(June 2, 2006, 18:30:02 to June 3, 2006, 02:00:03)
Gas-pistoning is an interesting phenomenon seen at Kīlauea and some other basaltic
volcanoes. It is caused by the accumulation of gas near the top of the lava
column within a volcanic vent
(Swanson and others, 1979). The shallow accumulation of gas causes the lava surface to rise (the "piston"). Eventually, the gas breaches the surface and escapes, typically as a forceful jet of fume and spatter. The lava then drains back into the vent. Gas pistons can occur as single events or as a repeating series comprising dozens or even hundreds of events. During mid-2006, eruptive activity at the informally named "Drainhole" vent, on the floor of the Pu‘u ‘Ō‘ō crater, was often characterized by periods of gas-pistoning. This movie sequence is an example of the gas pistons that were occurring at that time.
The images that make up this movie were acquired by a time-lapse camera positioned on the northern rim of the pit that hosted the "Drainhole" vent. The opening in the pit floor is about 5 meters across.
File size = 96.1 MB
Image interval = 1 minute
Playback speed = 10 frames/sec
Movie duration = 00:00:45
Camera Coordinates (WGS84):
View direction = ~186º