Online Encyclopedia

DESERT OF ATACAMA

Online Encyclopedia
Originally appearing in Volume V02, Page 822 of the 1911 Encyclopedia Britannica.
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DESERT OF ATACAMA  , an arid, barren and saline region of western South
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America, covering the greater
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part of the Chilean provinces of Atacama and
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Antofagasta, the
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Argentine territory of Los
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Andes, and the south-western corner of the Bolivian department of
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Potosi . The higher elevations are known as the Puna de Atacama, which is practically a continuation southward of the
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great pupa region of Peru and
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Bolivia . It is a broken, mountainous region, volcanic in places, saline in others, and ranges from 7000 to 13,500 ft. in general
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elevation . Its culminating ridges are marked by an irregular
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line of peaks and
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extinct volcanoes extending north by east from about 28° S. into
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southern Bolivia . On the eastern side, occasional rainfalls occur and streams from the snow-clads peaks produce some slight displays of fertility, but the general aspect of the plateaus, which are dry and cold in winter and in summer are swept by rain-storms and covered by occasional tufts of coarse grass, is barren and forbidding . They are also broken by great saline lagoons and dry salt basins . This region forms the Argentine territory of Los Andes and is habitable in places . On the western slope the
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land descends gradually to the Pacific, being broken into great basins, or terraces, by mountainous ridges in its higher elevations, widening out into gently-sloping sandy plains below, famous for their nitrate deposits, and terminating on the coast with sharply-sloping bluffs, having an elevation of 80o to 1500 ft., and looking from the sea like a range of flat-topped hills . This desolate region, which is rainless and absolutely barren, and was considered worthless for three and a
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half centuries, is now a treasure-house of
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mineral
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wealth, abounding in copper,
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silver, lead, nickel, cobalt, iron, nitrates and borax . It is occupied by many
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mining settlements, and includes some of the most productive copper and silver mines of the
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world . See L . Darapsky, " Zur Geographie der Puna de Atacama," Zeits .

Ger . Erdk. zu

Berlin, 1899; G . E . Church, " South America: an Outline of its
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Physical Geography,"
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Geographical Journal, 1901 ; John Ball, Notes of a Naturalist in South America (
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London, 1887); F . O'Driscoll, " A Journey to the North of the Argentine Republic," Geographical Journal, 1904 . (A . J .

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there is only 0.01 cm rain in it.it is said that no rain has fallen in it since 400 years
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