|Lava flows may surge or back up due to a constriction downflow
and flow out of windows or entrances. Often
this lava leaves a lining deposit around the edge as evidence of its passing,
and may even deposit lava balls that were
being carried along, around the edges of the entrance or window. A different
sort of upwelling can occur from floors of tubes when segregations boil
out of the semi-solid floor. Sometimes these resemble miniature volcanoes
or even lava roses.
In the photo below, lava has upwelled from a lower level through a window and sealed the window shut as it cooled. In the lower photo are some features upwelled on a floor.
|Created: August 4, 2000
Author: Dave Bunnell