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Cerro Vicuña Mackenna
Cerro Vicuña Mackenna is the highest point in the Sierra Vicuña Mackenna and the Chilean Coast Ranges. The peak has a stark desert climate, typical of the Atacama Desert. The peak is named after Benjamín Vicuña Mackenna Benjamín Vicuña Mackenna (August 25, 1831 – January 25, 1886) was a Chilean writer, journalist, historian and politician. Vicuña Mackenna was of Irish and Basque descent. Biography Benjamín Vicuña Mackenna was born in Santiago, the .... References Mountains of Antofagasta Region Three-thousanders of the Andes {{Antofagasta-geo-stub ...
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Chilean Coast Range
The Chilean Coastal Range () is a mountain range that runs from north to south along the Pacific Ocean, Pacific coast of South America parallel to the Andes, Andean Mountains, extending from Morro de Arica in the north to Taitao Peninsula, where it ends at the Chile triple junction, in the south. The range has a strong influence on the climate of Chile since it produces a rain shadow to the east. Because of this the vegetation growing on the seaward slopes is much more exuberant than in the interior. Compared to the coastal lowlands and the Intermediate Depression, it is sparsely populated with land use varying from protected areas of Chile, protected areas to grazing and silviculture. The range is present in all Chilean regions, except for Coquimbo Region and Magallanes Region. Geography Like the Andes, the coastal range becomes progressively lower with increasing latitude. The range begins at Morro de Arica in the north and reaches its highest point, of above sea level, in Sier ...
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Atacama Desert
The Atacama Desert () is a desert plateau located on the Pacific Ocean, Pacific coast of South America, in the north of Chile. Stretching over a strip of land west of the Andes Mountains, it covers an area of , which increases to if the barren lower slopes of the Andes are included. The Atacama Desert is the driest nonpolar desert in the world, and the second driest overall, behind some specific spots within the McMurdo Dry Valleys. It is the only Desert climate, true desert to receive less precipitation than polar deserts, and the largest fog desert in the world. The area has been used as an experimentation site for Mars expedition simulations due to its similarities to the Martian environment. The constant Inversion (meteorology), temperature inversion caused by the cool north-flowing Humboldt Current, Humboldt ocean current and the strong South Pacific High, Pacific anticyclone contribute to the extreme aridity of the desert. The most arid region of the Atacama Desert is s ...
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Benjamín Vicuña Mackenna
Benjamín Vicuña Mackenna (August 25, 1831 – January 25, 1886) was a Chilean writer, journalist, historian and politician. Vicuña Mackenna was of Irish and Basque descent. Biography Benjamín Vicuña Mackenna was born in Santiago, the son of Pedro Félix Vicuña and Carmen Mackenna Vicuña, and grandson of General Juan Mackenna, hero of the Chilean War of Independence. He studied in Santiago, and joined the school of law in 1849. From the beginning of his career he contributed to ''La Tribuna'' newspaper, writing political articles. In 1851 he participated in Pedro Urriola's revolution against the government but was taken prisoner during the attack on the headquarters of the Chacabuco Regiment. On 4 July 1851 Vicuña Mackenna and Roberto Souper managed to escape from the prison disguised as women. In 1852 he lived in exile in the United States, and travelled from San Francisco through Mexico and Canada. A year later he studied agronomy in England, and then visited man ...
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Mountains Of Antofagasta Region
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountai ...
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