Favorable wind conditions permit a good view inside the crater
of Pu`u `O`o in late February 1999. The crater floor is marked by several
large pits, and lava is visible in one.
The decline in crater activity in 1998 (the most recent overflow
of lava from Pu`u `O`o was in January 1998) probably results from lava downcutting beneath the flank vents and tubes leading from the vents. As
downcutting of the flank vents progressed, the level of lava in the crater
lowered, because
the vents inside and outside the crater are in hydrostatic equilibrium.
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