February 14, 1997
A weekly feature provided by scientists at the Hawaiian Volcano
Observatory.
Pu`u `O`o: extinct or waiting?
Pu`u `O`o was alive and well on Wednesday, January 29, with acrid
fumes drifting across the landscape and an active pond glowing
red at night. The next morning, it seemed to be a dead, gutted
hulk. So goes the cinder-and-spatter cone whose name has become
synonymous with 14 years of eruption at Kilauea Volcano. What
happened?
On Wednesday, January 29, at 6:41 p.m., the east rift zone eruption
changed its style. Magma from Kilauea Volcano's main conduit
was cut off from Pu`u `O`o. As a consequence, over the next 24
hours the flow of lava through shallow tubes dwindled to a dribble
and the coastal steam plume dissipated.
These changes resulted from the opening of new cracks underground
along the east zift zone near Napau Crater, 6 km (4 mi) closer
to Kilauea's summit. As the cracks opened, magma rapidly drained
from the magma reservoir that lies deep beneath the summit caldera
and upper east rift zone. The lava pond at Pu`u `O`o also drained,
apparently into subterranean cracks nearby. The force that drove
the drainback was gravity, but gravity needed an opportunity.
Its chance came when a part of the Earth's crust became so weakened
that it could fracture and open with only the slightest change
in magmatic pressure.
With its lava pond and plumbing system drained, Pu`u `O`o lost
much of its underlying support. First the crater floor collapsed.
Then large slices of crater wall slid downward, filling the empty
pipe with debris. The collapses generated clouds of red rock
dust that roiled upward 300 m (1,000 ft) or so and drifted downwind
to be deposited as a thin blanket across an area reaching 5 km
(3 mi) southwestward from the cone.
In the aftermath, the cone gained a new shape. Its crater walls
are nearly vertical, and the crater floor, once only 60 m (200
ft) below the rim, is now about 250 m deep (820 ft). Collapse
wasn't limited to the crater, however. The "Great Pit,"
a once-circular crater on the cone's northwest flank, has widened
into a great gash. The gash enlarged abruptly as magma drained
away from Pu`u `O`o. Before dawn on Thursday, January 30, the
gash had consumed blocks from the summit and lowered the cone
by as much as 45 m (150 ft).
Today, Pu`u `O`o steams slightly as rain and fog dissipate the
heat that remains. The crater is deeply notched where it connects
to the gash. The cone is notably lower when seen from many viewpoints
in the Puna district. The glow is extinguished.
Is Pu`u `O`o extinct or merely waiting? Only time will tell.
Magma supplied from deep in the Earth is slowly refilling the
summit magma chamber that lies beneath Kilauea caldera, 16 km
distant (10 mi). Once that space has been reoccupied, magma is
likely to seek other pathways to the surface. Scientists at HVO
are uncertain what to expect. But given the lengthy eruptive
history from the Pu`u `O`o vent area, we wouldn't be surprised
by a reappearance of lava in the crater pond or from a new vent
nearby. Pu`u `O`o is one site where money might be made by those
who bet on future eruptions.
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