Fresh lava domes fill most of the 10,000-year old caldera of Chaitén volcano. Dome 1 began forming in May 2008, when Chaitén erupted for the first time in written history. Dome 2 began growing later, in the fall of 2008. On September 30, 2009, shifting winds were blowing the plume of ash and steam to the southeast, revealing the northern and western sides of the two domes (the southern side of Dome 1 was visible on September 27, 2009).
According to Servicio Nacional de Geología y Minería [the Chilean National Geological and Mining Service (translated by The Volcanism Blog)], the dome complex is currently growing steadily. Active lava domes are extremely unstable and dangerous. They are often steep-sided, composed of weak rocks, and prone to frequent collapses. A lava dome collapse can release one type of pyroclastic flow, a fast-moving landslide composed of extremely hot rocks, ash, and gas.
The Advanced Land Imager (ALI) aboard the Earth Observing-1 (EO-1) satellite acquired this natural-color image of Chaitén at roughly 10:30 a.m. local time.
References & Resources
- The Volcanism Blog. (2009, September 23). Chaitén bulletin no. 106. accessed September 30, 2009.
NASA image by Robert Simmon, using EO-1 ALI data provided courtesy of the NASA EO-1 team. Caption by Robert Simmon.
