Tungurahua
The Black Giant of the Eastern Andes
5,023 m
2016
Stratovolcano
Ecuador
Location
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Volcanic Hazards & Risk Assessment
Primary Hazards
- Pyroclastic flows
- Lava flows
- Volcanic bombs and ballistics
- Lahars and mudflows
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 10 years ago | Recent | Recently active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Authority Sources
Other Volcanoes in Ecuador
- Cotopaxi
Stratovolcano
- Fernandina
Shield volcano
- Guagua Pichincha
Stratovolcano
- Reventador
Stratovolcano
Interesting Facts
Tungurahua towers more than 3,200 m above the city of Banos at its base β one of the most dramatic volcano-to-city elevation differences on Earth.
The name 'Tungurahua' means 'Throat of Fire' in Kichwa (Quechua), a name given by indigenous communities who witnessed its eruptions centuries before European contact.
The 1999-2016 eruption lasted 17 years, making it one of the longest continuous volcanic crises in South American history.
Approximately 25,000 people were evacuated from Banos in 1999, but frustrated residents forced their way past military blockades to return in January 2000 while the volcano was still erupting.
Tungurahua has experienced two catastrophic edifice collapses: Tungurahua II collapsed ~3,000 years ago, producing a debris avalanche that traveled down the Rio Pastaza valley.
The volcano's maximum known eruption intensity is VEI 5 (~1010 BCE), far larger than anything witnessed in historical times.
The famous 'Casa del Arbol' swing at Banos overlooks Tungurahua and became one of the most photographed locations in South America.
Banos de Agua Santa ('Baths of Holy Water') takes its name from the volcanic hot springs heated by Tungurahua's geothermal system.
During the 2006 eruption phase, pyroclastic flows traveled several kilometers down the flanks, killing at least 5 people in the community of Palictahua.
Tungurahua's monitoring network is one of the most comprehensive in South America, including seismometers, infrasound sensors, SO2 analyzers, GPS, lahar detectors, and webcams.
Three successive volcanic edifices β Tungurahua I, II, and III β have been built at this site since the mid-Pleistocene, with each predecessor collapsing catastrophically.
The volcano's glacier cap has been retreating rapidly, both from climate change and volcanic heating, increasing the lahar risk from rainfall on exposed ash deposits.