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Kilauea Archive
5 July 2000

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Many surface flows were visible today on the eastern side of the active flow
field. This pahoehoe flow advanced across the flow field as it filled in low
areas and spilled over the edges of previous pahoehoe toes.
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Broad pahoehoe lobe that gushed from crack in inflating lava flow near site of
photo above. Molten lava in this lobe was exposed for several minutes before crusting
over. Once crusted, small toes, such as those in photo above, began to ooze from it.
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6 July 2000

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A substantial new pahoehoe flow on the east side of the Smoke flow began
from a breakout point at about 200 m elevation on Pulama pali. The breakout
probably began on July 4. The flow is about 500 m long and 150-200 m wide.
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Lava continues to spill into the sea at three sites, and the corresponding
lava benches are still quite narrow. The most vigorous entry remains at
Waha`ula, which generated two steam plumes today. The plume in the upper
left is from Kamokuna. The third entry generates a wispy plume in the lower
right.
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18 July 2000

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In the past week, new flows have expanded nearly 150 m north into area west of lower Royal
Gardens and east of the Hawai`i Volcanoes National Park boundary. This area
is located at the base of the pali on the east edge of the flow field. As
the flows move through vegetation, small fire flare-ups draw the attention
of passing helicopters. This view is toward the south from above the base of
the pali (distance from left to right is about 1 km).
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25 July 2000

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Nearly vertical aerial view of lava dribbling over the sea cliff
east of Waha`ula. Note the lava drapery left of the dribble, formed by
earlier flows spilling over the cliff. Part of the sea cliff right of the
dribble appears ready to tumble into the surf (click on
"large" to see the detached part of the cliff). Visitors should stand mauka (landward) of any ground cracks near the cliff to avoid the danger of
a sudden collapse.
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29 July 2000

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Pu`u Koa`e, a large spatter cone on Kilauea's southwest rift zone, looms over the dark 1974
lava flow in middleground. Green pasture in background grows in Ka`oiki
fault system on Mauna Loa. Runners in the Kilauea marathon, one of the
world's toughest, approach the 11-mile post. John Smith, geophysicist at
University of Hawai`i and colleague of HVO, won the marathon for the second
time in three years, in 3 hours and change.
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Northwesternmost fault scarp in Koa`e fault system east of Pu`u Koa`e. The Koa`e fault system, a set of grabens and half-grabens whose north-facing scarps are
generally most prominent, separates the mobile south flank of the Kilauea from the relatively stable rest of the volcano. Runners in Kilauea marathon
struggle up steep trail, covered with loose sand from past Kilauea
explosions, just past the 11-mile post.
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31 July 2000
Waha`ula still most active entry with spectacular "fire
hose" display

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This view is southeast across the coastal plain of Kilauea Volcano, showing
the active ocean entries (marked by steam plumes). The most vigorous entry in lower left is
located at
Waha`ula. For the past couple of days, lava has been streaming into the sea
from atop the narrow bench below the sea cliffs in the form of a spectacular
"fire hose" (see images below).
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Lava pours from a tube directly into the sea like water shooting from
the end of a giant fire hose. The lava gushes about 10 m away from the
cliff, which is 12-15 m tall. The lava "fire hose" is very
difficult to see from the shoreline, because it begins from the edge of a
narrow lava bench; these photos were taken from a helicopter.
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Collapse features on west and south flanks of Pu`u `O`o

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A spatter cone in the West Gap has tumbled into the adjacent collapse crater,
which is about 15 wide and 25 m long (see image of spatter cone in the March 2000 update). The crater is 20-30 m deep. Red-colored tephra produced by the
collapse blankets an area 50 m wide and as far as 80 m south of the
West Gap. Sloshing sounds from lava degassing below the crater can often be
heard from the crater rim.
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This view is northwest across the south flank of Pu`u `O`o. Thick fume
escapes from the string of collapse craters leading from Puka Nui to
the minivent (see image of minivent spattering in the photo
gallery), likely marking the trace of the lava tube leading
southeastward from Pu`u `O`o. This area has not changed
significantly in the past few weeks, except that the amount heat in the area seems
to have increased.
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Map of lava flows from Pu`u `O`o to the ocean
1 July 2000

Large
map. Map shows lava flows (red) on Pulama pali and coastal
plain active since October 1999, as well as flows erupted earlier from
Pu`u `O`o and Kupaianaha. Compare this map with that for the previous updates to
see how the flow has widened eastward between Royal Gardens and Waha`ula.
Lava reached the ocean at the Lae`apuki bench on December 17-18, 1999; this
was known as the West flow. The West flow has been inactive since early April. The
eastern part of the active flow field reached the Royal Gardens private
access road on January 11 and entered the sea near Waha`ula on February 3-14,
2000. The flow descending Pulama pali to feed this area is
the Smoke flow; it is currently the only active flow.
Eruption-viewing opportunities change constantly, refer to the HVO home page for
current information. Those readers planning a visit to Kilauea or Mauna Loa volcanoes can get much useful
information from Hawai`i Volcanoes National Park.
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