
Parinacota Volcano
Arica y Parinacota
Parinacota Volcano is a dormant stratovolcano situated on the border between Bolivia and Chile, forming part of the Nevados de Payachata volcanic chain alongside Pomerape. It rises to an elevation of 6,380 meters (20,930 feet), featuring a strikingly symmetrical cone capped by a summit crater approximately one kilometer wide. The volcano's southern slopes host three parasitic Ajata cones that have produced lava flows. Parinacota's growth began during the Pleistocene epoch, with a significant western flank collapse occurring between the Pleistocene and Holocene, creating a vast landslide deposit that altered local drainage and expanded Lake Chungará. Subsequent volcanic activity rebuilt the cone, erasing the collapse scar. Throughout the Holocene, Parinacota experienced numerous effusive and explosive eruptions, with the most recent about 200 years ago. While no recorded eruptions exist, Aymara local legends suggest eyewitness accounts of volcanic activity. The volcano lies within the Central Volcanic Zone of the Andes, a region characterized by thick crust and active volcanism due to the subduction of the Nazca and Antarctic Plates beneath South America. Its name derives from the Aymara language, meaning "flamingo lake," reflecting the local fauna and geography. Despite its dormant status, Parinacota remains a prominent natural landmark with potential for future activity, though the area's low population density limits risk to human settlements.
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Astuce: Visitors should consider the dry season months for clearer weather and safer access to the high-altitude volcano. Due to its remote location and challenging terrain, proper acclimatization and physical preparation are essential. It is advisable to arrange guided tours with local experts familiar with the region. While there are no official recorded eruptions, awareness of volcanic activity warnings is prudent. Purchasing any necessary permits or arranging transport in advance is recommended, as infrastructure is limited. Discounts may be available for groups or students through local agencies.
Faits intéressants
- •Parinacota and Pomerape are known as the Nevados de Payachata, meaning 'twins,' due to their similar appearance.
- •The western flank collapse created a large hummocky landslide deposit that altered regional drainage and led to the formation or expansion of several lakes, including Lake Chungará.
- •The volcano lies precisely on the Bolivia-Chile border, with the crater rim marking the international boundary.
- •Despite no recorded eruptions in modern history, local Aymara legends suggest they may have witnessed volcanic activity.
- •Parinacota is part of the Central Volcanic Zone, which contains about 44 active volcanoes and is characterized by thick crust and unique geochemical signatures.
Histoire
Parinacota Volcano began forming in the Pleistocene epoch, developing a large volcanic cone.
Between the Pleistocene and Holocene, its western flank collapsed, generating a massive landslide that reshaped local hydrology and enlarged Lake Chungará.
Volcanic activity subsequently rebuilt the cone, erasing the collapse scar.
Throughout the Holocene, Parinacota experienced multiple eruptions, with the latest occurring approximately 200 years ago.
The first recorded ascent was made in 1928 by Carlos Terán and Joseph Prem.
Guide du lieu
Summit Crater
A large, approximately 1-kilometer-wide crater at the summit of Parinacota, offering panoramic views of the surrounding Altiplano and the neighboring Pomerape volcano. The rim marks the international border between Bolivia and Chile.
Ajata Cones
Three parasitic cones located on the southern slopes of Parinacota that have produced lava flows, contributing to the volcano's complex morphology.
Landslide Deposit AreaPleistocene-Holocene transition
The extensive hummocky deposit west of the volcano resulting from the massive flank collapse between the Pleistocene and Holocene, which dammed preexisting drainage and formed Lake Chungará.