Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Torres del Paine

Inselbergs and Crystalline Monoliths

The Torres del Paine are three granite peaks, or torres, rising to nearly 2,850 meters in Torres del Paine National Park in Chilean Patagonia, formed from a body of granite, called the Paine Pluton, that intruded into and slowly cooled beneath overlying sedimentary rock roughly 12 million years ago. Later uplift of the southern Andes exposed the pluton at the surface, and the intense glacial erosion of repeated ice ages carved away the softer surrounding sedimentary rock and sculpted the harder granite into the towers' steep, near-vertical faces, leaving a dark sedimentary cap still visible atop some of the peaks. The towers are considered a classic example of glacially exposed granite batholith topography and give the national park its name, Paine, from a local word for blue, describing the color of the surrounding mountains.

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Glaciation, Processes

In Discipline

In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Torres del Paine
Sources
1. Cordillera Paine (Wikipedia)
Lead section
Quote, Lead section
The Cordillera Paine is a group of mountains (a cordillera) in Torres del Paine National Park in Chilean Patagonia. It is 280 km (170 mi) north of Punta Arenas, and about 1,960 km (1,220 mi) south of the Chilean capital Santiago.
View the Source
Wikidata: Torres del Paine
Wikidata Q124305089, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.