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224:. The western border of Cordillera Domeyko is characterized by a inland cliffs and a sharp topographic transition known as El Bordo Escarpment. El Bordo Escarpment contain the main rock
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220:. It runs north-south for approximately 600 km, parallel to the main chain. The mountain range marks the eastern border of the flat parts of
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Cretaceous to
Paleogene geology of the Salar de Atacama basin, northern Chile: A reappraisal of the Purilactis Group stratigraphy
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262:"Interactions between basement and cover during the evolution of the Salar de Atacama Basin, northern Chile"
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Cordillera de la Sal, part of
Cordillera Domeyko. In the distance can be seen
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239:and is the world's lowest humidity mountain range.
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317:. Fourth ISAG, Goettingen. Goettingen, Germany.
232:, which make up much of the mountain range.
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350:Virtual Tour on 360° of Cordillera de la Sal
292:: CS1 maint: multiple names: authors list (
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111:600 km (370 mi) north-south
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235:Cordillera Domeyko was named after
436:Antofagasta Region geography stubs
379:. You can help Knowledge (XXG) by
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426:Landforms of Antofagasta Region
279:10.4067/S0716-02082002000100004
328:ASTER's Global View from Space
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59:4,278 m (14,035 ft)
260:and Jordan, T. (July 2002).
33:Cerro Quimal in the distance
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266:Revista Geológica de Chile
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431:Mountain ranges of Chile
16:Mountain range in Chile
375:location article is a
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311:Mpodozis, Constantino
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212:located in northern
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373:Antofagasta Region
333:2008-02-22 at the
202:Cordillera Domeyko
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39:Highest point
22:Cordillera Domeyko
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152:24.500°S 69.000°W
130:Range coordinates
87:23.117°S 68.667°W
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218:Salar de Atacama
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222:Atacama Desert
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381:expanding it
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272:(1): 55–80.
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170:Parent range
48:Cerro Quimal
256:Muñoz, N.,
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65:Coordinates
420:Categories
243:References
216:, west of
190:Licancabur
103:Dimensions
116:Geography
55:Elevation
331:Archived
226:outcrops
194:Juriques
175:Central
228:of the
208:of the
143:69°00′W
140:24°30′S
121:Country
78:68°40′W
108:Length
75:23°7′S
371:This
214:Chile
210:Andes
204:is a
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377:stub
294:link
200:The
192:and
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