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Tag Archives: Bagana
Bagana, Papua New Guinea
Based on analysis of satellite imagery, the Darwin VAAC reported that on 29 December an ash plume from Bagana drifted about 75 km W. On 30 December an ash plume rose to an altitude of 2.4 km (8,000 ft) a.s.l. … Continue reading
Bagana, Papua New Guinea
Based on analysis of satellite imagery, the Darwin VAAC reported that on 16 December an ash plume from Bagana rose to an altitude of 3 km (10,000 ft) a.s.l. and drifted SW. Source: Darwin Volcanic Ash Advisory Centre (VAAC) – … Continue reading
Bagana, Papua New Guinea
Based on analysis of satellite imagery, the Darwin VAAC reported that on 8 October low-level ash plumes from Bagana rose to an altitude of 3 km (10,000 ft) a.s.l. and drifted about 55-110 km WSW. Source: Darwin Volcanic Ash Advisory … Continue reading
Bagana, Papua New Guinea
Based on observations of satellite imagery, the Darwin VAAC reported that on 22 May a low-level ash plume from Bagana rose to an altitude of 3.7 km (12,000 ft) a.s.l. and drifted S. Source: Darwin Volcanic Ash Advisory Centre (VAAC) … Continue reading
Bagana, Papua New Guinea
Based on observations of satellite imagery and information from RVO, the Darwin VAAC reported that a diffuse plume from Bagana rose to an altitude of less than 3 km (10,000 ft) a.s.l. and drifted SW on 3 March. Later that … Continue reading
Bagana, Papua New Guinea
Based on observations of satellite imagery, the Darwin VAAC reported that an ash-and-steam plume from Bagana drifted WSW on 26 December. A plume rose to an altitude of 3 km (10,000 ft) a.s.l. and drifted W on 27 December. RVO … Continue reading
Bagana, Papua New Guinea
Based on observations of satellite imagery and reports from the RVO, the Darwin VAAC reported that a plume from Bagana rose to an altitude of 3 km (10,000 ft) a.s.l. and drifted SW on 21 December. An ash-and-steam plume was … Continue reading
Bagana, Papua New Guinea
RVO reported that during 18 October-10 December white vapor plumes from Bagana were occasionally accompanied by ash plumes generated by rockfalls from the edges of the lava flow on the SE flank. Occasionally, booming and roaring noises were heard and … Continue reading