Chilean Coast Range
The Chilean Coastal Range () is a mountain range that runs from north to south along the Pacific coast of South America parallel to the 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 to grazing and silviculture. The range is present in all Chilean regions except for Coquimbo Region and Magallanes Region.
Chilean Central Valley
In northernmost Chile the central valley is made up of the Pampitas, a series of small flats dissected by deep valleys. Immediately south of the Pampitas, in Tarapacá Region and northern of Antofagasta Region, the Central Valley is known as Pampa del Tamarugal. Contrary to the Pampitas valleys descending from the Andes do not incise the plains but merge into the surface of Pampa del Tamarugal at a height of "c". 1500 m. The westernmost portion of Pampa del Tamarugal has a height of 600 m. This western part contain a series of raised areas called "pampas" and basins containing salt flats. Interconnecting basins are important corridors for communication and transport in northern Chile.