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Geological Formation

Chilean Central Valley

Structural and Tectonic Formations

The Chilean Central Valley, also called the Intermediate Depression or Longitudinal Valley, is a depression running north to south between the Chilean Coastal Range and the Andes. It extends from the border with Peru to Puerto Montt in southern Chile and contains many of the country's most populous cities, including Santiago, Temuco, Rancagua, Talca and Chillan. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Chilean Central Valley

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Chilean Central Valley
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Chilean Central Valley
Sources
Chilean Central Valley (Wikipedia)
Lead section
Quote, Lead section
The Central Valley (Spanish: Valle Central), Intermediate Depression, or Longitudinal Valley is the depression running north to south between the Chilean Coastal Range and the Andes Mountains.
View the Source
Wikidata: Chilean Central Valley
Wikidata Q1031793, class allow-list match (w-wdresolver-0926)View the Source
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