Only
four days old, this fan-shaped lava delta (center of image) extends
about 200 m into
the ocean on the southeast coast of Kilauea Volcano, Hawai'i. The
diffuse plume of white steam
at the leading edge of the delta indicates that several small lava
flows are pouring into the ocean. Countless deltas have formed along
this coastline during Kilauea's eruptive history.
"Two mighty agencies in collision. Two antagonistic
and gigantic forces in contact, and producing effects on
a scale inconceivably grand!"
"The atmosphere in all directions was filled with
ashes, spray, gases... while the burning lava, as it fell
into the water, was shivered into millions of minute particles,
and, being thrown back into the air, fell in showers of
sand on all the surrounding country. The coast was extended
into the sea.... and a pretty sand-beach and a new cape
was formed."
T. Coan, minister in Hawai'i, 1841
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Explosions and collapsing land endanger people
Such vivid descriptions and scenes of lava entering the sea along
Kilauea's shoreline draw
millions of people to Hawai'i who are hoping to witness for themselves
growth of new land and experience the remarkable interaction of
lava and water. Beautiful and stunning, the explosive interaction
can be dangerous to visitors who venture too close to a lava entry
point. Also, the
new land created by lava entering the sea is unstable. Large areas
regularly collapse into the sea, usually triggering a series of
stronger explosions and sending a wave of scalding seawater
onshore. Such explosions have hurled hot rocks and lava fragments
more than 100 m inland!
Unfortunately, the entry of lava into the ocean is difficult to
observe from a distance because it
is often obscured by an energetic and acidic steam plume or by an
abrupt cliff above the entry point. This often invites visitors
to jeapardise their safety by walking right up to and over the
point where lava enters the ocean. Activity that may appear stable
and non-threatening can actually change without warning, leaving
no time for escape.
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