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.
Natural regions of Chile
Covers all of Chilean Patagonia, and the Chiloé Archipelago. Zona austral has a subpolar oceanic climate and a vegetation of Magellanic subpolar forests in the west and Patagonian grasslands in the east. The former Patagonian Ice Sheet have eroded the coast range so that it now of islands and is not present south of Taitao Peninsula. The Intermediate depression is under the sea level. Fjords penetrate the Andes where there are also two ice sheets and several glacial lakes.