Ticsani

Ticsani

The Ticsani lava dome complex (center)
Highest point
Elevation 5,408 m (17,743 ft)[1]
Coordinates 16°46′03″S 70°35′59″W / 16.76750°S 70.59972°W / -16.76750; -70.59972Coordinates: 16°46′03″S 70°35′59″W / 16.76750°S 70.59972°W / -16.76750; -70.59972[2]
Geography
Ticsani

Peru

Location Moquegua Region
Parent range Andes
Geology
Mountain type Lava domes
Last eruption 1800 ± 200 years

Ticsani or Tixani[3] is a volcano in the Andes of Peru, about 5,408 metres (17,743 ft) high. It is situated in the Moquegua Region, Mariscal Nieto Province, in the districts of Cuchumbaya and San Cristóbal.[4] Ticsani, Ubinas and Huaynaputina sit on a volcanic lineament slightly oblique to the main volcanic front, and Ticsani and Huaynaputina are the product of discrete silicic eruptions[5] and appear to share a geochemical source.[6] The volcano is of dacitic composition and has been K-Ar dated to be 190000 years old.[7] The volcano was constructed in several steps, starting from lava flows and volcaniclastics. This system collapsed westward leaving a 3 km (1.9 mi) long NW-SE ridge. In the middle Holocene, three andesitic lava domes formed with explosive eruptions. These were later overlaid with brown pumice and bombs from a later phreatomagmatic eruption. The activity of this system ended with the emplacement of the Ticsani lava dome.[8] One dacitic pumice fall of 0,4 km3 has been dated ca 11600 yr BP.[9]

Ticsani was one of the volcanoes ascended in summer 1902 by Francisco Alayza Paz Soldan.[10]

Recent activity

In May 1999, inhabitants of the neighbouring towns of Calacoa, Cuchumbaya and Carumas noticed earthquake swarms with the maximum strength magnitude 3.5 at a minimum depth of 50 kilometres (31 mi), raising fears of a reactivation of the volcanic system.[11] Between November 2005 and September 2006 a swarm of earthquakes on the NE side was observed,[12] resulting in surface deformation in the northwest sector of the volcano and subsidence in its southeast sector.[13]

References

  1. Hernando Tavera, La Crisis Sísmica de octubre del 2005 en la Región del volcán Ticsani, Instituto Geofísico del Perú, Lima 2006 (in Spanish)
  2. ign.gob.pe IGN, Peru
  3. "Volcán Ticsani". mincetur. Retrieved 2015-06-22.
  4. escale.minedu.gob.pe - UGEL Map of the Mariscal Nieto Province (Moquegua Region)
  5. Floyd W. McCoy; Grant Heiken (1 January 2000). Volcanic Hazards and Disasters in Human Antiquity. Geological Society of America. p. 16. ISBN 978-0-8137-2345-7.
  6. S. Byrdina, D. Ramos, J. Vandemeulebrouck, P. Masias, A. Revil, A. Finizola, K. Gonzales Zuñiga, 1, V. Cruz, Y. Antayhua, O. Macedo (March 2013). "Influence of the regional topography on the remote emplacement of hydrothermal systems with examples of Ticsani and Ubinas volcanoes, Southern Peru". Earth and Planetary Science Letters. 365: 152–164. doi:10.1016/j.epsl.2013.01.018. (subscription required (help)).
  7. Proceedings of the ... New Zealand Geothermal Workshop. University of Aukland, Geothermal Institute. 1988.
  8. Y. Lavallé; L.S. de Silva; G. Salas; J.M. Byrnes (2009). "Structural control on volcanism at the Ubinas, Huaynaputina and Ticsani Volcanic Group (UHTVG), Southern Peru". J. Volcanol. Geoth. Res. 286 (4): 253–264. doi:10.1016/j.jvolgeores.2009.07.003.
  9. Thouret, J. - C., E. Juvigne, J. Mariño, M. Moscol, A. Legeley-Padovani, I. Loutsch, J. Davila, S. Lamadon, & Rivera M. (2002). "Late Pleistocene and Holocene Tephro-stratigraphy and Chronology in southern Peru". Sociedad Geológica del Perú. 93: 45–61.
  10. John F. Ricker (1981). Yuraq Janka: A Guide to the Peruvian Andes. The Mountaineers Books. p. 7. ISBN 978-1-933056-70-8.
  11. Lionell Fidel Smoll; Bilberto Zavala Carrión (2001). Mapa preliminar de amenaza volcánica potencial del volcán Tutupaca (in Spanish). INGEMMET.
  12. Geos (in Spanish). La Unión. 2006.
  13. Jay, J.; Pritchard, M. E.; Aron, F.; Delgado, F.; Macedo, O.; Aguilar, V. "Volcano-tectonic interactions at Sabancaya and other Peruvian volcanoes revealed by InSAR and seismicity". American Geophysical Union. Retrieved 2015-06-21.
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