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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.
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.
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.
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.