Destruction of Amazonian Rainforest and its effect on the environment

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Destruction of Amazonian Rainforest

This area of the Amazon rain forest has been cleared by burning, following which a ground cover of small plants grew quickly, but could not prevent the rapid erosion of the soil by rain water, the signs of which can be seen in the channels leading down to the central gully. The fast erosion of already nutrient-poor soil makes regeneration of the forest an even more precarious prospect.

Anne LaBastille/Bruce Coleman Inc

Deforestation, the large-scale removal of forest, prior to its replacement by other land uses. It is proceeding at about 17 million hectares each year (170,000 sq km or 65,000 sq mi, an area larger than England, Wales, and Northern Ireland combined). Between 1980 and 1990, annual deforestation rates were 1.2 per cent in Asia and the Pacific, 0.8 per cent in Latin America, and 0.7 per cent in Africa. Forest area is generally stable in Europe and North America, although the rate of transition from old-growth forest to other forms in North America is controversially high.

Deforestation may be distinguished from forest degradation, which is a reduction in forest quality. The two are linked, and result in several problems. They cause soil erosion and watershed destabilization, resulting in flooding or drought. They reduce biodiversity (the range of habitat, species, and genetic types), particularly significant in tropical forests which are home to much of the world's biodiversity. The culture and knowledge of many forest peoples have evolved through centuries of nurturing the forest; they are diminishing as forest area reduces, access to forest is increasingly restricted, and traditional rights are eroded by governments. Deforestation affects the livelihoods of between 200 and 500 million people who depend on forests for their food, shelter, and fuel. Deforestation and degradation may contribute to regional and global climate imbalances. Forests play a major role in carbon storage; with their removal, excessive carbon dioxide in the atmosphere may lead to global warming, with many problematic side-effects.

While deforestation is now viewed as a problem, historically it was considered to assist national development. Natural forest “capital” was liquidated and replaced by other forms of capital to produce food, raw materials, energy, or infrastructure.

Agriculture in temperate regions has depended upon forest removal, capitalizing upon forest soil fertility. Most of England's woodlands were deforested by 1350. In continental Europe and North America, deforestation accelerated in the 18th and 19th centuries to clear land to grow food for industrial cities, and to meet fuel and construction needs. Rising agricultural productivity has since allowed much temperate farmland to revert to forest. From a low of 5 per cent in 1900, the United Kingdom's forest and woodland area is now 10 per cent.

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Deforestation processes are, in general, more destructive in the tropics. Most forest soils in the tropics are far less fertile than temperate soils, and are erodible. This is because high rainfall leaches out nutrients from the soil, preventing them from building up. However, colonial policies were based on the mistaken assumption that lush forests were on fertile soils. They aimed to “conquer” the forests, principally for cash crop plantations and agriculture; and have left a legacy of exhausted soils.

Tropical deforestation increased rapidly after 1950, helped by the availability of heavy machinery. Since then, rising human populations have also cleared ...

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