|
Lava bubble bursts above a lava tube within the bench at the Kamoamoa
entry. Such explosions are caused when sea water invades the hot
lava-tube system and flashes to steam. The expanding steam blows a
thin-walled bubble of lava through the roof of the tube and hurls spatter onto
the bench. Thin translucent sheets of glass, named limu o Pele for their
resemblance to limu (seaweed), drift hundreds of meters downwind. Such explosions typically occur when
the bench subsides, so that the tube is at or below sea level.
|