Report on Tungurahua (Ecuador) — 18 April-24 April 2012
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
18 April-24 April 2012
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2012. Report on Tungurahua (Ecuador). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 18 April-24 April 2012. Smithsonian Institution and US Geological Survey.
1.467°S, 78.442°W; summit elev. 5023 m
All times are local (unless otherwise noted)
IG reported that on 18 April a plume with low ash content rose 2 km above Tungurahua and drifted NW. Ashfall was reported in Juive (7 km NNW) and Cusúa (7 km NW). The next day, steam rose 1 km above the crater and drifted W, and lahars descended the W and SW flanks. On 20 April steam plumes rose 500-800 m and drifted W. A moderate-sized explosion on 22 April produced "cannon shots" and sounds resembling blocks rolling down the flanks. Rice-sized tephra fell in Pillate (7 km W). Lahars descended the Choglontus (SW), Confesionario (WSW), Romero Ingapirca, and Chontapamba (W) drainages, causing the Baños-Penipe road to close near Chontapamba. On 24 April a steam-and-ash plume rose 2 km above the crater.
Geological Summary. Tungurahua, a steep-sided andesitic-dacitic stratovolcano that towers more than 3 km above its northern base, is one of Ecuador's most active volcanoes. Three major edifices have been sequentially constructed since the mid-Pleistocene over a basement of metamorphic rocks. Tungurahua II was built within the past 14,000 years following the collapse of the initial edifice. Tungurahua II collapsed about 3,000 years ago and produced a large debris-avalanche deposit to the west. The modern glacier-capped stratovolcano (Tungurahua III) was constructed within the landslide scarp. Historical eruptions have all originated from the summit crater, accompanied by strong explosions and sometimes by pyroclastic flows and lava flows that reached populated areas at the volcano's base. Prior to a long-term eruption beginning in 1999 that caused the temporary evacuation of the city of Baños at the foot of the volcano, the last major eruption had occurred from 1916 to 1918, although minor activity continued until 1925.
Source: Instituto Geofísico-Escuela Politécnica Nacional (IG)