Search results
Results from the WOW.Com Content Network
Cono de Arita in Salar de Arizaro. Located in the central-western area of the Puna de Atacama, it covers an area of 1,600 km 2. [4] Per extension, the Salar de Arizaro is the 6th largest salt flat in the World and the 2nd largest in Argentina after the Salinas Grandes.
Many visit the Cachi mountains and the villages (such as Payogasta) around it. There are three national parks in Salta: El Rey National Park in the Yungas jungle, Baritú National Park and Los Cardones National Park. The Train to the Clouds one of the highest railways in the world, taking its way across the high peaks of the Cordillera de los ...
Salar del Hombre Muerto (transl. Salt Pan of the Dead Man) is a salt pan in Argentina, in the Antofagasta de la Sierra Department [2] on the border between the Salta and Catamarca Provinces. [3] It covers an area of 600 square kilometres (230 sq mi) and is in part covered by debris.
Pages in category "Salt flats of Argentina" ... Salinas Grandes (Jujuy and Salta) This page was last edited on 25 December 2016, at 21:18 (UTC). ...
The $870 million project in the northern province of Salta puts Argentina, the world's No. 4 lithium producer, in the spotlight ahead of projects due online in the country in the coming months ...
The Salinas Grandes are located in the north in the provinces of Jujuy and Salta (in Argentina), at an average altitude of 3,450 meters (11,320 feet) above sea level. It covers an area of 212 km 2 (82 sq mi) and is well-known for its vast white desert. [1]
Salinas Grandes seen from the RN 60. The Salinas Grandes ('Salina' is a spanish word for salt flat) is a large salt flat in central-northern Argentina, spanning the borders of four provinces (Córdoba, Catamarca, La Rioja and Santiago del Estero), at an average altitude of 180 metres (590 ft) above sea level, and having an area of about 4,700 km 2.
The salt flat contains systems of oncoids that grow in the interface between proper salt flat and an adjacent wetlands. [1] The geology surrounding the southern part of Salar de Antofalla is made up of continental (e.i. non-marine) sedimentary rock that deposited from Late Eocene to Early Pleistocene times.