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Tipas
EntityQ422807· pop 22· linked from 26 articles

Cerro Walther Penck (also known as Cerro Cazadero or Cerro Tipas) is a massive complex volcano in the Andes, located in northwestern Argentina, Catamarca Province, Tinogasta Department, at the Puna de Atacama. It is just southwest of Ojos del Salado, the highest volcano in the world. Walther Penck itself is perhaps the third highest active volcano in the world.

Key facts

Mountain.name
Walther Penck
Mountain.other_name
Tipas or Cazadero Grande
Mountain.photo
cazadero.jpg
Mountain.photo_caption
Cazadero (or Tipas) from the east
Mountain.elevation_m
6670
Mountain.location
Argentina
Mountain.range
Puna de Atacama, Andes
Mountain.parent_peak
Ojos del Salado
Mountain.map
Argentina
Mountain.relief
1
Mountain.map_size
230
Mountain.label_position
right
Mountain.type
Complex volcano
Mountain.age
Holocene
Mountain.last_eruption
Unknown
Mountain.first_ascent
14/12/1970 - Sergio Kunstmann, Pedro Rosende (Chile) and Takaya Takeshita (Japan)
Mountain.easiest_route
Hike, east side from El Arenal

via Wikipedia infobox

Wikidata facts

Elevation
6658
Image
Cazadero.jpg
Sources (1)

via Wikidata · CC0

~2 min read

Article

5 sections
Contents
  • Vulcanism
  • Elevation
  • See also
  • External links
  • References

Cerro Walther Penck (also known as Cerro Cazadero or Cerro Tipas) is a massive complex volcano in the Andes, located in northwestern Argentina, Catamarca Province, Tinogasta Department, at the Puna de Atacama. It is just southwest of Ojos del Salado, the highest volcano in the world. Walther Penck itself is perhaps the third highest active volcano in the world.

==Vulcanism== alt=View of the main summit from central summit plateau|thumb|View of the main summit from central summit plateauThe complex covers a surface area of , it consists of stratovolcanoes, lava domes, and lava flows. There are reports of fumarolic activity, and de Silva and Francis (1991) considered that the volcano was last active in the Holocene. Crater lakes with a smell of sulfur were reported in 2013. The Tipas-Cerro Bayo complex was active 2.9-1.2 million years ago with dacites and rhyolites. Magma composition is typical for Andean stratovolcanoes. Tomographic studies of the underlying crust indicate a pattern of seismic attenuation beneath Tipas.

Gallery (2)

On the map

3 mapped locations

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