Tungurahua

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This article is about the volcano. For the Ecuadorian province, see Tungurahua Province.
Tungurahua

From North (Nov. 2004)
Elevation 5,023 metres (16,479 feet) [1]
Location Ecuador
Range Andes
Coordinates 1°28′1″S, 78°26′30″W
Topo map IGM, CT-ÑIV-D1 [1]
Type Stratovolcano (active)
Age of rock Holocene (Gomez 1994)
Last eruption 2008 (continuing)
First ascent 1873 by Alphons Stübel and Wilhelm Reiss
Easiest route Scrambling/Snow/Ice PD

Tungurahua, (pronounced /tʊŋɡʊˈrɑːwə/), (Quichua tunguri (throat), rahua (fire): "Throat of Fire"[2]) is an active stratovolcano located in the Cordillera Central of Ecuador. The volcano gives its name to the province of Tungurahua. Volcanic activity restarted in 1999 and is ongoing as of 2008 with major eruptions on August 16, 2006 and on February 6, 2008.

Contents

[edit] Geography and geology

Map showing the location of Tungurahua and other volcanoes in Ecuador.
Map showing the location of Tungurahua and other volcanoes in Ecuador.

[edit] Location

Tungurahua (5,023 m) is located in the Cordillera Central of the Andes of central Ecuador, 140 km (87 miles) south of the capital Quito. Nearby notable mountains are the Chimborazo (6,267 m) and El Altar (5,319 m). It rises above the small thermal springs town Baños (1,800 m) which is located at its foot 5 km to the north. Other nearby towns are Ambato (30 km to the northwest) and Riobamba (30 km to the southwest). Tungurahua is part of the Sangay National Park.

[edit] Glacier

With its elevation of 5,023 m Tungurahua just over tops the snow line (about 4,900 m). Tungurahua's top is snow covered and did feature a small summit glacier which melted away after the increase of volcanic activity in 1999.

False-color satellite image of Tungurahura (center right, with plume of ash emanating from it) and its neighbor Chimborazo (center left).
False-color satellite image of Tungurahura (center right, with plume of ash emanating from it) and its neighbor Chimborazo (center left).

[edit] Volcanism

Today's volcanic edifice (Tungurahua III) is constructed inside its predecessor's (Tungurahua II) caldera which collapsed about 3000 (±90) years ago. The original edifice (Tungurahua I) collapsed at the end of the late Pleistocene. (IG-EPN n.d., [2])

[edit] Historical volcanic activity

Tungurahua's eruptions are strombolian. They produce andesite and dacite. All historical eruptions originated from the summit crater and have been accompanied by strong explosions, pyroclastic flows and sometimes lava flows. In the last 1300 years Tungurahua entered every 80 to 100 years into an activity phase of which the major have been the ones of 1773, 1886 and 1916-1918. (IG-EPN 1999, [3])

Tungurahua spews hot lava and ash at night (1999).
Tungurahua spews hot lava and ash at night (1999).

[edit] Recent volcanic activity

In 1999, after a long period of rest, the volcano started an eruptive process that continues to this day (as of January 2008). After the first eruptions in October 1999 which produced a major ash out-fall and led to the temporary evacuation of more than 25,000 inhabitants of Baños and its surroundings (El Comercio 1999), the activity continued on a medium level until May 2006, when the activity increased dramatically culminating in violent eruptions on July 14 and August 16. The August 16 eruption has been the most violent since the beginning of activity in 1999, accompanied by a 10km high ash cloud which later spread over an area of 740 by 180 km (IG-EPN 2006, [4]) and pyroclastic flows resulting in seven deaths and destroying several hamlets and roads on the western and northwestern slopes of Tungurahua (El Comercio 2006). The seven people who died were a family of five and two scientists.

Eruption, November 2006
Eruption, November 2006

[edit] History

[edit] Etymology

After one theory the name Tungurahua is a combination of the Quichua tunguri (throat) and rahua (fire) meaning "Throat of Fire" [5]. After another theory it is based on the Quichua uraua for crater (Schmudlach 2001). Tungurahua is also known as "The Black Giant" and, in local indigenous mythology it is referred to as Mama Tungurahua ("Mother Tungurahua").

[edit] First ascent

During their 7 year long South America expedition (1868 to 1876) the two German volcanologists Alphons Stübel and Wilhelm Reiss climbed Cotopaxi (Reiss with Angel Escobar, 28. Nov. 1872) and Tungurahua (Stübel with Eusebio Rodruguez, 9. Feb. 1873) (Schmudlach 2001).

[edit] Climbing

The Refugio Nicolás Martínez at 3,800 m (1998)
The Refugio Nicolás Martínez at 3,800 m (1998)

Climbing[3] Tungurahua is a grade PD scrambling ascent with some snow and a small glacier[4] towards the summit.

Please note: As of August 2007, climbing Tungurahua is not advised due to the high level of activity of the volcano. In addition, both refuges listed below are either severely damaged or no longer in operation. It is not recommended to attempt this climb without first consulting with locals that have familiarity with the volcano's recent activity.

  • Tungurahua can be climbed year round with best seasons being December-January and July-August.
  • A good height acclimatization is highly recommended for this climb.
  • The mountain is contained on the IGM (Instituto Geografico Militar) 1:50000 Map Baños(CT-ÑIV-D1) (IGM 1989, [6]).

[edit] Routes

The normal route starts from the Refugio at 3,800 m, scrambling towards the crater ridge, continues then inside of the eastern crater ridge via a short glacier walk to the summit ridge and the summit (4 to 6 hours). On an alternative route the summit can also be reached from the south via a camping spot at Laguna Patococha (3,730 m) via Cima Minza (4,800 m) to the top.

[edit] Refugios

There are two huts[5] serving the main route, the Nicolás Martínez hut (3,800 m) and a newer hut just below. The huts can be reached in 3 hours from the entrance to the Sangay National Park (2,800 m) just above Pondoa.

[edit] References

  • El Comercio. "Different Tungurahua eruptive activity related articles", El Comercio, Quito, 1999 to 2006. (Spanish) 
  • Gomez, Nelson (1994). Atlas del Ecuador. Editorial Ediguias. ISBN 9978-89-009-2. 
  • IGM (Instituto Geografico Militar, Ecuador) (1989). Baños Ecuador, CT-ÑIV-D1. Retrieved on 2008-01-26.
  • IG-EPN (Instituto Geofisico Escuela Politecnica Nacional, Ecuador). Tungurahua. Retrieved on 2006-08-18.
  • Neate, Jill (1994). Mountaineering in the Andes. Expedition Advisory Centre. ISBN 0-907649-64-5. 
  • Schmudlach, Günter (2001). Bergführer Ecuador. Panico Alpinverlag. ISBN 3-926807-82-2. 
  • Ruiz, M et alii (2006). Source constraints of Tungurahua volcano explosion events. Springer. 

[edit] Notes

  1. ^ Several elevation data between 5,016 and 5,029 m are used, 5,023 m is the one used on IGM maps. Used extremes are: 5,087 m (Stübel 1897) and 5,005 m (Neate 1994).
  2. ^ http://news.bbc.co.uk/2/hi/americas/5319818.stm BBC News]
  3. ^ Due to the current volcanic activity climbing of Tungurahua is not recommended since 1999 (ongoing as of 2007)
  4. ^ The summit glacier disappeared due to the volcanic activity in recent years (from 1999 onwards)
  5. ^ Due to the recent volcanic activity (Major eruptions in July and August 2006) the huts may now be heavily damaged or destroyed.

[edit] External links

Coordinates: 1°28′1″S, 78°26′30″W