Tipas
Vulcanism
The complex covers a surface area of 25 square kilometres (9.7 sq mi), 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.
Elevation
It has an official height of 6658 meters, however, based on the elevation provided by the available Digital elevation models, SRTM (6663m), ASTER (6627m), SRTM filled with ASTER (6663m), TanDEM-X(6699m), and also a handheld GPS survey by Maximo Kausch on 04/2013 (6688 meters), Walther Penck is about 6670 meters above sea level.
The height of the nearest key col is 6019 meters. so its prominence is 651 meters. Walther Penck is listed as mountain, based on the Dominance system and its dominance is 9.76%. Its parent peak is Ojos del Salado and the Topographic isolation is 9.8 kilometers. This information was obtained during a research by Suzanne Imber in 2014.
See also
External links
- Elevation information about Walther Penck
- Weather Forecast at Walther Penck
- Information about Cazadero
References
- ^ Perucca, Laura P.; Moreiras, Stella M. (2009). "Seismic and Volcanic Hazards in Argentina". Developments in Earth Surface Processes. 13: 267–300. doi:10.1016/S0928-2025(08)10014-1. ISBN 9780444531179.
- ^ "Walther Penck / Tipas / Cazadero Grande". Andes Specialists. Retrieved 2020-04-12.
- ^ Scanu, Marcelo (2013). "Argentine Andes 2012-13" (PDF). The Alpine Journal: 311. Retrieved 23 October 2021.
- ^ Kay, S. M.; Mpodozis, C.; Gardeweg, M. (7 August 2013). "Magma sources and tectonic setting of Central Andean andesites (25.5-28 S) related to crustal thickening, forearc subduction erosion and delamination". Geological Society, London, Special Publications. 385 (1): 303–334. doi:10.1144/SP385.11. S2CID 129489335.
- ^ "IGN Argentina". IGN Argentina. 14 April 2020. Retrieved 14 April 2020.
- ^ USGS, EROS Archive. "USGS EROS Archive - Digital Elevation - SRTM Coverage Maps". Retrieved 12 April 2020.
- ^ "ASTER GDEM Project". ssl.jspacesystems.or.jp. Retrieved 2020-04-14.
- ^ TanDEM-X, TerraSAR-X. "Copernicus Space Component Data Access". Retrieved 12 April 2020.
- ^ "Andean Mountains - All above 5000m". Andes Specialists. Retrieved 2020-04-12.
- ^ "Dominance - Page 2". www.8000ers.com. Retrieved 2020-04-12.
- ^ ap. "Academic and adventurer describes the incredible task of climbing and cataloguing one of the most remote regions of the South American Andes mountains — University of Leicester". www2.le.ac.uk. Retrieved 2020-04-12.
- "Tipas". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-28.
- Biggar, John (2020). The Andes: A Guide for Climbers and Skiers (5th ed.). Andes Publishing (Scotland). ISBN 978-0-9536087-6-8.