Copiapó (volcano) explained

Copiapó
Other Name:Azufre
Elevation M:6052
Elevation Ref:[1]
Parent Peak:Ojos del Salado
Prominence M:1701
Prominence Ref:[2]
Listing:Ultra
Map:Chile
Map Size:150
Location:Chile
Range:Andes
Coordinates:-27.3058°N -69.1308°W
Type:Stratovolcano
Last Eruption:Unknown
First Ascent:Pre columbian, first modern ascent by Stefan Osiecki, Witold Paryski, Jan Szczepanski and Justyn Wojsznis (Poland) in 03/10/1937.[3] [4] [5]

Copiapó, also known as Azufre, is a stratovolcano located in the Atacama Region of Chile. The volcano separates the two portions in which Nevado Tres Cruces National Park is divided. In its vicinity lies Ojos del Salado. At its summit an Inca platform can be found.[6]

Dacitic volcanism occurred at this centre 11-7 million years ago and covered a surface of . The Valle Ancho fault can be traced beneath this volcano. The main cone is formed by dacites and block and ash flows that were later intruded by dacitic porphyries, associated with hydrothermal alteration. A smaller centre formed on the northern side of the main cone, as well as thick (100-) ignimbrites in two units. A complex of lava domes lies at their southern-eastern end with more hydrothermally altered porphyric intrusions named Azufrera de Copiapo. The last activity 6-7 million years ago formed a shield overlying the lava dome complex and the San Roman dome.[7] Obsidian from this volcanic area has been found in archeological sites.[8]

Some rocks in the upper parts of the volcano may be of Quaternary age.[9] The Global Volcanism Program claims that Copiapó was reported to be fumarolically active[10] by Ferdinand von Wolff 1929 who refers to Rudolph Hauthal; it also gives "Lastarria" and "Azufre" as alternative names for Copiapó.[11] Hauthal does not refer to Copiapó volcano as fumarolically active, but instead refers to Azufre and Lastarria which are volcanoes unrelated to Copiapó.[12]

Climbing

There is an Inca ruin about 40m (130feet) from the summit, accessible via the northern ridge. The platform measures 10mby6mm (30feetby20feetm) and has a 4m (13feet) high wall. The summit is probably 6065m (19,898feet) based on a Tandem-X study.[13]

The first recorded modern climb was by Stefan Osiecki, Witold Paryski, Jan Szczepanski and Justyn Wojsznis (Poland) October 3, 1937.[14] [15]

See also

External links

Notes and References

  1. http://www.peaklist.org/WWlists/ultras/andes1.html "Argentina and Chile North: Ultra-Prominences"
  2. Web site: Copiapo / Cerro Azufre. Andes Specialists. en. 2020-04-12.
  3. Book: Fantin. Le Ande.
  4. 1950. ACAB. ACAB. 72–79.
  5. www.inalto.org. www.inalto.org.
  6. Echevarria. Evelio. Summit Archaeology. The Alpine Journal. 2014. 193. 28 January 2016.
  7. Kay. Suzanne Mahlburg. Mpodozis. Constantino. Tittler. Andrew. Cornejo. Paula. Constantino Mpodozis. Tertiary Magmatic Evolution of the Maricunga Mineral Belt in Chile. International Geology Review. December 1994. 36. 12. 1079–1112. 10.1080/00206819409465506. 1994IGRv...36.1079K .
  8. Seelenfreund. Andrea. Miranda. Javier. Dinator. María Inés. Morales. J. Roberto. CARACTERIZACIÓN DE OBSIDIANAS DEL NORTE Y CENTRO SUR DE CHILE MEDIANTE ANÁLISIS DE FLUORESCENCIA DE RAYOS X. Chungará (Arica). December 2005. 37. 2. 10.4067/S0717-73562005000200009. es. free.
  9. Segerstrom. Kenneth. Geología de las Hojas Copiapó y Ojos del Salado: provincia de Atacama. Instituto de Investigaciones Geológicas. 1968.
  10. 355140. Copiapó.
  11. Book: Von Wolff. F. de. 1929. Der Volcanismus II Band: Spezieller Teil 1 Teil Die Neue Welt (Pazifische Erdhalfte) der Pazifische Ozean und Seine Randgebiete. Stuttgart. Ferdinand Enke. 828.
  12. de. Die Vulkangebiete in Chile und Argentinien. Rudolf. Hauthal. Petermanns Geographische Mitteilungen. 5. 1903.
  13. Web site: Copiapo / Cerro Azufre. 2020-04-12. Andes Specialists. en.
  14. Book: Fantin. Le Ande.
  15. 1950. ACAB. ACAB. 72–79.