million tons of winegrapes on over 540,000 acres each year and produces roughly 90 percent of all S. wine.
  • The highest and lowest points in the continental United States are located within 100 miles of one another in California: Mount Whitney measures 14,505 feet and Badwater Basin in Death Valley is 282 feet below sea level.
  • Considered to be the hottest, driest place in the United States, Death Valley often reaches temperatures greater than 120 degrees Fahrenheit during the summer and averages only around two inches of rain each year.
  • With a trunk slightly greater than 102 feet in circumference, the General Sherman in Sequoia National Park is the largest living tree (by volume) in the world. It is estimated to be somewhere between 1,800 to 2,700 years old.
  • Southern California has about 10,000 earthquakes each year, although only 15 to 20 of them have a magnitude greater than 4.0.
  • Despite its urbanization and the loss of land to industry, California still leads the country in agricultural production. About one-half of the state’s land is federally owned. National parks located throughout the state are devoted to the preservation of nature and natural resources.
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