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Cordillera

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cordillera [‚kȯrd·əl′er·ə]
(geography)
A mountain range or group of ranges, including valleys, plains, rivers, lakes, and so on, forming the main mountain axis of a continent.

Cordillera 

a narrow island ridge (an archipelago of small, usually rocky islands), corresponding to the arch section of a developing geanticlinal uplift. Cordilleras appear in the early state of the development of a geosyncline. They occur most extensively during the final stage of development of the geosyncline, disappearing as independent formations when uplifts begin to predominate, that is, during the state of orogeny. The term was introduced by the Swiss geologist E. Argand in 1916 and was first used in Russian geological studies by V. P. Rengarten in 1926.



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We ascend the lofty peaks of the Cordillera and we find an alpine species of bizcacha; we look to the waters, and we do not find the beaver or musk-rat, but the coypu and capybara, rodents of the American type.
In a lofty valley of the Cordillera, near Mendoza, I found another spider with a singularly-formed web.
Some occur among the Cordilleras of the Andes, where cities, and towns, and cultivated farms are to be seen eight thousand feet above the level of the sea.
 
 
 
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