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The Atacama Desert - Miscellaneous Notes
summary from 'Deserts - a miracle of life' by Jim Flegg (Blandford Press - 1993)

South America has two main deserts, the Atacama and the Patagonian Deserts, both along its Pacific coastline, with the Andes as their natural boundary in the east.

The Atacama Desert is the more northerly and lies mainly in Peru and Chile, stretching from the Equator to about 20o South, some 3,000 km (1875 miles) in length and rarely more than 200 km (125 miles wide).  The Andes, with heights of up to 6,000 m (19,700 ft) effectively block the passage of moist tropical air from the Amazon Basin, shedding their moisture as rainfall when they rise over the Amazonian Andes foothills.

Along the coast, the cold waters of the Humboldt Current that originate in the Antarctic, flow north.  The cold water and the air above it causes a thermal inversion that dries the air, condensing any remaining moisture into insubstantial short-lived mists, the Camanchaca.

The Atacama is often said to be the driest desert in the world, enduring continuous draught for many years in succession.  There are no significant subterranean moisture reserves, and where they are found, the water is heavily contaminated with boron that is toxic to most forms of life.  It is a mineral rich area, particularly in deposits of sodium nitrate that together with guano gathered from the off-shore seabird colony islands were a significant source of the world's agricultural fertilizer industry up to the 1920s.

At some locations the Atacama is a low, arid coastal plateau, while over a considerable proportion a range of low mountains rise as cliffs of up to 450 m. height from the ocean, increasing in height to rocky crags towering to 2,000 m.  Behind these mountains is found a valley corridor that reaches up to the Andean foothills.  The coastal hills prevent water flowing down from the Andes from reaching the Pacific, so that their waters evaporate, leaving large salt pans surrounded by alluvial fans from the mountains, consisting mainly of pebble and gravel, with some sand desert areas with typical dune formations.  Occasional volcanic cones rise from this barren moonscape. The surface layer of soil can best be described as volcanic in origin and often broken down into small particles, 'sandy', in texture 

Animal life is scarce.  Infrequently the Andean Condor can be seen high up in the sky on the lookout for carrion.  In the cactus areas, the cactus wren can be found while elsewhere the oven bird, a South American endemic, builds its dome shaped mud nests on stumps or posts.

The dominant animal group consists of lizards, including a number of colourful pot-bellied species of Iguana.  One of the species can reach lengths of up to 2 m and although fierce and dragon-like in appearance, is actually a quite timid scavenger.

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