Cuernos del Paine — mountain
Image by jmarti20 from Pixabay

Cuernos del Paine

  • 2 min read
  • 51.002° S 73.012° W

Interesting facts

  • Paine is generally said to mean 'blue' in the Tehuelche language, a reference to the vivid lakes around the massif.
  • Uranium-lead dating of crystals in the granite gives ages of about 12.5 million years.
  • The pale granite sits on a grey gabbro-diorite body; together they form a laccolith, a mushroom-shaped intrusion that lifted the rock above it.
  • The first ascent of Cuerno Principal was made by Aguilera, García, Latorre and Oyarzún, climbing the southwest ridge.
  • Cuerno Norte fell in 1971 to a party of six climbers, three years after the main horn.
  • Cuerno Este resisted until 2022, when Jurado, Marcotti and Pelletti reached it by a route graded 5.11-, some 54 years after the first horn was climbed.
  • Though only 2,600 metres high, the summit stands in a tundra climate zone under the Köppen classification.

Why it is worth it

The Horns of Paine are the most arresting silhouette in Chilean Patagonia: a jagged row of towers rising about 2,600 metres, their lower walls of pale grey granite abruptly capped by bands of almost black rock, as if someone had set dark hats on the peaks. From the shore of Lake Nordenskjöld the summit rises more than 2,500 metres in a horizontal distance of only two and a half kilometres, and the contrast of pale stone, dark caps, turquoise water and yellow steppe is the image most people carry away from Torres del Paine National Park.

The two-tone look is a geological snapshot. Around 12 to 13 million years ago a body of magma pushed up and spread sideways between layers of older mudstone and sandstone, cooling into granite and gabbro-diorite; the heat baked the surrounding sediments into dark metamorphic rock. Erosion later stripped away most of the covering layers, leaving the dark remnants perched on top of the granite. Dating of the intrusion shows that the whole body of magma was emplaced and crystallised in a geologically brief span of roughly 160,000 years, which is why the contact between light and dark is so clean and sharp.

The Cuernos have a climbing story as dramatic as their shape. The main horn, Cuerno Principal, was first climbed on 31 January 1968 by a party of four from Santiago; Cuerno Norte followed on 30 December 1971, while Cuerno Este held out until 19 January 2022. For walkers the massif is the centrepiece of the treks around the Paine range, and one of the most rewarding short outings leads from Pudeto past the Salto Grande, the waterfall where Lake Nordenskjöld spills into Lake Pehoé, to the Mirador Cuernos, a viewpoint about three kilometres on that looks straight up at the horns across the lake. The wind here is fierce and constant, and the southern summer, December to February, brings the mildest conditions.

Getting there

The Cuernos stand in Torres del Paine National Park, about 90 km north-west of Puerto Natales, the usual base for the park. Teniente Julio Gallardo Airport (PNT) at Puerto Natales is roughly 80 km away. The Mirador Cuernos walk starts at Pudeto, where there is parking and a small café and from where the catamaran crosses Lake Pehoé to Paine Grande.

Plan your visit

We have no confirmed visit data yet. Once it is confirmed, this block also carries the date it was checked.

Nearby places

On these lists

From the encyclopaedia

Cuernos del Paine is a mountain in the Magallanes Region of Chile.

Wikipedia · CC BY-SA 4.0

-51.00243, -73.01190per Wikidata