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Photo and Video Chronology - Kīlauea - March 29, 2002

March 29, 2002
Spatter structures, and crustal overturning in Episode 55 crater

 

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Two different structures built of spatter. Remarkable, 11.8-meters-high spire at one of the hornitos at the 2300-foot elevation, between Pu`u `O`o and the rootless shields. Note person for scale.
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Two flows spilling from January 02 vent, the middle of three spatter cones on the floor of Pu`u `O`o's crater. This cone is 9.3 meters high. Shiny crust is fresh and hot.

Crustal overturning in Episode 55 crater

Lava began to fill the Episode 55 crater, just west of Pu`u `O`o, on March 27-28. A pond formed, with a floating crust. Gas bubbles rising from the lava in the pond are trapped by the crust. A density inversion results; lighter, bubbly lava underlies denser crust. Eventually a crack forms in the crust. The lighter lava gushes to the surface and overrides the crust. A slab of the crust breaks off, turns on end, and dives into the pond like a sinking ship. This process is called crustal overturning. An overturning event often sweeps across the surface of a pond in a few tens of seconds. These photos show one such event, moving toward the camera.

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The overturning has just started. The red line is the advancing front. Lava behind the front is crusting over and clearly hotter than the older crust nearer the camera.
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The overturning is advancing across the long dimension of the 85-90-meters-long, 25-30-meters-wide crater.
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Note a bit more fume in the crater. The rapid release of trapped gas as the crust overturns contributes to the fume.
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In this view, the crust nearest the camera has just overturned, and the fresh lava has not yet developed new crust.
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The crust has now been completely renewed by the overturning event. The radiant heat from such overturning is great--witness the observer protecting his face.
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