PVMBG issued a special report based on recent observations of Papandayan. The number of shallow volcanic earthquakes had increased in January and although the numbers fluctuated, low-frequency earthquakes also increased overall during January and February. Webcam images from the camera in the parking area showed incandescence emanating from Kawah Baru during the night on 22 February. A team of PVMBG scientists inspected the crater during 2100-2300 on an unspecified date to identify the source of the incandescence. They observed intense emissions rising from Kawah Baru, heard faint rumbling, and detected a strong sulfur odor, but did not see incandescence. Gas plumes rose 300 m from a solfatara. The color of the lake in Kawah Baru was greenish. Rumbling sounds from both the Kawah Mas and Kawah Baru solfatara complexes varied from weak to strong and gas emissions were sometimes intense. Solfatara temperatures were variable at Kawah Mas, Kawah Manuk, and Kawah Baru with a maximum temperature of 123.8 degrees Celsius. Sulfur dioxide gas concentrations were high at a distance of 500 m from the solfatara complexes. Based on the field observations PVMBG concluded that conditions at Papandayan were relatively normal. The Alert Level remained at 1 (on a scale of 1-4) and tourists were advised to stay 500 m away from the active craters.

Geological Summary. Papandayan is a complex stratovolcano with four large summit craters, the youngest of which was breached to the NE by collapse during a brief eruption in 1772 and contains active fumarole fields. The broad 1.1-km-wide, flat-floored Alun-Alun crater truncates the summit of Papandayan, and Gunung Puntang to the north gives a twin-peaked appearance. Several episodes of collapse have created an irregular profile and produced debris avalanches that have impacted lowland areas. A sulfur-encrusted fumarole field occupies historically active Kawah Mas ("Golden Crater"). After its first historical eruption in 1772, in which collapse of the NE flank produced a catastrophic debris avalanche that destroyed 40 villages and killed nearly 3000 people, only small phreatic eruptions had occurred prior to an explosive eruption that began in November 2002.

Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM)